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I ^ I J

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iiïVjr-• ^ \'»Vi/:;-\'.-ii^. ,•■ \' . , • \'.J^. \'

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STELLINGEN

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STELLINGEN.

I

Het karakter der lichtwisseling van R V Tauri tusschen J D 7129
en J D 7687 is onbekend.

II

De uitkomsten aangaande S 5 Cygni, door Whittaker en Gibb af-
geleid met behulp van het periodogram dezer ster, hebben geen waarde.

III

Nijland heeft als kenmerk van zijne interpolatie-methode aangegeven,
dat het schatten der
verhoudingen van de in „Stufenquot; uitgedrukte helderheids-
verschillen hoofdzaak is, de absolute waarde van deze verschillen bijzaak.
Men moet echter beide schattingen als even belangrijk beschouwen.

IV

Ten onrechte meent Shapley bij de afleiding van de hchtkromme
eener /g\'o/-veranderlijke, stuf en waarnemingen te mogen verwerpen wanneer
hij tevens over photometrische waarnemingen kan beschikken.

The Astrophysical Journal XXXVIII No. 2.

V

Aan beschouwingen, zooals Kiess, Martin en Plummer en ten slotte
Prager gegeven hebben over R R Lyrae, had een kritisch onderzoek van het
waarnemingsmateriaal vooraf behooren te gaan.

Lick Bulletins VII; Monthly Notices LXXV; Sitzungsberichte der Königl. Preuss. Akademie der
Wissenschaften 1916 VIII.

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Het optreden van „stationna.requot; radianten is door W. H. Pickeking

voldoende verklaard.

The Astrophysical Journal XXIX.

VII

De xr^eenrng van Easton dat ons zonnestelsel zich dichter bij C.g^.s dan
^.tA^rh^ndi, heeft door sterren-tellingen steun gevonden.

VIII

De radiale verdeelmg der straling over de zonne-schijf is voor de lange
golven gelijkmatig.

IX

Voor het onderzoek van de wisselende samenstelling van den damp-
kring der aarde zijn stralingsmetingen onontbeerlijk.

X

Het IS niet aan te nemen dat bij het tot stand komen der geluidstilte-
gordels de bovenste lagen van den dampkring een rol spelen.

^ Veisl Kon. Ak. v. Wetlsch. Amsterdan. XXIV. He.el en Dan.pknng

XI

De door Van Lohuizen bij de afleiding van zijne spectraalformule
toegepaste benadering is niet geoorloofd.

^ VAK LoHnizKK. Bifdrage tot de kennis van lijnenspectra. Den Haag X9X..

XII

De beoefenmg der sterrenkunde m Nederland zou er bij ^^
wanneer een der sterrenwachten werd vrijgemaakt van het Universitair

verband.

XIII

De strijd tegen den oorlog zal eer gewonnen worden door de beoefenaars
der natuurwetenschappen, dan door de pacifisten.

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^^ , l^ir Li

THE VARIABLE STARS
R SAGITT^ V VULPECUL^

RV TAURI

PART I

AN ANALYSIS OF THE
LIGHT-CURVE OF RV TAURI

PROEFSCHRIFT

TER VERKRIJGING VAN DEN GRAAD VAN DOCTOR
IN DE WIS- EN STERRENKUNDE AAN DE RIJKS
UNIVERSITEIT TE UTRECHT OP GEZAG VAN DEN
RECTOR-MAGNIFICUS DR. ERNST COHEN HOOG-
LEERAAR IN de FACULTEITDER WIS- EN NATUUR-
KUNDE VOLGENS BESLUIT VAN DEN SENAAT DER
UNIVERSITEIT TEGEN DE BEDENKINGEN VAN
DE FACULTEIT DER WIS- EN NATUURKUNDE TE
VERDEDIGEN OP VRIJDAG 7 APRIL 1916 DES NA-
MIDDAGS TE 4 UUR DOOR

JAN VAN DER BILT

GEBOREN TE KAPELLE (Zuid-Beveland)

BIBLIOTHFrK DFR
WJKS\'JNiVtnbsp;17

W T R E C H T

drukkerij J. van boekhoven — utrecht

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RECHERCHES
ASTRONOMIQUES

DE L\'OBSERVATOIRE

D\'UTRECHT

VI

utrecht

J. VAN BOEKHOVEN
1916

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THE VARIABLE STARS

R Sagittce V Vulpeculce
RV
7 ami

JBY

J. VAN DER BILT

observator at the utrecht observatory

PART I

An analysis of the light-curve oi R V Tauri

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S;.

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TS

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n-wi.

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CONTENTS.

Introduction
Chapter I.

Chapter II.
Chapter III.
Chapter IV.
Chapter V.
Chapter VI.
Chapter VII.
Chapter VIII.

Chapter IX.
Chapter X.

Appendix.
Summary.

The reduction of the observations to a photometric
scale .......................

The reduction of the observations to one observer......

The magnitudes....................

The light-curve.....................

The maxima and minima.....................

The periodogram .......................

A closer examination of the three periods.............

The three periodicities combined, and the possibihty of

a solution with only two periods...............

A detailed analysis of the three waves

On a possible interpretation of the results of the analysis

Page
1

10

35
42
78
89
94
103

110

116

128

133
136

The leveled light-curve . .......................................pl^^^nbsp;^

The long periodicity.........................jj^

The curves resulting from periodogram-analysis ............platenbsp;II b c and d

Stars surrounding R V Tauri ................................................pj^^^nbsp;\' jjj

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INTRODUCTION.

Ten years ago, at a meeting of the Dutch Physical and Medical Congress,
Prof. Dr.
A. A. Nijland, Director of the Utrecht Observatory, maintained
the view that the variable stars of the
Mira type must be considered as a
physically connected class, not only on account of the well known corre-
lation between their periods and their colours, but also on account of the fact
that the lengths of their periods are grouped around the mean value of 300
days, according to the probability-curve. The number of variable stars and
the knowledge of their elements have been considerably increased since
then, and it is worth while to see whether
Nijland\'s view still holds good.
If we take the periods from the latest pubhcation available (E.
Hartwig,
Katalog und Ephemeriden veränderlicher Sterne für 1915), and if we consider
all the periods in excess of 100 days, the material consists of 532 periods,
ranging from
100 to 698 days. The mean period is 297, the probable error
64; the first of these quantities (the mean period) enables us to give the
observed number of deviations from the mean, between successive limits; the
second quantity enables us to
calculate the same numbers, considering these
deviations to be quot;accidental errorsquot;.

The results are given in the following table:

Number of

errors

0

C

O—C ;

j

d

between 0

d

and 40

174

174

i

0

40

„ 80

158

146

12

80

„ 120

100

102

^ 2

120

„ 160

55

61

— 6

160

„ 200 .

31

30

1

above 200

days

14

19

— 5

---^--- _ _

-

i

.. _l 1

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This table shows that the agreement is all that can be desired, seeing
that the assumed number of 100 days for the shortest period is somewhat
arbitrary, and only the periods, not the hght-curves, have been considered,
whereas it is not certain whether all the stars with periods of about 100
days show a hght-variation of the
Mir a type.

Since m the Ephemeris there are 117 stars of the Algol class, 82 Cepheids,
17 and 8 stars belonging to the Lyrae and ? Geminorum types respectively,\'
and 4 stars, which show the characteristic hght-variation of
U Gemtnorum,
making a total of 760 stars belonging to definite classes, we may conclude,\'
in accordance with our present knowledge, that 55 % of the variable stars
have not yet been admitted to the typical classes. Nor has there been in the
last 60 years any reason to estabhsh a new class of variable stars.

There is perhaps one exception. At the close of a paper by F. H. Shares
and E. S. Haynes, concerning the light-changes of F = F14 Tauri *) (period
about 79 days), after observations made at the Laws Observatory of the
University of Missouri, between 1906 Nov. 27 and 1908 March 11, the following
interesting remark occurs:

quot;The unusual character of the variation, recorded by these observa-
quot;tions recalls that of the stars
R SagtUae and V Vulpeculae, both of which
^\'^\'have been classed as of the
Beta Lyrae type, and both of whose light-curves
\'\'have undergone very curious changesquot;

And further on:

quot;Thus far it has not been possible to formulate a satisfactory theory,
quot;accounting for the alterations of light-curve in either
R Sagittae or V Vulpe-
yiae. The discovery of a third object presenting some points of resemblance
quot;to these stars is therefore a matter of considerable interestquot;.

In these sentences we find, mentioned in the same connection,
the names of three stars, none of which belong to the
Mira variables or to
any of the three standard types of short period variables, the hght-
variations of which however seem to be ruled by the same (apparently com-
plicated) law.

See quot;Astronomische Nachrichtenquot; no. 4705.

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Let us first consider the data on which the remarks of Seares and
Haynes are based.

The variabihty of the star R Sagittae was detected in the year
1859 by J. Baxendell Sr., whose first series of observations showed the
occurrence in the hght-curve of a distinctly marked secondary minmium
between each of two principal minima, thus presenting a similarity with
the
Lyrae type. But the period was much longer (70^ 88) and the light-curve
far less regular, since the maxima precedmg and following a principal minimum
had unequal brightness; and the elements, computed from observations
extending over a period of
9 minima, could only represent these with residuals
to an amount of
3 days. Thus, Baxendell concluded that quot;this star may
quot;be ranked in the class of moderately regular variablesquot;.

Till 1865 R Sagittae was only observed by its discoverer, but in that
year E.
Schönfeld became interested m the star, and his observations soon
led him to the same conviction, that no mean curve can exactly represent
the remarkable hght-variation. In the quot;Astronomische Nachrichtenquot; no. 1857
he deals elaborately with the observations made by
Baxendell and himself
up to the year 1871, producing the first, but at the same time the last treatise
on this variable. It had been proved already that the elements derived from
his earlier observations gave the epochs of minimum brightness too early,
and that many principal minima of the years 1869 and 1870 were much
fainter than those of the years 1865 and 1866. Though for his exhaustive
discussion 25 principal minima were available, extending over 58 periods of
about 70 days, and a quadratic term had been involved in the formula, there
remained large residuals.

This formula ran as follows:
Ep. of min. = 1865 Oct. 24.587 42338 (E—31) — 0^0037369 (E—31)^

The residuals have the largest values around the principal minima,
and
Schönfeld makes the interesting remark, that they look as if a regular
process of the light-variation is disturbed by causes working for a long time
in the same direction.

quot;Man kann sich dies so vorstellen, dass die störenden Ursachen eine
quot;Zeitlang wenig oder gar nicht wirken, und dass dann ihre Wirkung plötzlich.

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^\'^^oder wenigstens sehr rasch anwächst, sich auf dieser Höhe einige Zeit erhält,
quot;und dann ebenso rasch wieder abnimmt.quot;

But, besides these irregular changes, the period seems to have shortened
since the year 1860, and the secondary minimum is no longer, as a rule, ob-
served to fall midway between two principal minima.

The observations of the years 1871 and 1872, did not confirm the shorte-
ning of the period, and those of
1873 gave a slight mdication of its lengthenmg.

Next year Schönfeld drew attention to a phenomenon of still greater
importance, viz. that of the changing brilhancy of consecutive mmima.

quot;Während in den letzten Jahren die Minimalhelligkeit durchgehends
quot;über der der mittleren Curve geblieben ist, und ins besondere die vom Jahre
^\'^\'1869 um durchschnitthch 6 Stufen übertroffen hat, ist andererseits die
quot;Helligkeit im secundären Minimum stets kleiner gefunden worden als früher,
quot;so
dass man, wäre R Sagittae erst neuerdings entdeckt worden, geneigt sein
\'\'könnte die beiden Minima nicht zu unterscheiden, und die Periode nur
35T
\'\'lang- anzunehmenquot;.

The observations made by Glasenapp m December 1875 and during
the year
1876, according to Beljavsky who reduced them, point to the
same fact. He concludes his paper on that subject by saying: quot;Der Stern
quot;R Sagittae scheint einem ausgeprägten Cephei-Typus mit einer Licht-
quot;änderung von
35.3 Tagen Dauer anzugehörenquot;.

Schönfeld, after having been called to the Directorship of the Obser-
vatory at Bonn, was obliged to stop his work on variable stars, in consequence
of which his researches into the character of the light-changes of
R Sagittae
came to a premature end.

S. C. Chandler Jr.^ well aware of the peculiar behaviour of this star
m the year 1875, formulated his conclusions in the following sentence:

quot;The results, when charted, exhibit a well marked minimum on Sept.
quot;22, but only a slight depression of the light-curve at about Aug. 23. These
quot;phenomena, which seem to indicate a reversal of the principal and secondary
quot;minima as given by Prof.
Schönfeld, are so anomalous, that, as I cannot
^\'^\'deem the observations, on which they rest, though somewhat fragmentary,
quot;to be at fault, I have thought proper to submit them in detail.quot;

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And still the full measure of the caprices of this star had not been
observed.
Baxendell, who had stopped his observations in the year 1869,
but had taken them up 8 years later, reports on his estimates of the year 1885,
that quot;in August, when a secondary minimum was due, the magnitude remained
\'\'constant {at
8™.8) for a feriod o/ 16 daysquot;.

But after Sch5nfeld, though the star was put on the list of many
observers, none of them has ever tried to detect the true character of its
light-fluctuations. In the meantime, the problem received an increased in-
terest, when in the year 1904
Stanley Williams discovered the varia-
bihty of the star
BD 26°3937, V Vulpeculae, the light-curve of which
exhibited, in approximately the same period, the same type as
R Sagittae
had shown at the time of its discovery. The period was 75.3 days, the secondary
minimum fell midway between two principal minima and exceeded these
by a full magnitude in brightness. But here too, in the years that followed,
information of a different kind came in, first of all from
E. C. Pickering,
who, from a series of 58 photometric measurements made by O. C. Wendell,
remarked: \'^they show that the successive light-curves are not the same,
quot;and that therefore this star cannot be regarded as of the (5
Lyrae type.
quot;The form of the hght-curve appears rather to be of Class II1) and resembles
quot;i?
Sagittae in having a secondary minimum nearly midway between the
quot;principal minimaquot;.

The short photometric series of Wendell was followed by an extensive
hkewise photometric, series by
F. H. Seares and E. S. Haynes. Neither did
they find the
(i Lyrae type confirmed, but thought that the star had to be in-
corporated with the short period variables, with a period half as long as that
derived by
Williams; a result running parallel with Schonfeld\'s remark
about
R Sagittae in the year 1875.

What has been said of R Sagittae apphes equally to V Vulpeculae.
The hght-changes of this star also have not been thoroughly examined over a
period of sufficient length. Moreover, the conformity of the character of
the light-variations of both of them has never been proved.

1nbsp; Variables of long peiiod.

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Shortly after the discovery of V Vulpeculae, Mrs. Ceraski, examining
the plates taken at the Moscow Observatory by
Blajko between 1895 and
1905, found the star
BD 25°732 to be variable. Very soon after its dis-
covery, this star,
RV^V 14. Taun, happened to be put on the programme
of several keen observers (i. e.
Enebo, Haynes, Nijland), and it has
been kept under examination by these three observers in such a regular
manner, that the story of its light-variation - apart from the unavoidable
gaps resulting from the star\'s place near the ecliptic - has been set down
very completely. But of this star also the data of observation have not been
uniformly studied, and what has been published by the separate observers was
derived from their personal work only. The results they have reached, strongly
recall the vicissitudes of
R Sagittae and V Vulpeculae, with this exception,
that the order of things is now reversed. In the first instance the star was
considered by both
Seares and Enebo to be one of the short-period type,
with a period of about 40 days; but a closer examination revealed the fact
that the light-curve was of the
S Lyrae type, havmg a period of about 79
days, which compares with the periods of 70 and 75 days assigned, as we have
seen, to the two stars which were discovered earlier.

Seares and Haynes were struck, moreover, by the appearance of
irregularities in all the phases of the hght-variation; and it was this fact, taken
in connection with the general character of the hght-curve, which led them
to the remark quoted on
p. 2 of this work.

After the rejection of the short-period hypothesis, Enebo discussed
his observations in three separate papers. In the first of these he says that the
star probably belongs to the
^ Lyrae type, but that there exists a secondary
variabihty, which finds its expression in the fluctuating values of the maximum
brightness. Taking
Blajko\'s photographic magnitudes into account, the
period of this secondary variation seems to him to be about three years.
The mean period of the principal variation is 78.57 days.

In the second paper, the suggestion regarding the long-period variabil-
ity of the maximum, brightness is fully confirmed, the phase of that variation
being in the spring of 1910 the same as in that of 1907. Moreover it would
seem that, roughly speaking, the minimum brightness follows a parallel curve.

-ocr page 25-

The miiiiiTLa observed in the beginning of 1910 differ fro in each other so httle
in brightness, that a strong probabihty arises, that the succession of principal
and secondary minima will shortly be reversed, thus reproducing the same
phenomenon as has been observed in
R Sagittae and V Vulpeculae. The mean
period of
79.0 days, given by Seares and Haynes, seems to be more accurate
than that of
78.57 given in his first paper.

The third paper corrects the 79.0 days\' period, since it was discovered
that the minima of
1911 March and 1912 January feU, respectively 4 and 6 days
earher than was anticipated. A mean period of 78.76 days must be preferred
to that of
79.0 days. In accordance with the three years\' period of the secondary
variation, the maximum brightness reached its greatest value towards the
end of
1911.

Nijland, arguing from a first series of observations, is inclined to
reject the
Lyrae type, and, in view of the many different values of the
depth of the consecutive minima, to consider the star an irregular short-
period variable, with a period of about 39 days.

All that has been said and suggested about the light-changes of
R Sagittae, V Vulpeculae and\' V Tauri, justifies a thorough investigation
of the observed light-variation of these stars, from the date of their discovery
till the present time; and the fact that all three have been under
regular observation at the Utrecht Observatory during the last 8 years
{R V Tauri by Nijland, R Sagittae and V Vulpeculae by the writer), provides
an additional reason for undertaking the present work. It embraces the follow-
ing points:

(«) to secure copies of all the series of observations in the form of the
original note-book records.

{§) to adopt a scale of photometrically determined magnitudes of the
comparison stars, and to bring the individual conceptions of the observers,
regarding the differences between the comparison stars, into harmony with
the photometric scale.

(/) to derive from this newly adjusted scale the brightness of the variable,
and to construct a light-curve, which shall be homogeneous, from a consider-

-ocr page 26-

atlon of the systematic differences between the results obtained from the
various observers.

to study the details of the light-curves, to embody in a mathematical

formula the law which governs them, and to seek for a possible physical inter-
pretation.

(0 and, finally, to see whether the three stars under investigation may be
regarded as specimens of a new class of variables.

The latter point is of special interest, since Enebo, m his latest public-
ations, announces that the same kind of hght-variation as is found mRV
Tauri, is to be observed in the stars T F = F 29 Andromedae and SW = V 23
Persei, and probably also in Z = F 16 Ursae majoris, T Y = V 32 Dracoms

R Y = V 17 Laceriae, T X = V 31 Perset, AV =VlQ Cygni and U Y =
V 38 Pegasi.

Though the present writer is unable to estimate the soundness of this
presumption, it appears to him that a warning should be uttered against
any premature association of an observed light-curve with such a compli-
cated type as that of
F Tauri.

The material at hand consists of

1938 observations of R Sagittae.

^^^ » ,, V Vulpeculae.
1129nbsp;,,nbsp;^^ R V Taurt.

makmg a total of 3884 observations. Most of these have never been published
before, and were handed to us by the courtesy, either of the observers them-
selves, or of the astronomers in whose care the manuscripts have been placed
Our special thanks are due to Prof. H. H.
Turner and Miss M. A.Blagg for
Baxendell\'s valuable observations of R Sagittae, and to Prof F H Seares
for sendmg us, m the most complete form, not only his own observations

but also those made by Messquot; E. S. Haynes and H. Shapley, upon F VulpL
culae
and R V Tauri.

-ocr page 27-

In the following table a summary is given of the manuscripts used.

Number

iVuthor

of

Period

i observ.

J. Baxendell

370

1859-

-1869

y 1

1 403

1877-

-1887

p. S. Yendell

: 171

1891-

-1902

J. van der Bilt

302

1907

-1915

St. Williams

298

1903

-1907

E. S. Haynes

118

1906

-1908 1

F. H. Seares

24

1906

-1908

H. Shapley !

8

1908

S. Beljavsky

48

1907

-1910 1

J. van der Bilt

225

1908

-1915

See p. 14.

Star
R Sagittae

V Viilpeculae

R V Tauri

As we have aheady mentioned, the observations of F Tauri have been
very complete. In the series of
R Sagittae gaps of several years appear, and in
that of
V Vulpeculae unnecessary gaps of several months. Moreover it^proved
possible in the case
oi R V Taun alone, to reduce the whole material to one
single observer; whereas the Hght-variation of the other two could only be
studied in separate periods; a fact which, to some extent, affects the uniform-
ity of the results. For these reasons it seemed to be preferable to devote
attention first of all
to R V Tauri, rather than to consider the stars in the
chronological order of their discovery.

-ocr page 28-

CHAPTER L

the reduction of the observations to a photometric scale.

A. The polarizing photometer.

In the summer of 1913 the instrumental equipment of the Utrecht
Observatory was enlarged by the purchase of a polarizing photometer. It
was supplied by O.
Toepfer of Potsdam, and differs from the original Zöllner
type only in the fact that the lamp is an incandescent one of 2 candle power
(requirmg 1 Ampère at 8 Volts), while the colorimeter is replaced by col-
oured glasses. It can be adjusted both to the 4} inch and to the 10 inch re-
fractors; in the former case the eye-piece has a field of 50\' and a magnifying
power of 49, in the latter the field is 30\' and the magnifying power 78.

The constancy of the current can be kept under control by using a
milhampère-meter. The influence of any change in the current-intensity
on the brightness of the artificial star can easily be expressed in terms of
stellar magnitude. For this purpose, while continually varying the current-
intensity, we have compared the maximum brightness of the artificial star
with that of a few faint stars; and we have moreover carefully noted the
reading of the ampère-meter at which the artificial star became invisible.
The results of several nights were plotted and a correction-table derived
from the curve. This table shows that, from the maximum reading used,
VIZ. I = 104.5 (1.045 Ampère) to I = 85, the change in magnitude may be
considered to be directly proportional with the change in current-intensity,
and that, for values of I smaller than 0.85 Ampère, the brightness decreases
more rapidly than the intensity.

But these low values of current-intensity have seldom been used in
the observations.

-ocr page 29-

The artificial star becomes invisible at a current-intensity of 0.64
Ampère.*).

The light-intensity of the artificial star can also be changed by the

use of different diaphragms. But though there are 8 of them, it proved in

practice to be preferable always to use the same opening of an intermediate
size.

The sector for the coloured glasses contains three openings; one of
them is empty, while the other two contain a red and a blue glass respectively.
If the intention of the constructor was to give a yellow, red or blue tint
to the artificial star, he has not succeeded, since, even with the quot;bluequot; glass,
the colour, as compared with that of a few Potsdam stars, is not appreciably
different from the designation WG of the Potsdam scale. In consequence
of this the whole series of photometric measurements has been made with
the quot;bluequot; glass; but the observation of really blue or white stars has proved
to be very difficult.

The star to be measured has always been compared with the image
formed by reflexion on the front side of the glass plate. Since care was taken
to keep the light source to the right in every position of the telescope, this
was always the right-handed image. During the observations it was found
convenient always to place the object between the two images of the arti-
ficial star, which are 5\'.4 apart; the line joining the observer\'s eyes was kept
parallel with that joining the star images.

brightness of the comparison stars for R F Tauri had been photometrically
etei mined, the same curve could be derived, with still greater accuracy, by determining from a
large number of measurements, the full brightness (M) of the artificial star at different current
intensities (I). This gave the following results:

I

M

z/M

I

M

105

m

6.70

1 m

90

m

8.20

m

100

,7.20

; 0.50 ,

85 i

8.75

\\ 0.55 ^

95

i 7.70

0.50

80

9.35

0.60

90

8.20

0.50 H

75

10.00

0.65

______

— —.....---

-ocr page 30-

Hie distance of the object from the right-handed image of the artif-
icial star was not always the same; for experience showed that, in ascertain-
ing their equal briUiancy, a feeling of confidence in the results was attamed
m the case of the brighter stars, when the images were kept at a distance
of about r; while, m the case of the famter stars, the equality could best be
ascertamed when the images were seen as a relatively close double star.

An quot;observationquot; consisted of 8 readings of the intensity circle two
m each of the quadrants. These two were obtamed
(l) by diminishing the
light of the artificial star until it had attained the brightness of the object
(2) after havmg carried on the darkening process nearly to the zero-pomt by
brightening the image again until the equahty of hght was once more verified
The current-intensity was read off before and after each observation and the
changes were taken mto account by using the correction-table mentioned above

Group
Pleiades

BD 20°

{Praesepc)

Pair

M. K.

B—M.K.

m.e.

0.57
0.41
0.98
1.12
0.86
1.25
2.03
2.01
0.57
2.76
0.38
0.42
1.14
2.06
-0.01
0.14
0.18
0.34
0.29
0.04

0.07
■ 0.07
, 0.09
0.08
: 0.03
0.05
0.06
0.05
0.04
0.10
0.07
0.08
0.10
0.06
0.04
0.07
0.06
0.06
0.06
0.08 ^

-0.01

0.12
0.14
—0.15

0.09
—0.08
0.10
—0.18
0.12
—0.11 I

0.17 !
0.10
—0.16
0.26 :
—0.04 r
0.08 i
0.07
0.10
0.01 •
—0.22 H

z/ m
M.K. I B

11

15

: 6.17

6.75

0.58

21

25

i 7.24

7.53

0.29

: 18

31

7.15

7.99

0.84

\' 27

49

7.78

9.05

1.27

12

22

i 6.51

7.28

0.77

17

39

7.10

8.43

1.33

14

44

1 6.72

8.65

1.93

9

32

1 5.84

8.03

2.19

19

26

7.18

7.63

0.45

10

45

5.98

8.85

2.87

34

37

8.12

8.33

0.21

23

26

7.31

7.63

0.32

20

41 !

7.23

8.53

1.30

12

33 1

6.51

8.31

1.80

22

23 1

7.28

7.31

; 0.03

27

29 1

7.78

7.84

0.06

2150

2149 i

6.68

6.79

0.11

2158

2159 I

6.54

6.78

0.24

2149

2172 i

6.79

7.07

0.28

2178

2185 1

6.92

7.18

0.26

-ocr page 31-

Before proceeding to the measurements of the magnitudes of the com-
parison stars for
R V Tauri, V Vulpeculae and R Sagittae, a small series of
test-measurements was made with the 4} inch refractor on a number of select-
ed pairs of
Pleiades and Praesepe stars. The magnitudes of the former were
taken from the
Müller and Kempf list in the \'\'Astronomische Nachrichtenquot;
no.
3587; those of the latter from the quot;Potsdam Durchmusterungquot; (PD).

The preceding list contains, in the fifth column, the results of these
test-measurements. Each pair has been measured on one night only; no ob-
servation has been rejected.

The sixth column gives the mean error of the interval B; it shows
that the differences B--M. K. in the last column are not much greater than
could have been expected.

Together with these measurements the number of observations made
with the
Zöllner photometer was 341, most of which concern the three vari-
able stars, forming the subject of this paper. To these are added a small
number of measurements of the variables
R Leonis and R Boötis, and of
some faint stars mentioned on p. 10.

From a consideration of the different data which can be derived from
these measurements, it appears that the mean error of an quot;observationquot; (i. e.
of the mean of 8 readings) is 0\'^037, that is to say, about half the value of
the mean error given in the preceding table. The intensity-circle shows an
index-error of 0°.5, whereas there is no appreciable effect clue to eccentricity,
or to the personal error alluded to on p. 12.

-ocr page 32-

B. The material at hand.

The following hst contains a complete enumeration of the observations
made on the star under investigation since its discovery, and which were
either available when the work was started, or were sent to me in response
to a request, published in the quot;Astronomische Nachrichtenquot; no. 4693 and
the quot;Astronomical Journalquot; no. 657.

Observer

Mrs. Ceraski
E. Hartwig .
L. Pracka...

43
73

66
4

31

46
533

47
10
11

S. Enebo . .

E. S. Haynes

E. H. Seares
} ^

No. of
obs.

11

7

8

H. Shapley . .
A. A. Nijland

J. Voûte ....
A. Brill ....
K. Boda......

Epoch

1895/1905
1905/1907
1906/1907

239 : 1906/1912

1912/1915
1906 /1908

1908 /1909
1908

1908
1908/1910
1908 /1915

1908 /1909
1913
1913

Reference

Discovery. Measures on plates taken bj\'
Blajko. Astron. Nachr. no. 4010.

Veröffentlichungen der Remeis-Sternwarte
zu Bamberg. Reihe II. Band I, Heft II.

Beiträge zur Untersuchung des Licht-
wechsels verändei-licher Sterne. 1—2.
Prague 1910. (Bulletin international del!
i TAcadémie des sciences de Bohème ij
14—10—1910).nbsp;I

I Beobachtungen veränderlicher Sterne, an- i
: gestellt auf Dombaas (Norwegen), \'teil p
II; IV; VI. (Archiv for Mathematik og
m
Naturvidenskab Bd. XXIX: XXX- Ii
I XXXII.)

^ MSnbsp;•!

! PubHcations of the University of Missouri. \'
Laws Observatory Bulletin no. 14.

IMS ■

Publications of the University of Missouri.
Laws Observatory Bulletin no. 14.

MS

MS

MS. Preliminary results have been publish-
ed in the quot;Astronomische Nachrich-
tenquot; nos. 4404, 4485, 4560, 4642 4765 •
and 4797.nbsp;|

MSnbsp;j

MSnbsp;i

MS

-ocr page 33-

comparison stars.

The estimates of the various observers have, as a rule, been made with

the use of the 10 comparison stars given in the table below. The first column

contains either the star\'s designation after the quot;Bonn Durchmusterungquot;, or

the coordinates which relate them to the variable. The next 5 columns give

the letters, with which these stars appear in the pubhcations or MSS of

the observers. The last column gives the notation adopted in the following

pages and which is also used in the chart, to be found at the end of the
volume.

C The

HartwigI
Pracka
j

Seares
Haynes
Shapley

Star

Enebo

25° 734

b

m

25° 742

26° 746

c

c

25° 728

n

25° 733

a

26° 747

d

b

25° 735

f ^

i }

d

—14s ; —8\'.7

h

88s ; 2\'.8

49« • 7\'.8

o

e

Nijland| Brill
Voute ; Boda

A

a

Adopted

a
h
c
d
e

f

h

g

k
I

h ^ c

d

a

c
e
d

Comparison stars for R V Tauri.

No photometric magnitudes of these stars were available. The exten-
sive series of measurements of the variable, which were made with the wedge
photometer of the Laws Observatory, furnish accurate values for the m-
tervals c—a and
f~~c- but none of these 3 stars have been brought into con-
nection with an existing photometric scale.

A complete hst of photometric magnitudes of the comparison stars
being of great value for the reduction of the observations, the necessary meas-

*) Probably by a misprint Pracka gives 26° 733.

-ocr page 34-

urements for this have been made by the writer with the photometer des-
cribed above. The magnitudes so obtained are based on the photometric
values, taken from the Potsdam quot;Generalkatalogquot;, of the two following

stars.

A = BD 26° 759 = PD 2966 Colour WG M = 7-.66
B = BD 25° 720 = PD2816 Colour WG M = 7\'quot;.69

The star BD 25° 731 = PD 2890. M = 8^.08, which, by its cen-
tral position among the comparison stars, lent itself still better to the pur-
pose, could not be used on account of its colour GW- (See p. 11).

Using A and B as a basis, the magnitudes of the comparison stars a—;?,
have been derived by photometric triangulation, after the scheme given
below. This produced 25 equations (considered to be of equal weight), with 10
unknown quantities, which had to be solved by the method of least\'squares.
The faint stars k and I have not been measured, since they have been used
only twice and by a single observer.

The photometer was attached to the 10 inch refractor, and each inter-
val was measured on three separate nights. Though the observations were
commenced on 1914 March 2, when the star group was still conveniently plac-
ed, the unfavourable conditions of the weather did not allow of the series
of measurements being completed in similar circumstances. On a few occas-
ions the measurements had even to be made at zenith distances of 50 to 60
degrees. This should generally be avoided here, both on account of the haze
which lies above the town, and because the observatory is shut in by high
trees, especially on its Western side. Though the corrections for atmospheric
extinction amoxmted to no more than 0™.01 and 0™.02, they were duly applied.

-ocr page 35-

March

18

21 1 22

i

26

1 27

28

1 .65

1.801

1.84
1.93

2.77
i2.85

2.73

,02
,88
59

0.60
0.33

.0.14

0.541

0.52

2.50

i2.77

2.87

0.16

12.86

0.97
1.08

0.31

i

Date
1914

April

m.e.

of
mean

m

0.052
070
076
090
086

109

042

058

059
018
067

110
102
012

043
012
033
042
022
070
058
066
012

mean

6 11 17

Interval

a~B
a
A
h~B
b^A
h
a
c-^-B
c~A
c
a
d~h
e
c
e
d
f-B
d-f
f~c

ha
h
c
h~e
h^f
g~a
g—c
g~e

g~f
g~h

6 12 14

1.83

72
64

1.73
1.67
1.89
2.09
0.46
2.56
2.81
0.96
0.97
0.58
0.39
2.71
0.06
0.27
1.98
0.99
0.41
0.71
1.95
1.02
0.49
0.73
0.02

1.56
1.79
2.11

2.40

2.04

0.40
2.52

0.88
0.94

24
35

0.63

0.17

0.25

0.27\'

0.97

1.00

iO.39

0.79

10.29

2.061.911.98
1.01
0.37 0.48

0.65
1.911.971.98

0.69

1.15
0.60

0.02

0.91

0.40

0.64

0.04

0.99
0.48
0.69 0.86

0.00

mean :0\'quot;.064

Photometric triangulation of the comparison stars for R V Tauri.

The normal equations come out as follows:

5 Bnbsp;- a ^

4A ^ a --- b —
6« — h —

A
A
A

h =

4Z)

d

7c

h =

___ B

B~
B~
B~

— e~ f^ g —
__ g — /

- d 4:6 - g -

— dnbsp; 5/ — g —

- /

— c
—■ c
c

—1.20
1.08
—1.95
3.47
3.47
0.64
0.07
1.48
4.21
4.07

/ 5g —

—nbsp;a

—nbsp;a

g 5A -

~ /

-ocr page 36-

These equations can easily be solved by using a method of approx-
imations. When the values of A and B are left as the Potsdam catalogue gives
them, and the values of the measured intervals are applied directly, we get
a set of approximated magnitudes for the comparison stars, from which the
true values can be derived by means of the normal equations. In the present
case the third approximation, which indeed differs but little from the first,
gives the final result.

.....- - -

-... —

star ;

appr.

2quot;^ appr.

i

appr.

i ^

m

7.65

1--------

j ra

7.63

m 1

i 7.63

i ^

7.69

7.76

7.77 !

a

9.37

9.37

1 9.37

b

9.72

9.72

9.72

c

10.35

10.35

! 10.36

d \\

10.69

10.64

10.64 1

1 e

1 j

11.01

10.96

10.95

\' / 1

10.55

10.59

10.59

g i

11.39

11.37 1

11.37

h

11.35

11.35 1

11.34 i

From these results we learn that the star / must, as regards its photo-
metric brightness, be placed between
c and d- but the notations given had
been previously chosen after
Enebo\'s hst of comparison stars (so far as his
material carries us), which gives / fainter than
d and

The stars g and h may be considered as equally bright. Enebo sees
g lt; h, Nijland g gt; h. Since these differences persist after the reduction
of their hght-scales to that of the photometric, the already adopted notation
for the comparison stars has not been altered.

The observer\'s estimates of the intervals between the comparison
stars give a scale in which the light-values are represented by a sequence
of \'\'stepsquot;, commencing from the arbitrary value of 1.0 for the faintest star.
With the aid of the photometric results, this light-scale must be changed
to a magnitude-scale. This can be done graphically, or by computation.

-ocr page 37-

By the latter method, a set of equations of the form

^ — a, y = p^

had to be solved by the method of least squares. In these equations means
the photometric magnitude of the comparison stars, x the reduced mag-
nitude of one of them, a, the difference, expressed in steps, between ^ and
the other comparison stars, and
y the value of one step.

We have slightly changed the above method on the following grounds:

1.nbsp;For certain intervals, the conceptions of the observers frequently
appear to differ from the photometric results to such an extent, that, when
they are admitted into the computation, they are apt to affect\'the accuracy
of the reduction of the other intervals.

2.nbsp;It is evident that the photometric scale is not absolutely correct,
and that the difference between this scale and the observer\'s conception is
not entirely attributable to the latter.

The following method, which is used in the present paper, seems to
meet these objections with some adequacy.

The light-scales of the observers are first constructed and reduced to
the photometric scale. The resulting magnitude-scales are then compared
with this scale; and when, for a certain star, the values taken from the mag-
nitude-scales differ from the photometric value
in the same direction for all
observers,
this value is changed in the same direction to an amount not
exceeding the mean error.

With this definitive photometric scale, the construction of the mag-
nitude-scales is repeated, and new values for the differences Observer minus
Photometry result. If, for one or more of the stars, this difference exceeds
the somewhat arbitrarily chosen value of 0^.20, such stars are excluded; the
step-values of the rem.aining stars are again reduced to the photometric scale,
and, finally, the excluded stars are inserted, using for this purpose the value
of one step, which has resulted from the final computation.

By this m.eans we obtain this double advantage; that the greater part
of the comparison stars can be reduced with fair accuracy to the photometric
scale; and that a value, best suited to the observer\'s conception can be adopted
for one or two divergent stars,
without spoiling the precise results of the others.

-ocr page 38-

For each individual observer, the value of one step has been treated
as a constant quantity throughout the whole range of the Hght-variation.

In the case of R V Tauri the prehminary reduction to the photometric
scale gave the following differences Observer minus Photometry. Unit = 0quot;\'.01

(E = Enebo, L = Laws observers, N = Nijland, V = Voûte).

Star

E

L

N

V

a

07

08

—02

—06

h

02

09

c

02

—11

—07

—08

e

i

f

38

04

15 1

17

g

10

—19

—11

h

-28

08 i

The star d does not appear in this comparison, since it has been used
by one observer only, and by him on very few occasions.

The differences for the stars 6 and / being all positive, we have made
their photometric magnitudes fainter; while the magnitude of 0 has been
made brighter, to an amount as large as the mean error would permit.

This mean error does not result from the normal equations, as they
have been solved by an approximative method; but it can readily be estimated
from the mean error of the measured intervals (see p. 17 last column). This
comes out at 0-.064, making the mean error of each of the magnitudes forming
0\'°.064

= 0™.045*)

the interval = -

Thus the photometric scale finally adopted, was not that resulting
directly from the solution of the normal equations, but the following:

mnbsp;m

« = 9.37nbsp;= 10.64nbsp;g =z 11.37
b = 9.76 e - 10.91 h = 11.34
_ c 10.36 / = 10.63

*) Since this quot;internalquot; mean error must be smaller than the quot;externalquot; mean error which
would have resulted from the normal equations, we are sure to be on the safe side as to the
corrections, which we now apply.

-ocr page 39-

D. The observations of Hartwig.

The observations of Hartwig have been made at Bamberg with a
10 inch refractor; they are very few in number, one estimate being made in
1905, one in 1906, and 5 in 1907.

It is, sometimes, very difficult to bring the observations of this observer
mto connection with a photometric scale, for the following reasons. They are
recorded in an unusual form, the differences in brightness being very seldom
expressed in steps. As soon as these differences exceed about 0\'^25, three
different symbols are used, two of which are explained in the introduction,
but in terms too vague to be of much use to the computer. The latter has
thus to compare the records themselves for more detailed information; and
this leads to still further confusion. For each variable the adopted magnitudes
of the comparison stars have been given, but without any information as to
their origin; and in the reductions of the observations these magnitudes are
apparently independent of the instrument used.

The brightness of the variable is derived in a way which is not described,
and which in several cases is wholly incomprehensible. Each method consistently
adopted for examining his results, is found to lead to conclusions different
from
Hartwig\'s own. Consequently, since the meaning of Hartwig\'s sym-
bols is not clear, and the course which he followed in deriving the hght of
the variable is not explained, a computer finds himself unable to attach to
the observations the weight which they probably merit.

In the few cases, however, in which R V Tauri was observed, we can
derive more or less trustworthy values for the brightness of the variable, if
we adopt the direct photometric magnitudes of the comparison stars.

Here follows, in the notation adopted by us, a summary of Hartwig\'s

-ocr page 40-

estimates; the third column gives the magmtude derived by Hartwig himself;
and the last column contains criticisms, to which, according to the present
writer, these records are hable.

Comparison stars: BD 25° 725 (A) 8^0 / o\'e

anbsp;8.5nbsp;dj 10.0

cnbsp;9.2

Remarks.

Date

Estimate

i no.

M

1905 Oct. 10 \\a»vyy c»f

8.9

/\'S.5 v3 e 1 9.8

9.2

19
29

8.85
9.2

1906 March n \\ A gt; vS.5 a\\ 8.3

1907 March 4
1907 Oct. 15

» V = c

a 6 V » c

a » V )gt; c
a»gt; c = v»/

Apparently reduced as y - i
(a c), neglecting the star/.
Then the first two symbols gt;gt;
have values less than 0?5,
contrary to the statement
in the introduction.

Apparently reduced with a
value 0™.06 for one step and
neglecting the comparison
with A.

Value of one step in accordance
with 2.

The comparison with a has been
neglected.

Reduced with the same value
for one step as under 2 and
3; the comparison with
c
has been neglected.

See 1.

The symbol »gt; is not explained
in the introduction of
Hart-
wig\'s
work; in this case it
seems from a comparison
with 4 not to differ from the
symbol ».

Reduced as = c.

-ocr page 41-

E. The observations of Pracka.

Pracka observed R V Tauri at Bamberg, sometimes with the 10 inch
refractor, sometimes with the inch comet-seeker of the Observatory, and
he obtained 1 observation in 1906 and 7 in 1907.

He too has made an extensive use of the symbols gt;, gt;gt; and gt;gt;gt;.

No explanation of these is given, but apparently no definite value
has been attached to them in the reduction of the observations.

For star-magnitudes within the limits and 12™ Pracka arrived
at the value 0quot;\\06 as being the photometric equivalent of one step. In view
of the small number of observations, we have in their reduction applied this
same value, leaving the photometric magnitudes of the comparison stars
unaltered.

-ocr page 42-

F. The observations of Enebo.

These were made at Dombaas in Norway, in 1906 with a 2| inch
refractor, and from 1907 to 1915 with a 4i inch.

The observations made with the former instrument have been reduced
to the photometric scale with the following result:

Star

Light-scale (L)

7

SL

M—Ph.

c

5.59

r

10

n

.35

m

— 0.01

e

1.00

10,

,80

— 0.11

f

1.41

10.

75

0.12

m

1 Step = 0.097

Smce none of the differences in the last column exceeds 0^.20, a second
reduction (see p. 19) is not necessary.

From a first review of Enebo\'s long series of observations made with

the larger instrument, it appears that his conception of the differences in

brightness between the various comparison stars was a different one for each

season. To illustrate this, we give, in the following list, for the different seasons the

values, expressed m steps, of the star-intervals which have been generally

used. The second column represents the values for the period 1907 Jan 3 to

April 10, and the following 5 columns give those belonging to the observational

seasons between 1907 and 1912. The last column has been constructed

by makmg use of three seasons, the number of observations being too small
to treat each season separately.

-ocr page 43-

Season
Interval^-

1910/11

1911 /12

1912/15

9.5

3.6
4.6
0.5

ac
c
e

o-f

10.5
5.7
6.6
1.1

10.4
6.6
7.2

0.8

12.4
7.1
7.6
1.6

7.0

3.5
4.1
2.3

4.0

1.1

2.5
5.4
2.2

5.3

7.2

2.3
8.3
5.9

Attention was drawn to the differences exhibited in the foregoing
table in the following way. In the course of a prehminary investigation,
Enebo\'s
light-scale was deduced from his observations as a whole, and his results
were compared with those of
Nijland in the way described on p. 35. From this
comparison it appeared that the remaining errors, which should have shown
a distribution in harmony with the probabihty-curve, as a matter of fact re-
vealed a systematic discordance, whereby errors of an intermediate value
were found to be abundant, and smaller errors were fewer in number than
were expected. For this reason, we have treated the different seasons separately,
with (as will be shown on p. 41) a corresponding improvement in the results!

The reduction to the photometric scale gave the following results:

I. Season 1907. T\' reduction.

Star

L

M

M Ph

c

7.38

m

10.40

in

0.04

e

4.59

10.73

— 0.18

f

2.56

10.98

0.35

a

1.00

11.17

— 0.20

2iid

reduction.

Star / excluded.

Star

M

M—Ph

c

10.40

in

-h 0.04

1 Step =

m

0.157

e

10.84

— 0.07

/ =

11.16

g

11.40

-h 0.03

-ocr page 44-

li. Season 1907—\'08. L^\' reduction.

Star Lnbsp;Mnbsp;M—Ph

cnbsp;6.19nbsp;10\'quot;.48nbsp; 0quot;M2

^^nbsp;3.42nbsp;10.64nbsp;—0.27

/nbsp;1-00nbsp;10.77nbsp; 0.14

2-\' reduction. The number of stars being only 3, no star can be excluded
from the reduction. Perhaps the most natural way would now be to dis-
card the chosen criterion, and to accept the first reduction, though for . the

value M-Ph is larger than 0^20. But, on the following grounds we have
preferred another course.

The first reduction is not only unsatisfactory for but for c and / as
well. The following pages will show that, for the stars involved in the final
reduction, the value M-Ph can nearly always be kept under 0^.10.

Further: the differences for the various seasons, though m some wav
irregular, show a marked tendency to a gradual diminution of the value of
one step. Now, while for the preceding season this value is 0^.157 and for
the following 0-105, the first reduction for 1907-\'08 would give it as 0-.056-
that IS to say, a value smaller than that acquired even after six years\' obser-
vation (see p. 29). On these grounds we have preferred to adopt for this
season the values for c and / of the preceding one, and to insert thequot; star .
The origmal estimates give the interval directly = 5.43 steps, and the same

^ -nbsp;The mean is 5.07 steps for a magmtude-interval

of 0™.76. Hence 1 step = 0°M50.

10quot;\'.81

in.

c =

10\'?40

e

= 10.40

0.38

/ =

11 .16

e

= 11.16

— 0.33

e =

10.81

Season

1908—09.

J St

reduction

Star

L

M

M-Ph

a

14.55

9

quot;38

0quot;01

c

5.30

10

.36

0.00

. e

1.77

10

.73

— 0.18

f

1.00

10

.81

0.18

1 step = 0\'M05

-ocr page 45-

The step-estimates give for the stars d, and BD -h 25° 729 = p,
which were only used on a single occasion, 10\'quot;.37 and 10quot;\\39 respectively.
A second reduction is unnecessary.

)ud

) ncl

Season 1909—TO

. V^ reduction.

Star

L

M

M^ Ph

c

14.35

10\'!^39

-f 0\'quot;03

e

9.02

10.80

— 0.11

f

7.09

10.95

0.32

h

6.00

11 .04

— 0 .30

g

1.00

11 .43

0 .06

reduction.

Stars / and h excluded.

Star

M

M—

Ph

c

10?42

-f 0?06

1 step 0?074

e

10.81

— 0 ,

.10

/ - 10.96

a
6

11 .41

0.

04

h =11 .04

Season 1910 -Tl.

reduction.

Star

L

M

M Ph

a

17.96

-H 0™07

c

7.46

10.34

— 0.02

d

5.96

10.47

— 0.17

e

2.26

10.78

— 0.13

f

1.00

10.89

0.26

reduction.

Star /

excluded.

Star

M

M-

-Ph

a

9™37

O^^OO

1 step = 0quot;\'.099

c

10.41

0

.05

/ - 11 quot;\'.06

d

10.57

— 0

.07

p (see under III) =

e

10.93

0

.02

-ocr page 46-

VI. Season \'

1911—\'12.

V reduction.

Star

L

M

M—Ph

a

18.64

9?53

0?16

c

8.26

10.34

— 0.02

d

8.64

10.31

— 0.33

e

1.74

10.84

— 0.07

f

1.00

10.90

0.27

reduction.

Stars d and / excluded

Star

M

M—Ph

a

9?38

O^Ol

1 step = 0\';\'092

c

10.33

— 0.03

d - 10.30

e

10.93

0.02

/ = 11 .00

p = 10.41

VII. Seasons

1912—15

. 1®* reduction.

Star

L

M

M Ph

a

29.15

9?39

0?02

c

16.13

10.29

— 0.07

e

9.12

10.76

— 0.15

f

8.00

10.88

0.25

S

1.00

11.33

— 0.04

reduction.

Star / excluded.

Star

M

M—Ph

a

mo

0?03

1 step = 0?072

c

10.34

— 0.02

/ = 10.92

e

10.84

— 0.07

p = 10.42

S

11 .43

0.06

In the following table a

summary is given of the preceding results.

From an observer\'s point of view it is worth while to remark here, that three

of the comparison stars which Enebo used (i.

c, p and d) are practically

equal in brightness, viz. 10quot;.38,

10°.40 and 10°^.

.41. On the other hand he has

not interpolated a star between

a and c, which differ by a whole magnitude.

-ocr page 47-

Though its distance from the variable is somewhat great, such a star presents
itself in h, which has been used with great advantage by both
Nijland and
Voûte.

10.35

10.80
10.75

1907

1907/

1908 /

1909 /

1910/

1911 /

1912/

Mean

1908

1909

1910

1911

1912

1915

in

m

! m

m

m

m

rn

m

9.38

9.37

9.38

9.40

9.38

10.40

10.40

10.36

10.42

10.41

10.33

10.34

10.38

10.39

10.40\'

10.41

10.42

10.40

10.37

10.57

10.30

10.41

10.84

10.81

10.73^

10.81

10.93

10.93

10.84

10.84

11.16

11.16

10.81

10.96

11.06

11.00

10.92

10.98

11.40

11.41
11.04

11.43

; 11.41
i 11.04

0.074: 0.099

0.092

0.072

-ocr page 48-

G. The observations of Haynes, Seares and Shapley.

With the exception of the measurements taken on 1907 July 31; Aug.
3, 10, 18; Sept
12, 18; Oct 4, 5, 8, which were made with a polarizing photo-
meter, all the observations were made with the Zeiss wedge photometer, attach-
ed to the 71 inch equatorial of the Laws Observatory. A description of this
instrument is given in the Laws Observatory Bulletin no. 7, and the method
of observation has been explained in Bulletin no. 8.

The measurements yield, not only the differences in magnitude
between the variable and one or two of the comparison stars /, c, and but also
an extensive series of mutual differences between the latter. These differences

we have closely examined m the case of each observer separately, with the
following results:

Haynes
d m : obs.

50
82

Seares

Shapley

A m

obs.

! m

obs.

ni

0.71

12

111

0.70

34

0.35

8 1

0.48

10

Observer I

Interval

ca

0.74
0.41

Since the three values of each interval differ by so little, the mean
value can be taken without having recourse to weights. The result is:

c —a = 0™.72nbsp;f-~c = 0™.41

These values, together with the photometric magnitudes of a, c and /,
give 5 equations, from which the magnitudes to be used for reducing the Laws
observations can be derived by the method of least squares. The solution gives:

Star

M

M—Ph

a

9\'.quot;45

0?08

c

10.26

— 0.10

f

10.65

-f- 0.02

-ocr page 49-

H. The observations of Nijland.

These were made at Utrecht, the instruments used being the 10 inch
refractor of the University Observatory, and its 3 inch finder.

The method of observation is the direct interpolation method, designed
by the observer himself.*)

The following table gives the results of the reduction to the photo-
metric scale.

Lnbsp;Mnbsp;M—Ph

Star

10quot;

3quot;

10quot;

3quot;

10quot;

3quot;

a

25.18

23.80

9quot;\\37

9\'quot;.36

0™.00

— 0\'quot;.01

h

20.62

18.70

9.76

9.80

0.00

-f 0.04

c

14.15

13.11

10.31

10.29

— 0.05

— 0.07

f

8.89

8.89

10.76

10.66

0.13

0.03

g

3.75

11.20

— 0.17

h

1.00

11.43

0.09

1 step = 0™.085 (10quot; refractor)
,, - 0.087 (3quot; finder)
A second reduction is not necessary.

quot;Astronomis\':he Nachrichtenquot; no. 3695.

-ocr page 50-

I The observations of Voûte.

These were made at Leiden with the 6 inch refractor of the Univer-
sity Observatory; the method of observation is
Nijland\'s interpolation
method.

The observations have been reduced to the photometric scale with
the following result:

Star

L

M

M~Ph

a

20.16

9\'quot;.32

— 0\'quot;.05

h

15.24

9.82

-1- 0.06

c

10.64

10.29

— 0.07

f

5.83

10.78

0.15

g

1,00

11.28

— 0.09

1 step - 0quot;M02.

A second reduction is not necessary.
On two days in February 1909
Voûte saw the variable brighter than
On these occasions he interpolated it between a and BD -h 26° 750 which
he estimated to be 6 steps brighter than a on Feb. 1 and 6^steps on Feb. 5.

Using the value of one step as derived above, the resulting magnitude of
BD 26° 750 is 8quot;\\68.

-ocr page 51-

K. The observations of Brill and Boda.

These have been made with the 8 inch refractor of the Astronomical
Observatory of the quot;Physikahscher Vereinquot;, Frankfurt a. M. The variable
has been compared with
c and/only, after the direct Argelander method.1)
The mterval between these comparison stars has been estimated at from
0 to 6
steps, which difference the observers themselves are inchned to ascribe to a
variabihty of the star c. This, however, is not evident from the long series
of estimates made by the other observers.

The mean value of the interval c—/is 3.36 steps for Brill, and 3.21 for
Boda, from which, retaining the photometric magnitudes of these stars, the
value of one step becomes
0quot;\\089 and 0\'quot;.094 respectively. With these values
the brightness of the variable has been deduced from the direct photometric
values of the comparison stars.\'

1nbsp; The observations contain one single comparison with the star e.

-ocr page 52-

L. Summary.

The following table gives a summary of the reductions discussed in

the preceding pages, exclusive of the stars which have been used only by one
observer.

01

02
35
04

—30

L

N

08

00

—05

02

06

-10

—06

—07

02

08

15

1

—17

—09

09

Star

a
b
c

f

g

h

In Enebo\'s case we have taken the mean value for the two instruments
and for the different seasons, in
Nijland\'s the mean value for the two
mstruments. The first column gives the designation of the stars and the
following 4 columns the differences: Adopted minus Photometric magnitude,
O-^.Ol being the unit. (See also
p. 20.)

From this table it appears that the star / is, for all the observers, a fainter
object than is given by the photometric measurement, which is practically
the same for the Laws and the Utrecht photometers. Differences of this kind
which have often been remarked in other cases, must probably be ascribed to
the difference in colour between the real and the artificial stars.

-ocr page 53-

CHAPTER IL

The reduction of the observations to one observer.

With a star hke R V Tauri, which has been observed over a long period
by more than one observer, and frequently on the same night, the opportunity
is presented of reducing all the observations to the standard of one observer,
after a careful investigation of the systematic differences between the various
results. For the purpose of this reduction, that observer should obviously
be chosen, whose contributions have been most continuous, and have spread
over the longest period. In the case
oi R V Tauri this observer is Nijland.
Thus our next task will be to give the results of the following comparisons:
The observations of
Nijland with the 3 inch finder, and those
made with the 10 inch refractor. Abbreviation
N —n.

2.nbsp;Enebo compared with Nijland (NE).

3.nbsp;The Laws observers compared with Nijland (NL).

4.nbsp;Voûte compared with Nijland (N — V).

5.nbsp;The Frankfurt observers compared with Nijland (N — F).

In certain cases, allowances have been made for the difference in Green-
wich M.T. at which the observations were taken. As will be seen on pp. 76—-77
the change in magnitude was, in some extreme instances, about 0\'quot;.01 to 0\'quot;.02
per hour; and, had no allowance been made for the time-difference, this would
have led to erroneous results.

Since the observations of Hartwig and Pracka are very few in number,
and fall entirely beyond
Nijland\'s period of observation, they have been
excluded from this final reduction.

I N — n. The first table gives, in the second column, the magnitudes
as observed in the finder, and, in the third, the differences N — n, expressed

-ocr page 54-

in O-\'.Ol as the unit. From the second table, it appears that these differences
do not depend upon the brightness. The mean value is N—n = —

Date

1908nbsp;Nov. 4

6
28

Dec. 30

1909nbsp;Jan. 8

15
15

23
7

7

8
]0

Aug. 10
22

Sept. 16
19

Oct. 6

24

9.58
9.43
10.16

10.04
10.41
10.44
10.22

9.80
9.58
10.48
10.36

10.05
9.87

10.18
10.46
10.10
10.54
10.46 23
16
21
33
24
23
26
18
07

08
06
20
26
18
21
08
21
21
17
14
11
05
11
33
16
23

March
April

N

Nov.

7

10.38

8

10.38

Dec.

5

10.51

8

10.29

15

10.46

1910 Febr.

24

10.29

March

1

10.21

5

10.38

1

a;

i

Date

n

1

i3

II

1

Date

n

p

II

1

Date

n

i
II

1910 March27

10.4^

: 13

1912 Febr. 21

10.44

U7

! 1913 Dec. 1

10.35

i23|

29

10.44

:30

April 10

10.4^;

!24

1 7

10.24

! Sept. 30

10.54

01

21

9.8C

124

18

10.41

10

! Oct. 2

10.51

08

Sept. 14

10.46

;28

19

10.48

17

6

10.17

14

15

10.41

10

30

10.57

15

12

10.13

13

17

10.22

15

1914 Jan. 4

10.34

20

13

10.16

22

Oct. 17

10.21

16

19

10.39

16

14

10.19

21

Dec. 2

10.25

15

March 1

10.57

10

Nov. 2

10.29

16

1913 Jan. 8

10.07

10

14

10.66

08

\' Dec. 7

10.18

11

Febr. 6

10.29

19

27

10.25

20

26

10.29

28

8

10.38

24

31

10.19

09

1911 Febr. 19

10.09

08

21

10.29

24j

April 12

10.38

16

22

10.18

15

March 23

10.38

20

16

10.33

20

26

10.37

23

April 2

10.13

07

Aug. 4

10.29

19

March 19

10.13

08

Aug. 14

10.38

29

17

10.29

15

April 11

10.09

09

Sept. 6

10.48

25

Sept. 24

10.29 11

15

10.25

22

16

10.13

10

30

10.01107 \'

Aug. 6

10.20

17

24

10.45

30

1915 Jan. 2

9.96:

29

20

10.05

18

25

10.54

11

11

10.29:

26

Sept. 21

10.29:

23

26

10.571

04

16

10.18(

33

22

10.19lt;

34

Oct. 9

10.38

15

18

10.29:

14

Oct. 24

10.36(

39 I

25

10.29

19

22 :

10.19:

16

26 :

10.29i

24

26 :

10.29 :

19

March 2 :

10.46;

321

31 :

10.38:

24

1

28 :

10.45;

23

29 :

10.29 26

Nov. 1 :

10.291151

: 1

Nov. 3 ;

10.54!

23

31 :

10.1744

Dec. 11

I0.17i08

22 ;

10.57(

)6

April 11 :

10.08105

n = —0™.17

Interval

mean
n

m

9.72
10.13
10.31
10.49

N—n

comps

7
27
41
29

-0.16
-0.13
-0.19
-0.18

9.40—10.00
10.00—10.20
10.20—10.40
10.40—10.60

-ocr page 55-

2. For the argument E, the table contains not only the direct differences
N — E, but also those resulting from (n — O\'^.H) — E, on the nights
when
Nijland used the finder only. Here, too, there is no systematic change
corresponding with that of the brightness. The mean value is N—E = —0®.20.

Date

E

N-E

Date

E

N-E

Date

E

N-E

j

1908 Oct.

19

10

.43

33

1910 Jan. 17

10.62

—35

il911 Oct.

28

10

.45

—14

20

10

.46

—31

30

10.88

—12

31

10

.54

—40

21

10

.53

96

Febr. 9

11.37

—24

Dec.

15

9

.90

—02

24

10

.70

22

12

11.24

—11

1912 Jan.

17

10

.74

—41

Nov.

4

9

.87

—37

March 1

10.27

—24

27

9

.86

—41

Dec.

15

9

.89

45

13

11.05

—34;

Sept.

21

9

.83

00

1909 Jan.

8

10

.42

19

j 15

11.19

—47|

Oct.

8

9

.87

29

9

10

.51

—28

1 26

10.76

—08!

15

10

.00

—08 i

13

10

.49

03

April 1

10.15

—11

Dec.

30

10

.01

—^2 1

24

9

.76

—19

! 4

10.09

06

1913 Jan.

9

9

.98

—06 I

27

9

.76

22^

1 Sept. 8

9.98

—46

Aug.

30

11

.14

—03 j

28

9,

.87;

—41

1 Oct. 1

10.63

—lOi

Sept.

4

10

.66

—06 1

Febr. 25

10,

,16

—14

14

10.10

—12!

27

10

.70

—17

April

1

10.

,56

14

28

10.54

441

Oct.

9

10

.57

—34

3

10.

,56

16

Nov. 23

10.14

—23

Nov.

18

10

.88

—12 1

Oct.

6

10.

62

—31

1911 Jan. 9

10.10

—10

Dec.

18

10,

,63

—32

Nov.

13

10.

73

01

31

10.09

12!

1914 Jan.

19

10,

,51

—28

19

11.

09

04\'

Febr. 22

10.27

241

Nov.

17

10.

,08

—20

21

11.

14

—07 ^

March 5

11.06

—49

Dec.

21

10.

,00

—27

Dec.

5

10.

61

43 i

20

10.11

—07

1915 Febr.

13

10.

34

—32

8

10.

58

53 1

April 15

10.16

—13

1910 Jan.

10

10.

65

08

1

Oct. 18|

!

9.85

11

1

N — E = — 0quot;\\20

Interval

comps

mean

E 1

1

m m

9.76—10.20
10.20—10.60
10.60—11.00
1 11.00—11.40

!

25
17
14
8

m

9.98
10.47
10.70
11.16

j

—0.18
1 —0.24
—0.20
—0.21

-ocr page 56-

3. The number of nights, on which both Nijland (N) and one of the
Laws observers measured the star\'s brightness, being relatively small, the
number of comparisons has been augmented by adding the indirect compar-
isons: (E-0\'quot;.20)-L and (n-0-17) - L. The table contains both the
direct and indirect comparisons. There being no perceivable relation between
difference and brightness, the result is the mean: N^L = ^O^^.OO.

The first and the last numbers have been rejected for the present
purpose.

Date

L

N-L

1907 Febr. 7

11

.95

[—52]

March 1

10

.72

00

5

11

.12

—24

14

11

.27

—18

23

10

.93

—05

Oct. 12

10

.24

—10

1908 Jan. 1

10

.09

—36

4

9

.98

—38

Febr. 19

10

.24

—29

27

10,

.57

27

29

11.

,09

—01

March 5

10.

93

—11 1

6 ;

10.

68

—14

13

......

9.

62

—17

!

Date

1908nbsp;Oct. 21

27

28

Nov. 8
I Dec. 19
21

1909nbsp;Febr. 10

16
19
25

April 1
8

1910nbsp;March 2
11

L N-L

—121
15l
—13
04
—05
—15
—26
—15
25

L

1

j N-L

10.24

i -----

i 1
! 03 !

10.65

■ 02 ;

10.65 23 \'

9.38

—14

9.64

02

9.49

13

9.68

09 i

9.88

00 li

9.92

11

10.25

—23

10.70

00 1

10.33

—11 1

9.95

03 i

9.90|[ 63]I

Date

9.62

9.63
9.65

9.57

9.60

9.58

9.61
9.63
9.73

10.14
10.10
10.20

-17
-33
-20

15

16
17
20

23

24

25

26
1
2

5
11

6

April

10.24—10

Sept.

9.94

09

N —L ^

0quot;\'.09

mean
L

Interval

N—L

comps

8
8
8

9.38— 9.63
9.63— 9.94
9.94^10.24
10.24—10.68
10.68—11.27

9.

,56

—0,

.09

9.

,72

i —0.

,09

10.

08

; —0,

,17

10.

40

—0.

02

10.

93

—0.

09

-ocr page 57-

4. N — V. For N, as before, both N and n —-0quot;M7 have been used.
When taken in groups of four, as is done in the left half of the second table,
we see at a glance that the values of N —^ V vary in a systematic way with the
brightness. These values have been plotted, and the reduction table given in
the right half of the same table has been deduced.

V |N-V

Date

N-V

V

Date

Date

V N-V

1908 Dec. 151 9.50|—06
27! 9.59 04
28l 9.69—13
30

1909 Jan. 8
12
15
18
20

23

24

1909 Jan.

Febr.

9.52 26
10.39—16

I0.40I I3

02
28
00
—06
-11
-Hi

10.16
9.67
9.71
9.65
. 9.68
25 9.68

9.63
9.46
9.40
9.16
61 9.32
■7! 9.42

26

27

28
1

-07

08
06
21
13
02
—12
04
06
10
02
—44

10
12
16
17
19
21

9.71
9.74
9.82
9.82
10.01
10.40

1909 Febr. 23
25

April
Sept.
Oct.

Nov.

6

14
21

7
13

15
17
19

10.29
10.29
10.78
11.16
10.68
10.99
10.41
10.20
10.70
11.03
11.10
11.16

—21
—27
-—06
—33
—37
—28
01
02
02
—14
—19
—03

V

N-

-V

V

N-

-V

Reduction

table

V

N V

V

N-

-V

m

1

m . i

m

n

1

m

m

m

9.32

0.

11

10.40

0.

12

9.00

0.14

10

.20

—0

.08

9.52

0.

08

10.79

—0.

17

9.20

0.10

10

.40

—0

.11

9.66

0.

01

11.11

0.

17

{9.40

0.07

10

.60

—0

.15

9.70

—0.

091

9.60

0.03

10

.80

—0

.19

9.85

0.

05i

9.80

0.00

11

.00

—0

.22

\' 10.23

—0.

111

i

10.00

—0.05

11

.20

—0

.26

-ocr page 58-

The comparison N — F leads to the following result:

Date 1

F

N

F

1913 Febr. 20 1

m

10.31

! n
\' 0.

r

15

21

10.24

—0.

19

22 ;

10.19

—0.

15

24 1

10.12

—0.

19

March 25 :

10.94

0.

29

If the first value is rejected as being discordant, the mean is

=nbsp;whereas the general mean is —0\'M3. We have preferred

to adopt the latter value.

The ioregoing comparisons have enabled us to reduce all the obser-
vations to one observer, excepting only (perhaps) the short series which
Enebo
made with the 2i inch refractor; for, with regard to these observations, no
means were available for comparing them, either with the results obtained
with the larger instrument, or with those of
Nijland. It will be noticed further
on, that the corrections apphed to
Enebo\'s observations with the 4| inch
have, for this reason, been apphed to those with the 2i inch refractor also.

Before proceeding to discuss a light-curve based on the newly reduced
observations, a final criterion is wanted, for deciding whether we now have the
right to consider this curve as homogeneous. Such a criterion may be established
in the following way. The difference iV - # being very constant throughout,
the results 0^.17 may be considered to be equivalent with the results iv!
Assuming this, there remain 147 differences between
Nijland and the other
observers who have contributed to the light-curve.

If we find the values of these differences grouped as if they were
residuals from a mean value (TV), according to the probabihty-curve, the light-
curve we have obtained may be considered as homogeneous. The foUowing
table shows that there is an excellent accordance between the number of

5.

-ocr page 59-

cases (O), in which a difference has been quot;observedquot; witlhn certain hmits,
and the number of cases (C) which we should have expected to find, if these
differences had been purely accidental errors.

!

........ 1

Limits

0

C

0 C i

! \'
i

m m

0.00 0.10

74

72

2 :

0.10 0.20

44

43

1

0.20—0.30

22

25

—3 !

0.30—0.50

7

7

0 1

From this table it appears that our investigation has enabled us to
construct a light-curve, which would have been the same
had all the obser-
vations been made by a single observer, using the same instrument during the
whole period.
Therefore we are warranted in regarding this hght-curve (with
perhaps the one provision we have aUuded to above) as being strictly homo-
geneous.

-ocr page 60-

CHAPTER IIL
The magnitudes.

The following pages contain a complete hst of all the visual observations
of the hght of the variable, from its discovery until May 1915. This list is
given in two divisions, separated from each other by a double hue. The first
division, filling the left-hand side of the page, contains all that is directly
connected with the work done by the
observers; the second division contains
the data which the
computer derived, to form a basis for the construction of a
homogeneous light-curve.

In detail, the contents of the different columns are as follows: ■

1quot; Division.

Col. 1. The date, and, so far it is given by the observer, the time of
observation. This time is expressed by
Enebo in M. E. T. (G. M. T. l\'\' Oquot;\' 0quot;^),
by Nijland in Utrecht M. T. (G. M. T. nbsp;by Voûte in Leiden

M. T. (G. M. T. 0-17\'quot;56^), and by Brill and Boda in Frankfurt M.T.
(G. M. T. 0^^34-36^). Hartwig, Pracka and the Laws observers have
expressed the hour of observation directly in
G. M. T.

Col. 2. The observers. In this column the abbreviations have the
following meaning:

e E = Enebo when using the 2| and 4i inch refractors respectively.

Hg = Hartwignbsp;P - Pracka.

H = Haynesnbsp;S = Searesnbsp;Sh = Shapley.

n N = Nijland when using the 3 and 10 inch refractors respectively.

V = Voûtenbsp;Br = Brillnbsp;B = Boda.

Col. 3. The estimates. These are given in three different forms, viz.

a. the direct Argelander form. Thus (Enebo, Brill, Boda) c 3 v,
v2f or
(Hartwig, Pracka) c 3 y 2 /, means that the variable was 3 steps

-ocr page 61-

fainter than c, and 2 steps brighter than /. Equahty of brightness is indicated by
the sign
= {v = c), not by the designation 0 steps {vO c), as preferred by some
observers.

b.nbsp;the photometric form (the Laws observers), the measm-ed differ-
ences being expressed in 0*^.01 as the unit. Thus c 27; / —03 means that
the variable was 0\'quot;.27 fainter than
c, and 0quot;\'.03 brighter than /.

c.nbsp;the interpolation form (Nijland, Voûte). In this form the notation
a 3 y 1
h simply means (y —■ a) : {b — v) =3:1.

Col. 4. The brightness. This column needs no further explanation
after what has been said above. For the results of the estimates of
Hartwig
and Pracka see pp. 22—^23.

Col. 5. Remarks. These have been taken exclusively from the MSS
or pubhcations of the observers, and condensed into the fohowing system
of abbreviations:

m = moonnbsp;M = moon bright or troublesome

t = twilightnbsp;T = twilight strong

g = seeing goodnbsp;G = seeing very good

b = seeing badnbsp;B = seeing very bad

h = haze, dampness, mist H = strong haze or fog
c = clouds w = wind W = strong wind
d, D, u, U = observation difficult, very difficult, uncertain or very uncertain.
! = observation very good 1 = star at a low altitude.
In this column the reader will find a few estimates of the colour of the
variable made by
Nijland, and expressed in the weU known Osthoff scale.

Division.

Col. 1. The Julian day and its fraction in Greenwich Mean Time,
given in two decimals. In a few cases only was this impossible, viz. when
the time given by the observer was only accurate to the nearest hour.

Col. 2. The brightness, reduced to N, as derived from col. 4 of the
Division by means of the data arrived at in the preceding chapter.
Col. 3. References to the remarks suggested by the values of col. 2,
or by the light-curve which was constructed from these values.

-ocr page 62-

Date
local time

1905
Oct. 10

Remark.s

see
page 43

J. D.

G. M. T.

Obs.

Estimate

M

241

7129.44

Hg

V between a and c

9.87

Remarks
M\' ; see
I page 76

1906
March 3
Aug. 27
I Sept. 7
10
11
13
18

23

24
28

9

13

15

16
18
21

25
9

11

14
25
27

5

6
10
11

17

18

Hg

e

13.0
12.3
12.0

11.3

11.4
10.7
10.6
11.3
11.7

9.5
11.0
10.2

9.4
10.0
11.6

9.6

7.2

7.0

8.3

8.2

7.7

Oct.

Nov.

P

e
gt;}

H

e

H

e

H

Dec.

6.4

/0.5 V
c2 V

cl V
civ
civ
c2 V
c2 V
c2 V
c2.5 V
c3 V

c2.5 V

civ

cl.5 V
cl.5 V

/I V

G u

g u

G
G

G

V 3.5 h
e2 V
c2 V

c 15 / —06
v3 e v2 f c2 V
c 10 / — 38
v2 e v2 f c2.5 V
c 42
/ —23
c 82 / 02
vie V = f c3 V

Vnbsp;3.5a

v2 f

Vnbsp;==■- c
v4f
v4
f
v4f

9.16
10.80
10.57
10.35
10.41
10.41
10.41
10.52
10.52
10.52
10.65
10.70
10.62
10.45
10.48
10.48
10.45
10.82
11.14
10.99
10.54
10.50

10.54
10.31
10.59

10.55
10.87
10.70

G m U
G m

g m u

g

G
g 1
G

G

g

G ]
G
G
G

Vnbsp;=e

Vnbsp;2 e

Vnbsp;4: e

Vnbsp;4 e

Vnbsp;4 e
v3 e
v3 e
v3 e
vie
vie

Vnbsp;1 /
y 3 /

v3 /
f

Vnbsp;= e

V 1 /

G

g u
G 1

c It;

7273.
7450.
61.

64.

65.
67.
72.

77.

78.
82
93
97
99

7500
02
05
09
24
26
29
40.
42.

50.

51.

55.

37
50
47
46

43

44
40
40

.43
.45
.36
.42
.38
.35
.37
44

36
26
49
25

37

7

30

8
28

10.60
10.37
10.15
10.21
10.21 i
10.21 !
10.32 i
10.32 i
10.32 i
10.45
10.50 I
10.42
10.25
10.28
10.28
10.25
10.62

10.79
10.34
10.41
10.34
10.22
10.39
10.46
10.78
10.50

56.
62.
63.

23

1907

Jan. 3nbsp;7.8

5

6nbsp;8.2
13nbsp;7.2
19nbsp;7.9

E
P
E

v2 e I\' 1.5 / c3 V

f 4 v2.5 e
V = e V = f c3 V
vie v2 f c3 V
e2 Vnbsp;V ^ f

10.78
10.81
10.96
10.80
11.15

G
g

G

79.28 ao.58
81.3 —
82.30 10.76

10.60
10.95

89.26
95.29

-ocr page 63-

Date
local time

Obs.

Estimate

M

Remarks

see
page 43

J. D.

G. M. T.

M\'

Jan. 20

H

c 55

f 11

10

.78

7596

.8

10

.69

21

gt;gt;

c 80

/ 47

11

.09

97

.8

Tl

.00

25

J gt;

c 97

/ 54

11

.21

7601

.8

11

.12

27

! gt;

c 212

/ 159

12

.31

m

03

fj
. 7

12

.22

Febr. 2

6

.9

E

e 4 V

/3 V

11

.55

G

09

.25

11

.35

4

8

. 7

.gt;)

V = k V =

= g v2 I

11

.40

G

11

.32

11

.20

5

9

.9

gt;gt;

V = k y. =

^ g v2 I

11

.40

G

12

.37

11

.20

7

8

.7

\\ e 4 V

f4v

11

.63

b

w u

14

.32

11

.43

gt; !

H

^ c 180

f 119

11

.95

gt;)

.8

11

.86

8

!gt;

c 159

/ 103

111

.75

15

.7

11

.66

11

))

c 115

/ 70

11

.38

18

.7

11

.29

12

,) }

c 94

/ 55

11

.20

19

.6

11

.11

14

gt; gt;

c 69

/ 23

10

.91

21

. 7

10

.82

15

) gt;

c 50

/ 21

10

.81

22

.6

10

.72

16

gt; gt;

Sc 42

/ 11

10

.72

23

.7

10

.63

17

8

. 2

E

\\e2 V y 1

/ \'02g

11

.08

G

I

24

.30

110

.88

23

8

.7

))

elf 1

f c3 V

10

.96

G

M

30

.32

10

.76

24

H

c 63

/ 18

10

.86

31

.7

10

.77

26

,,

c 39

/ 17

10

.73

33

.7

10

.64

28

8.

. 1

E

: e I V

/

10

.92

g

m

35

.29

10

.72

March 1

9.

8

))

e 1 V

v2 j

10

.92

G

m

36

.36

10

.72

J)

H

c 48

f 05

10

.72

gt;) \'

.6

10,

,63

2

8.

9

E

el.5 V

V 1 /

11

.03

G

\\ 37,

,33

10,

,83

3

7.

7

))

e2 V

V 1 /

11

.07

G

38.

,28

[10,

.87

))

P

e2 V 4 h

11

.07

n

,34

4

Hg

f3.5v3e

10

.79

39,

,39

5

7.

8

E

e2.5 V

vl.b f

11

.08 i

G

40.

,28

10.

,88

.1)

H

c 90

f 46

11

.13

J J

,7

11.

,04

6

8.

6

E

e3 V

V 1 /

11.

,15

G

41.

32

10.

,95

9

7..

8

) gt;

e3 V

^ - /

11.

,23

G

44,

,28

11,

,03

10

8.

1

gt;gt;

e3 V f =

/ vl g

11.

,24

G

45,

29

11.

,04

11

8.

2

e3 V V 1 f V 1 g

11,

,24

G

46.

30

11,

,04

14

8.

0

))

e3 V / 0.5

V V 0.5 g

11,

,29

G

49.

29

11.

09

))

H

c 99

/ 64

11.

27

ygt; ■

6

11.

18

15

))

c 106

/ 74

11.

35

50.

6

11.

26

16

9.

1

E

e4 V /2 I

gt; V ^ g

11.

45

G

51.

34

11.

25

18

10.

8

J)

e 4 V f 2 I

\' w =

11.

45

G

53.

41

11.

25

21

H

c 125

/ 4- 76

11.

46

56.

7

11.

37 :

22

9.

2

E

e3 V V I f v2 g

11.

13

G

m

57.

34

10.

93

Remarks |

see
: page 76

-ocr page 64-

Remarks

see
page 43

J. D.
G. M. T.

Remarks;
M\'nbsp;see

page 76 :

Estimate 1 M

Obs.

\\e2 V vl / ti2g|ll
\'c 77 / 18 ^10
I c 61nbsp;/ 26|lO

\\e2v vlf v2g\\ll

G m
G

igquot;

G

8.7
9.5

\' e 1 V
c
57
e 1 V

/3 v2
c 61

c 58
e3 V V
c —45
c — 14
c 11
c 12
c 08
v2 e

V

10.78
ilO.69
11.04
9.71
10.04
10.08
10.22
10.27
10.39
10.19
10.52
10.48
10.50
9.96
10.29

9.98
10.14

10.13

9.99

9.94
9.99

9.88 \'
9.81

10.39

9

10 9.5
July 31
Aug, 3
10
12
18

Sept, 11 12.9
12
18

E
H

A

gt;gt;

4

i

gt;gt;

5

gt;)

8

) J

9

10.8

E

11

H

12

10.0

E

J !

P

gt; 1

H

15

Hg

16

9.8

E

18

Hg

))

H

19

11.4

E

) J

Hg

21

H

23

y J

29

j

Hg

1

9.5

E

2

P

00
21
23

43
— 31

vZ e
c — 04

V 4, e

c 09

V 5 e

34

G
G

G m
G m

G

c 5 V /

10

/ 11 10
V = f n
e
llO
/ 23 110
/ 08 ilO
= / i^lgill
/ — 86 I 9
/—51 10
/—68 10
/ —40 10
/—27 10
f 3 / c 1 y 10

/ —35I1O
/ 11 10
/ 00 ;io

/ —15 10

/—49 10.
y 4 / c 1 y 10,
/ —73 :10.
V 5 f V = cllO.
v7 e
nbsp;;io.

/ —56 IlO.

Vnbsp;^ cnbsp;IlO.

Vnbsp;5 f v2 c\\lQ.
dlt;o V
nbsp;19.

c —19 / —66 10.

Vnbsp;b e V 0 f v 2 c IQ.

Vnbsp;between a and c 9.

c — 28nbsp;/ __69 I 9

c —36 I 9.

V = cnbsp;ilO.

v2e v4f c2v\\l0.
vS/nbsp;10.

March 23 8.3
gt;}

25

26nbsp;9.3
31

y 1

April 1

E
H

J J

E
P
E
H
E
P
H

y)

E
H

G

.08
.93
.89
.08
.64
.08
.79
.08
.80
.87
.78
.24
.80
.13
.17
.31
.36
.59
.28
.61
.57
.59
.05
.49
.07
.34
.50
.22
36
19
73
03
19
87
97
90
I
36 I
59
46 ;

7658.30
.. -6
60.6

61.34
66.37
„ .32

67.6

68.35

69.40

74.7
75.6

76.36
7788.9

91.8

98.9
7800.9

06.9

30.50

31.9

37.8

53.8

54.8

57.8

58.41

60.9

61.37
„ .44
,, .8
64.66
65.36
67.35
„ .0
68.43
„ .45

70.7

72.8
78.47
81.35
82.3

10.88 I
10.84 I
10.80
10.88 !

10.88
10.70
10.88

m

-ocr page 65-

1

Date
local time

Obs

Estimate

1 M

1 Remarks
j see
1 page 43

1 J. D,

1 G. M. T.

M\'

: Remarks
j see
j page
76

Nov

4
8

H
P

1 c 28 /
c1 v^ f

— 17

lio.si
10.61

orange red

7884.0
88.39

10.42

i

j

1

25

H

c 06 /

— 55

; 10.21

; 7905.8

10.12

!

29

9

.5

E

V 4: e V 4 f ^

1 c

10.34

09.35

10.14

Dec.

4

H

c 01 /

— 35

ilO.28

14.9

10.19

5

J gt;

c 21 /

22

!I0.45

15.8

10.36

6

10

.3

E

el V vS /

c2 y

10.79

IG

16.39

10.59

1

23

8

.8

))

v2 e v3 f

c 1 y

10.59

G

33.32

10.39

i

25

7

.9

;)

\\v 5 e V 6 /

y 2 c

10.14

G

35.29

9.94

1
[

27

7

.4

yy

\\vQ e

y 3 c

9.93

G !

37.27

1 9.73

25

30

H

c — ] 5 /

— 46

10.15

40.8

10.06

23

1908

1

1 Jan.

1

/

.6

E

V 3 c

y 6 ß

9.93

G !

42.27

9.73

i

1)

H

\\c — lO f

— 62

110.09

-7

10.00

4

7

.8

E

V 4 c

1 9.80

g !

45.28

9.60

i i

))

H

c — 22 /

— 73

9.98

! „ .8

9.89

1 1
7

6

10

.6

E

3 c w 5

y 6 /

10.09

G

47.40

9.89

7

9

.0

w

V 3 c

V 5 e

10.00

G

48.33

9.80

8

H

c —13 /

— 29

10.24

49.7

10.15

33

14

))

c —30 /

— 67

9.97

55.6

9.88

16

! J

c — 14 /

— 25

10.26

57.6

10.17

17

})

c—06 /

— 36

10.24

58.7

10.15

18

gt;}

c — 05 /

— 36

10.25

59.6

10.16

19

7.

2

E

i\' = c y 4 ß

y 5 /

10.34

G m

60.26

10.14

21

H

c 05 /-

— 37

10.29

62.6

10.20

22

8.

6

E

y = c y 4 (3

y 6/il0.29

G

63.31

10.09 i

23

H

c 13 /.

- 34 :

10.35

64.5

10.26 i

i

24

)}

c 06 /-

34 i

i

10.31

65.6

10.22

25

7.

8

E

y 2 e y 4 /

c 2 y ^

10.59

g

66.28

10.39

27

H

c—05 /

— 30

10.28

68.6

10.19

29

c—06 /

— 33

10.26

70.7

10.17

Febr.

31

8.

2

E

y 4 c

y 8 5

9.70

G

72.30

9.50

8

1

7.

4

\'■\' 1

V 5 c

9.65

G !

73.27

9.45

4

6.

8

1

yy

V 4 c

9.80

G

76.24

9.60

5

6.

4

gt; y

V 4 c

9.80

g

77.22

9.60

6

H

c—27 /-

-49

10.07

78.7

9.98

30 1

9

8.

2

E

y 3 c

V Q e

9.93

G m

81.30

9.73

i

12

6.

8

yy

y 1 c

10.25

g M u

84.24

10.05

j:

-ocr page 66-

Febr. 16

17

18
19

21
22

24

25

26

27

))

28
29

March\'l

3

4

5

J1

Obs.

H

E

7.6
8.1
.7.2

H

7.2

7.3
8.2

9.1

7.8

8.6
8.3
9.1
8.0

E
H
E

H

H
E

) J

H

E
H
S
H
S
H
S
H
S

))
H
E
S
H
E
H
S
E
S

6

10

11
12

13 8.1

14 7.9

15 8.1

Estimate

14

vie

V 2 c

vie
c 03
c 15
c 10
c2 V v3 e
c 23
el V v2 f
e2 V
c 49
e3 V
e3v
c 83
e3v

e3 V fl.5v
e2.5
V
e2v
c
58
vie
c
43
c 27
c ^01
c — 13
c — 18
c — 32
c — 34
c —47
c —59
c — 49

c — 67
c —63

c — 58

/ —96

c — 69

v Q c

c — 67 « 23.

— 50
v 5 e

Vnbsp;5 e
/ — 42
/-18
f — 22

Vnbsp;5 f

/-17

c3 V

Vnbsp;1 /
/—04

/ 1 V
fl V

/ 45 I

^ = / 1
v3g\\

V = /;

1.5 /
/ 22 !

c3v\\
/-Ol
/ —05
i
/ — 43
/-51:
/ — 59 i
/ — 54
/ — 72
/ —68
/ —102
/-84

v3 f

v 5 c

/ —106
/ — 100

V 5 c

M

10.13
10.15
10.10
10.15
10.26
!I0.44
10.39
10.49
10.48
110.89
11.06
10.68
11.28
11.28
11.09
11.21
11.20
11.17
11.02
10.85 h b
10.74 ig m
10.66
10.56
10.23
10.13
10.07
10.02
9.92
9.88
9.65
9.79
9.65
9.59

9.64nbsp;I

9.65nbsp;I G m
9.68 1
9.57

9.50 \'G m
9.63 :

Remarks

see
page 43

g m
G m
G

G !

G !
G

G !
G !

G !

G
g

G

G m

^ J. 1).

G. M. T.

7988.6
89.27

90.29
91.26

-7
93.6
94.6
96.26
97.6
98.26

99.30
.. .6

8000.34
01 .28
„ .6
02.32

04.30
05.34

06.29
„ .6

07.31
„ .6
„ -6
]0.6
„ .6
11.6
„ -7
12.56
„ .57
13.56
» -57

14.30
„ .57
„ .57

15.29
„ .55
„ .66

16.30
„ -57

Remarks

see
page 76

M\'

10.04
9.95
J 9.90
i 9.95
10.17
10.35
10.30
10.29
110.39
|l0.69
110.86
\'10.59
jll.08
111.08
111.00
ill.01
11.00
: 10.97
110.82
10.76
10.54
,10.57
i10.47
10.14
10.04
9.98
9.93 ^
9.83
9.79
9.56
9.70
9.45
9.50
9.55
9.45
9.59
9.48
9.30
9.54

-ocr page 67-

Remarks

see
page 43

Remarks

see
page 76

J. D.
G. M. T.

Obs.

Estimate

M

M\'

March 15

16 8.1

17 8.4

18 8.0

19nbsp;7.8

20nbsp;8.1

J J

H

M

E
S
H
E
H
E
S
H
E
S
E

S
H
E

H

gt;j

E
H
E
S
E
S
H
S
E
H

22

23 8.8

c -
c -

Vnbsp;5
c -

Vnbsp;5

24nbsp;8.0

25nbsp;9.1

))

26nbsp;8.8

V 5 c

J)

30

Vnbsp;4

Vnbsp;3

8.9
8.9

v \\ c

c 14

c —44

April 1

2nbsp;9.2

3

5nbsp;9.3

6nbsp;9.0
8

11nbsp;9.5

12

13 9.4
16

H
E
S
E
S
H
E

a 20

c
20
c

19
06

c
c
c

a
a 02
a 04

23

24

-72
-63

c

-61

c

a
a

a

16
22

G

25

G

26

V 5 c

17
10

Vnbsp;5 e
15

Vnbsp;e

a

G

G
G

27

gt;}

31
33

a 30

07
14

c —
c-

v2 c

c —17

v2 c
c — 04
v2 c

G

G t
G

G m


Vnbsp;Q e

Vnbsp;5 e

Vnbsp;4 e

67

9.62
9.65
9.65
9.65

9.64
9.51

9.65
9.65
9.65
9.60

9.60
9.53
9.65

9.58

9.59
9.85
9.62
9.78

9.61
9.67
9.78
9.75
9.93

10.08

10.19
10.12

il0.15
10.10
110.05
10.15

10.20

10.23

10.25
10.34

10.24
10.31

10.26

10.25
9.84

.57
.29
.67
.31
.60
.60
.29
.28
.30
.60
.61
.58
.32
.56
.57
.29
.55
.34
.56
.57
.32
.63
.33
.33
.58
.58
.34
.58
.64
.35
.63
.33
.61
.35
.63
.61
.62
.35
.57

9.53
9.45
9.56
9.45
9.55
9.42
9.45
9.45
9.45
9.51

9.51

9.44

9.45

9.49

9.50

9.65
9.53
9.58

9.52
9.58
9.58

9.66
9.73
9.88

10.10
10.03

9.95
10.01

9.96
9.95

10.11
10.03
10.16

10.14

10.15
10.22
10.17
10.05

9.75

8016

17

y)

18

G m
G m

Vnbsp;5
a

Vnbsp;5
a 4-
a

Vnbsp;5

Vnbsp;5

Vnbsp;5

G m
G

G t

19

20
21

c — 67
c — 55
c — 68

Vnbsp;4 e

34

gt;}

35

37

gt;)

38
40

43

jy

44

gt;}

45
48

02

/
00

c

G

m u

c — 16

a 57
V 4 e
47

/

v3 e

c —01

v2.5 e

43

c
V 1

42

-ocr page 68-

Date

Obs

1

1

local time

Estimate

M

1

April 18

S

c —57 a 25

9.69

jj

H

c —54 a 16

9.66

19

S

c — 60 a 24:

9.67

21

H

c — 67 a 13

9.58

22

c —66 a 04

9.54

11

S

a 21

9.66

25

11

a 33

9.78

11

H

a 09

9.54

29

1 S

a 04

9.49

11

H

a 00

9.45

30

1 s

a 10

9.55

11

H

a 05

9.50 1

May 1

S

a 15

9.60

9

H

a 19

9.64

11

S

a 21

9.72

July 10

H

c — 74 a 09

9.53

16

11

c — 72 a 04

9.51

25

S

c —39 a 21

9.76

11

H

c — 45 a 30

9.78

i

27

11

a 48

9.93

28

11

c —23 a 52

10.00

29

11

c 00 / 49

10.21

Aug. 1

S

c 26 /—26

10.45

11

H

c 05 / 27

10.34

4

11

c 03 / 33

10.30

8

11

c 06 / 37

10.30

14

11

c — 53 a 43

9.80

15

J1

c — 41 a 32

9.81

16

11

c—51 a 33

9.76

19 12.—

E

v5 c a4v

9.82

G

25

H

c — 32 36

9.87

27

11

c — 47 a 31

9.78

30

11

c - 51 a 39

9.79

Sept. 1

11

c — 44 a 32

9.79

4 11.

E

V 4 c V 6 e a6 V

10.02

G

6 15.

gt;1

v2 c v4 e

10.23

G

11

Sh

c —29 a 49

9.95

11

H

c —- 31 « 46

9.93

7

11

c 31 a 41

9.90

J. D.

G. M. T.

Remarks

see
page 76

M\'

8050.59
„ .59
51.61

53.58

54.59
.. .60
57.59
„ .60
61.59
„ .60
62.59
» .59
63.59
71.59
» .60

8133.91

39.89

48.87
„ .88
50.93

51.86

52.90
55.89
,, .89

58.88

62.87
68.92
69.81
70.92

73.5

79.80

81.89

84.91
86.79
89.4

91.6
„ .74
„ .81

92.81

9.60

9.57

9.58
9.49
9.45
9.57
9.69

9.45

9.40
9.36

9.46

9.41
9.51
9.55
9.63
9.44

9.42
9.67
9.69
9.84
9.91

10.12
10.36
10.25
10.21
10.21

9.71

9.72
9.67
9.62
9.78

9.69

9.70
9.70
9.82

10.03
9.86
9.84
9.81

27

-ocr page 69-

Date
local time

Sept. 7
10

23 11.
26 16.
29

Oct. 1
2 ■

E
Sh
H

E

N

E
N
E
N
H
E

j)

N

E

N

Sh

N

H

10
12

13nbsp;10.-

14

3)

15
17

19 10.-
10.6

20

))
21

gt;gt;
22

24

8.3
13.7
9.8
11.6

8.4
8.2
„ 8.7
25 8.3
27 10.0

27

28nbsp;12.7

Obs.

Sh
H
E

Sh
H
S

))
H

))
S

J J

H

S

gt;gt;

H

Estimate

a 38
a 54
V 5 e
V S e a 5 V
a 15
a 25
a
—04
« 14
a 17
« 26
« 17
a—02

53

a 23
a 17
« 18
a 22
« 31

a 31

V 4: C

«4-17
a 34:
a 36
a 40

V 4 e

b 4 v2.5 c

c2 V v3 e v4 f

J 3.5 y 1.5 c
c2 V v2 e v3 f

Vnbsp;= c 1nbsp;vie
c
03 / —43
c3 V v2 e v2 f [
c3 V V e vl f\\

c2.5v4f

Vnbsp;^ e vO.6 f c3 v\\

c 6 y 1.5 / I
c 39 / 00 i
fl.5v4g \\
c 51 / —12:

jC — 19

U — 16

\'v2c
\\v 4 c
I c — 55

C

c
c
c
c

-57
39
46
69
41
51
c — 57

-43

-26
-44
-48
-32

c
c
c
c

c2v

Remarks

see
page 43

g 1

9.95
10.04
10.18 G u
9.91 G
9.65
9.69
9.64 I

9.69nbsp;I
9.59 I

9.78nbsp;I
9.68
9.56

9.70nbsp;i

9.62

9.63
9.67
9.76

9.79
9.94 G m u
9.81

9.80
9.79
9.89

10.43
10.10 a1 be.5c
\\c4f5g2h
10.46 g 1
10.15
10.53 G
10.27 4\'
10.25
10.60
10.70IG !
10.48
10.72
10.67
10.65
10.88
10.65

J. D.
G. M. T.

8192.81
95.88
8208.4
11.6
14.71
.. .72
16.68
17.73
„ .73
18.70
„ .70
20.69

u -69
22.68
23.68
» .68

25.67
27.70
28.4

29.68
„ .68
30.67
32.76
34.4
„ .43

35.31
„ .56
36.37
.. .47
.. .69
37.31
39.30
„ .35
40.30
42.41
„ .70
43.52
.. .68

Remarks

see
page 76

M\'

9.86
9.95
9.98

9.71
9.56
9.60
9.55

9.60
9.50

9.69
9.59
9.47

9.61

9.53

9.54
9.58
9.67

9.70
9.74

9.72

9.71
9.70
9.80

10.23
10.10

10.26
10.15
10.33
10.27
110.16
10.40
:10.50
110.48
|10.52
10.67
10.56
ilO.88
ilO.56

-ocr page 70-

Date
local time

Remarks

see
page 43

J. D.

G. M. T.

Remarks

see
page 76

Obs.

Estimate

M

M\'

Oct. 29 10.2

30nbsp;13.0

31nbsp;10.8
Nov. 3

4 7.3
12.7
))

6nbsp;13.4

}} )gt;

7

8nbsp;13.4
11

14

15nbsp;8.1
17 10.4

19nbsp;7.9

20

23

25

26

28

gt;}

29

30
2

3

4

8.2
8.3
8.1

9.0

gt;)

7.6
9.3
6.2
9.3

Dec.

8 14.8
12 8.3

13nbsp;12.8

14

15nbsp;7.1
8.5

„ 11.5

18nbsp;13.0

19nbsp;7.7

Nnbsp;c5vl f

c2v4 f

Vnbsp;= c
c — 45 a 38
v4: c a4v

a2v4h
a 2.5 V 2.5 b

Vnbsp;= a
a 1 V 5 b

c —57 a 10

Vnbsp;1.5 a
c~84 a —10
c
— 60 a 06
c80 a—06
c
—80 a—04

aZ v2b
y 6 cnbsp;a4v

a 5 vl b
c — 62 a 11
c — 64
a 09
cnbsp;aQ V

h4:v3 c
v0.5cnbsp;v4ce

b2 V 3.5 c
b i vl.5 c
V = c vie V 4: f
vie
vie
vie V 4 e
v2 c V 5 e
c —
43 a
a2v2b

v5 c

a3 v3 b
c —74 «
a4 v3 b
v5 ca5v v4p v5d
a2v3.5b
a3.5 V 1.5 b
vQ c a4v v8 e v5 d

H

E
N
n
N
n

Sh

N

Sh

H

Sh

n

E

n

H

Sh

E

N

E

N

n

E

v4f
v4 f
V 5 f
42

a 4 V

10

Sh
N
E
n

Sh
n
E
V

E

f 8 g2 h

G m
M

G M 3\'

,, .55

53.62
54.55
„ .65
57.68
„ .69

60.63

61.33
63.39
65.32

66.64
„ .65
69.30

71.34

72.29
74.37
„ .37

75.27

76.35
78.22
79.34
80.61
84.61

88.30

89.52

90.65
91.29
,, .31
. .47

94.53

95.28

G M

G !

G
G

G
G

G m
G m

M d

g

10.69
10.46
10.31
9.82
9.87
9.50
9.58

9.37
9.43

9.62
9.24

9.38
9.58

9.42

9.43

9.63
9.76
9.73

9.60
9.58
9.97

10.07

10.31
9.96

10.16
10.35

10.32
10.32
10.22

9.85
9.56
9.82
9.58
9.53

9.61
9.89
9.50
9.67
9.82

8244.41
45.53
46.44
49.72
50.26
» .52
.. .52
52.55

10.69
10.46
10.31
9.73
9.67

9.50
9.41
9.37
9.26
9.53
9.24
9.29
9.49

9.33

9.34
9.46
9.56 I
9.56i

9.51nbsp;I
9.49;
9.77\'

i10.07i
!10.11
9.96
9.99
10.151
10.121
10.12
10.02i
9.76!
9. 56 I
9.62
9.41
9.44
9.44
9.69
9.55
9.69
9.62

m

G

-ocr page 71-

Date

Obs

1

Rem arks

local time

Estimate

M

see
page

43

Dec

19

Sh

c

— 57 a 15

9.64

20

yy

c -

— 71 a 12

9.56

21 9.7

E

v5 c a4:V

9.82

G

Sh

- 69 a 04

9.49

22

51

c

— 100 a 16

9.43

26 12.2

n

b 1 V 5 c

9.88

27 9.5

V = b

9.80

.. 11.8

V

aS v2.5 b

9.59

28 6.1

n

a 5 V 1 b

9.73

m d

h

t

„ 6.9

V

aS vl b

9.69

„ 15.0

n

b2 V 4 c

9.96

G

30 7.8

yy

6 3 y 3 c

10.04

N

b = c

9.78

,, 7.9

V

a2v3b

9.52

1

31 8.1

N

hi vQ c

9.84

m d

1909

Jan.

2 7.1

E

v2 c V 5 e

10.18

g M

u

6 7.7

yy

V 1

c V 5 e

10.23

G M

8 6.4

yy

c2

V V 4 e y 4 /

10.42

G m

„ 10.1

N

vie

10.23

M 3quot;

n

cl v2 f

10.41

M d

„ 12.6

V

cl v4f

10.39

M

9 6.0

E

c2v v2.5e v3f

10.51

g

!

„ 8.0

N

vl cl

10.23

c 4quot;

12 6.0

y y

c3v3 f

10.53

„ 12.1

V

cl v3.5 f

10.40

13 6.0

E

c 1

V v2 e v3 f

10.49

G

i 1

,, 13.5

N

c2.5v5f

10.46

m

15 7.1

V

b4: V 1.5 c

10.16

1

„ 8.6

N

vl cl

10.23

b h

n

c2v3f

10.44

b h

„ 11.5

N

v2 c

10.14

g

J J jy

n

bQ vl c

10.22

g

18 6.1

y y

b4.5 v2.5 c

10.12

» 6.7

V

a 3.5 V 1.5 b

9.67

20 6.2

n

bl V 5 c

9.88

1

„ 8.7

V

a 3.5 V I b

9.71

22

Sh

c —

-41 a IQ

9.73

-ocr page 72-

Date
local time

Jan. 23 6.6
,, 13.6

V
N
n

E

V

n

V

3 gt;

E
n
E

V
n

) gt;

V

n

V
n

V

25

27

28

Febr. 1

gt;gt;

5

10

24

gt;)
6.1

9.3
11.4

7.0
„ 10.7

26 10.9
„ 10.9
6.6
7.6

8.5

6.4
6.9

7.6

7.1
12.7
12.0

7.6
11.7

7.8
11.6
12.6

7.7
12.1

n

V
Sh

V
n

V
n

V
H
n

V

n

V
Sh

18
19

11 12.6
12 7.5
. 12.6
16 11.5
„ 12.6

17 10.2
12.0
9.4
8.7

9.0

Obs.

Estimate

a 4 w 2 J
v2 b

V = b
a6 V 1 b

V 5 c

m

G m

G m
m

G m

M

M

M

M

M

M
M

M

a3 V

a4 V 1.5 b
a2.5vlb
a 6 V 1 b
a 5 V 1 b
a 2.5
V 1.5 b
al V 2.5 b
vQ cnbsp;a4v

a 5.5 V 1.5 b
V 5 cnbsp;a5
V

al V 5 b ,
a4 v2.5 b
a2 v3 b
B 4.5 1.5 a
^5.5 vl a
a3v2b

Vnbsp;= a
a4 V 3 b ■
al V 4 b
a2v3b

a 4.5 V 0.5 b
a 3.5 y 1 b
c
—43 a 13
a4 v 1 b
b2v4.5c
a5 vl b
b3 v3 c

Vnbsp;= b

c — 29 «4-35
b3v2c

Vnbsp;^ b

bl.5v2c
b 4.5 V 1 c
b2v3 c
c — 19 a 31

Remarks

see
page 43

M

9.65
9.59
9.80
9.74
9.76
9.68
9.68
9.74
9.73
9.63
9.46
9.76
9.71

9.87
9.40
9.63
9.54
9.16
9.22
9.62
9.32
9.61
9.42
9.52
9.76

9.71
9.70

9.72
9.95
9.74

10.05
9.82

9.88
10.09

9.82
10.02
10.20
10.01
9.94

h 1 d u

)3 gt;} gt;)

m
G

J. D.

G. M. T.

9.66
9.59
9.63
9.57

9.56
9.70
9.70

9.57
9.56
9.65
9.51
9.56
9.54

9.67
9.47
9.46
9.37
9.27
9.32
9.45
9.40
9.44
9.49

I 9.57
: 9.59
9.72
! 9.61
I 9.73

9.78
9.75
9.88
9.82

9.79
9.92
9.82
9.97

10.03
9.96
9.85

10

8330.26
.. .56
„ .56
31.24
„ .35
» .46

32.28
„ .44
33.44
.. .44
34.26
„ .28
» .34
35.22
„ .27
„ .31

39.29
„ .52
43.49
44.31
„ .48
45.31

.47
46.51
48.31
.49
„ .67
49.51

50.30nbsp;I
„ .51 I
54.47 I

-51 :
.62 i
55.42
„ .49
56.38
57.35
.37
.74

Remarks

see
page 76

M\'

-ocr page 73-

Date
local time

Obs

Estimate

M

Remarks

see
page 43

i

J. D.

G. M. T.

M\'

Remarks

see
page 76

Febr. 20

11.9

V

b2.5 V 1.5 c

10.11

8358.48

10.04

21

8.2

n

b 4 v2 c

10.13

59.33

9.96

12.0

V

c 1 y 3.5 /

10.40

» .49

10.29

29

1 23

8.7

n

b 5 vO.5 c

10.25

61.35

10.08

i gt;gt;

10.4

V

V = c

10.29

,, .42

10.20

24

Sh

C — 04 a 45

10.06

62.59

9.97

y)

H

c — 07 a 44

10.04

,, .59

9.95

25

7.8

n

b 4 V 1 c

10.19

m

63.31

10.02

9.5

E

vBcv4ev2pa7v

10.16

G

„ .35

9.96

11.0

V

V — c

10.29

.. .45

10.20

H

c — 02 / — 33

10.28

„ .62

10.19

))

Sh

c —08 / —41

10.21

.62

10.12

26

1)

c 04 / — 18

10.38

64.69

10.29

I 27

H

c —24 a 59

10.03

65.61

9.94

March 1

Sh

c — 21 a 30

9.90

j

67.60

9.81

H

c — 40 a 37

9.84

„ .60

9.75

3

Sh

c — 60 « 00

9.55

69.61

9.46

6

c — 60 a 06

9.58

72.64

9.49

i

)gt;

H

c — 70 a 04

9.52

„ .64

9.43

i-j
t

9.4

N

V = a

9.37

M d

73.38

9.37 1

}}

gt;)

n

a2v2b

9.58

„ .38

9.41 I

10

Sh

c — 62 a -02

9.53

76.64

9.44 !

12

9.0

n

a4 vl b

9.71

b

78.37

9.54

13

Sh

c —73 r/—01

9.48

79.58

9.39

16

9.1

n

a 3 57 1.5 6

9.65

82.37

9.48

17

10.3

N

« 3.5 y 1.5 amp;

9.65

83.42

9.52

11

H

c — 52 a 04

9.61

„ .59

9.52

gt;)

j

Sh

c — 53 a 01

9.59

,, .59

9.50

18

i

H

c — 64 a 07

9.57

84.64

9.48

20

Sh

c — 58 a 18

9.65

86.70

9.56

23

9.4

E

v3 c v2 p vQ e aSv

10.14

G

89.35

9.94

25

Sh

c — 33 a 49

9.93

91.69

9.84

April 1

8.8

N

c3.5 v 0.5 /

10.70

G M

98.36

10.70

9.4

E

c3 V v2 e v3 f

10.56

G m

„ .36

10.36

H

c 49 / 05

10.72

„ .59

10.63

2

8.4

N

c2v2 f

10.53

G M

99.34

10.53

3

9.1

gt;}

f = v4g

10.77

G M

8400.35

10.77

u

i

ygt;

vl f v4 g

10.67

„ .35

10.67

} gt;

9.4

E :

cd V v2 e v3f

10.56

g m

„ .35

10.36

31

-ocr page 74-

Date
local time

April 3nbsp;10.3

4nbsp;8.5

5nbsp;8.2

6nbsp;8.4

7nbsp;8.7

8nbsp;8.4

gt;gt;nbsp;gt;)

10nbsp;8.8

8.4

9.1

11

13

14
23

May 6
July 17
19

Aug.

23nbsp;13.3

24nbsp;14.0
26 14.4
30 14.3

4nbsp;14.7

5nbsp;14.4

n
V
N
n
N

10 14.6

15 13.6
22 14.4

Sept.

V

N
gt;gt;

))

4

5
7

25 14.6

28nbsp;13.5

29nbsp;14.0

1nbsp;13.6

2nbsp;14.0

3nbsp;12.6
,, 13.9

14.9
13.8
14.3

Obs.

V

N

n
N
n

Sh
N
n
N
Sh
n

Sh

J}

H

1-)
N

Estimate

M

Remarks

see
page 43

1 J. D.
G. M. T.

M\'

Remarks

see
page 76

- /

10.78

8400.42

10.59

^ - /

10.76

G M

01.34

10.76

c2.5 y 1.5 /

10.59

G M

02.33

10.59

c2.5 y 2.5 /

10.53

G M

i 03.34

10.53

V = c

10.31

G

1 04.35

10.31

c2v2f

10.48

» .35

10.31

h 5 v \\ c

10.22

G

^ 05.34

10.22

C \\ V 4 f

110.36

1

[ „ .34

10.19

1

02 / —

39

10.27

„ .65

10.18

h2v4c

9.94

i 07.36

9.94

6 2.5 v2.5 c

10.05

1 ,, -36

9.88

V ^ h

9.76

1

08.37

9.76

-58 fl

08

9.60

10.61

9.51

h \\ c

9.92

11.34

9.75

-58 «

12

9.62

^ 20.59

9.53

a 41

: 9.86

1 33.60

9.77

-54 a

15

9.66

8505.89

9.57

i

■54 a

16

9.66

1 07.90

9.57

vl.5 c

10.18

t 1

11.55

10.18

b 5 vS c

10.10

t

12.57

10.10

b 4 V 4: c

10.03

t d

14.59

10.03

b 5 v2 c

10.171

d h

18.59

10.17 :

bS v5 c

9.97

M d

23.60

9.97^

b2 V 4 c

9.94

G M

24.59

9.94

b = V 5 c

9.82

G m

29.60

9.82

b = V 4 c

9.87

„ .60

9.70

b 1 v2.5 c

9.95

34.56

9.91

h4v3 c

10.07

1 41.59

10.07

\\ c

10.18

„ .59

10.01 :

b 4 v2 c

10.13 j

j

44.60

10.13! 1

c2v4j

10.46

M

47.55

10.46

c 1.5 y 3 /

10.46

M

48.57

10.46

c3vZ j

10.53 i

G M

51.56

10.53 1

V =/

10.76

M h

52.57

10.76 i

/3 vl g

11.16

53.51

10.91 1

fl v5g

10.83

M 1

» .57

10.83

/2.5 vl.5 g

11.04

m

54.61

11.04\' ;

fSvSg

10.98 1

55.56

10.98 ;

fSvlg

1

11.09 i

57.58

11.09

i

-ocr page 75-

Date
local time

Sept. 9 12.2
10 12.2
14 13.7

16nbsp;13.4

19nbsp;15.5

gt;gt; jgt;

20nbsp;13.3
22 12.9
24 13.7

Oct. 2

6nbsp;10.5
,, 10.8
„ 12.9

9 10.8
10 11.3

14nbsp;10.8
,, 12.7

15nbsp;11.3

17nbsp;11.4

18nbsp;14.4

21nbsp;11.1
„ 11.2

24nbsp;10.8

25nbsp;13.3
28 14.0

Nov. 2 9.0

5

6

7nbsp;13.9
„ 14.4

8nbsp;9.6

gt;}

9

10 12.5

Obs.

N
V
N

n
N
n

1)

Sh
E

V
N
n

V
N

V
N
E
N

V
N
n
N

E

Sh

V
N
n
N
n

Sh

V

Estimate

f^vSg
f3.5vl.5g
c3 /

h 4: v2 c

c 2 V
amp;2.5 c

Inbsp;h4v3 c

h 4 V 4 c
I b 4
V 4 c
I c -— 30nbsp; 36

\' V 2.5 e V 4 f, c2 V
c4vl f

Vnbsp;= c
cS
V 1.5 f

c 4 V 1 f
c2v3f
fl.5v2g
c 4 y 0.5 /
e2 Vnbsp;V = f

flv4g

Vnbsp;=f
clv3 f
clv3f

vie

c2 V
h
6 V 1 c
b4v3 c

c2 V
c

f

G m
G m
G
G

10

V 4 e
-98

35

c IS / —48
c 35
b 4 V 1 c
b 5 V 1 c
c 1
V
b 4.5 V 1.5 c

cl V

C 39 /
c3.5
V 1 f

Remarks

see
page 43

M

10.98
11.13
10.50
10.13
10.46

9.94
10.10
10.08
10.05
10.05
9.88
10.62
10.68
10.31
10.54
10.68
10.49

10.99
10.71
10.96i
10.85 I
10.76 I
10.42 I
10.41j
10.23
10.46
10.23
10.07
10.54

9.79
10.30
10.61
10.20
10.22
10.38
10.17
10.38
10.60
10.67

b

h
h
G
G
G

g

G m

G

m

m
m

M d
G m

J. D.

G. M. T.

8559.50
60.50
64.56

66.55
„ .55
69.64
„ .64

70.54
72.53

74.56

82.77
86.40
„ .44
„ .53
„ .53
89.44

90.46
94.43
„ .52

95.43

97.47
98.59

8601.45
„ .46

04.44
44

05.55

08.57
13.33

16.78
17.57
» .78
18.57
„ .59
„ .59
19.39

.39
20.61
21.51

Remarks

see
page 76

10.98:
10.89
10.50
10.13
10.29
9.94
9.93
9.91
9.88
9.88
j 9.79
I 10.42
I 10.51
10.31
10.37
I 10.51
I 10.49
I 10.77
I 10.71
i10.76i
10.851
10.76
I 10.42
I 10.30\'
I 10.23
110.29
110.23
10.07
110.34 12;36
9.70 13;32
10.21

35

10.52
10.12
10.22
10.211
10.17:

I 10.21

I 10.51

I 10.50:

M\'

-ocr page 76-

Date
local time

Obs. Estimate

1

M

Remarks

see
page 43

J. D.
G. M. T.

M\'

Remarks

see
page 76

Nov. 13 8.1

E

\\ vl e v3 f cii

; 10.73

• g

!

8624.30

10.53

„ 9.6

1 V

1 c5vl f

10.70

,, .38

10.53

„ 15.5

N

vO.5 f

10.72

G

,, .64

10.72

14 8.4

10.76

25.34

^10.76

15 12.3

i /2y5g

10.89

26.50

10.89

„ 12.9

V

1 ;2.5v2.5g

i 11.03

„ .52

10.80

17 8.7

! N

! f2 vi g

!10.91

G

28.35

j

10.91;

,, 13.8

V

f3.5v2g

i11.10

„ .56

10.86:

18 11.3

N

f3vSg

10.98

G

29.46

10.98

19 9.4

E

e5vf3vv=hv6g

11.09

g

30.35

10.89 ;

„ 12.6

V

/4.5 y 1.5 g

11.16

„ .51

10.91

„ 13.5

N

fdvlg

11.13

G

„ .55

11.13 :

20 8.5

V

\\ ^ = g

11.28

31.34

11.00 i

21 7.8

E

\\ / 5 V V ^ h V 5 g

11.14

g m

32.28

10.94

8.1

N

f5v2g

11.07

G m

„ .33

11.07

22 8.3

}}

f5v2g

11.07

G M

33.33

11.07

23

Sh

c 87 / 52

11.15

34.57

11.06 ;

25 7.9

N

/3.5 v2 g

11.04

M

36.32

11.04

30 9.4

)gt;

c2 v2 f

10.53

M

41.38

i

10.53 1

Dec. 3 8.4

)y

c3vif

10.50

44.34

10.50 1

5 7.3

E

c3 V v3 e

10.61

g

46.26

10.41 !

„ 8.1

N

vl.5 c

10.18

5^= ?

„ .33

10.18

i

J} )) \\

n

c3v2 f

10.51

0 .33

10.34

8 7.4 ;

E

c3 V vie V 5 f

10.58

G

49.27

10.38

„ 6.9

N

v3 c

10.05

,, .28

1

10.05 1

J}

n

V ^ c

10.29

„ .28

10.12

11 7.5 ;

E

c3 V v3 e

10.61

G!

52.27

110.41

24

12 14.7 i

n

V — c .

10.29

53.60

10.12 \'

13 11.6

))

h 6 V — c

10.27

54.47

10.10 1

14 14.1

E

civ v2 e V i f

10.68

G

55.55

10.48 1

23

15 14.1 I

N

V 1 c

10.23

h

56.58

10.23

1

J J })

n

c2 V

10.46

h

„ .58

10.29

16 14.0

N

V ^ c

10.31

h

57.57

10.31

18 14.5

cl.5vif

10.43

59.59

10.43

19 13.9

c3.5 7; 2.5 /

10.57

c

60.57

10.57 1

20 7.6

E

c6 v vie V if

10.73

G m

61.27

10.53 !

21 7.9 :

N

c2v2f

10.53

m

62.32

10.53! I

29 7.0 \'

E

vlf e2 V

10.92

G

70.25

10.72

30 6.3

i

}}

i

V = f e2 v hi V

11.01

g

71.22

1

10.81

-ocr page 77-

Date
local time

Obs.

Estimate

M

Remarks

see
page 43

J. D.
G. M. T.

M\'

Remarks
1 see
i page 76

1910

Jan. 3

12.6

N

c4vlf

10.67

h

8675.51

10.67

6

7. —

E

c3.5

V vie v2 /

10.75

g

78.2

10.55

1 8

7.1

N

c3.5 y 3.5 /

10.53

h

80.29

10.53

10

9.7

c4v3 f

10.57

82.40

10.57

a

11.

E

c3 V

v2 e V 4 f

10.65

g

-4

i 10.45

11

i _

10.—

3 3

c3 V

v3 e V 4 f

10.65 G

83.4

10.45

! 17

7.6

N

V 0.5 c

10.27

m

89.31

10.27

i

9.~

E

c3.5v v3e y5/: 10.62

G m

„ .3

10.42

1 22

10.2

N

c3 V 1.5 /

10.61

G M c

94.42

10.61

24

9.

E

c3 V

v2 e V 4 f

10.65

G m

96.3

10.45

29

11.- -

33

c 5 V

el V v2 f \\ 10.82

G ! m

8701.4

10.62

30

8.4

N

10.76

02.34

10.76

10.—

E

e2 V

v2 f

10.881

G

.. -4

10.68

Febr. 1

8.6

N

fl.5 V 4 g

10.88^

04.35

10.88

4

8.

E

e 4r V

flv v 3.5 g

11.06

g

07.3

10.86

6

9. —

3 3

e5 V

flv v3 g

11.13

g

09.3

10.93

7

8.—

3 3

e 5 V

/2 v v4 g

11.13iG

10.3

10.93

8

8.—

gt;3

/3 V

v 4 g V = h

11.Ill

G !

11.3

10.91

1

9

8.

33

gl V

74 V

11.37:G u

12.3

11.17

7.5

N

f 5 vl g

11.13

G

„ .30;

11.13

j

11

8.—

E

f3v

v2 g h3 v

11.23

G

14.3 1

11.03

12

7.—

3 3

f4v

v2 g h2 V

11.24

G

15.2

11.04

J J

7.1

N

f5vlg

11.13

„ .29

11.13

13

8.6

i

33 !

/5 vl g

11.13

16.35

11.13

18

i ^

8.5

33

y 4 /

V 1 c

10.29 jm

21.34

10.29

24

8.8

3 3

b 4v4 c

10.03i

GMd3\'=

27.36

10.03

f)

gt;)

n

V — c

10.29

33 33 33

„ .36 1

10.12

27

8.

E 1

Sh

N

civ

vie

10.42 G

30.3

10.22

14;25

28

March 1

7.5

c — 16 a 53
b 4 V 4: c

10.04\'
10.031

31.55
32.30

9.95
10.03

1

n ;

b5vlc

IO.21I

„ .30 !

10.04

1

10.—

E

v2 c

10.27iG u

„ .4

10.07

I 2

9.2

n

b 5 v2 c

10.15|

33.37

9.98

Sh

c — 23 « 42

9.95

» .71

9.86

3

8.2

n

V = c

10.29

34.33

10.12

4

7.6

3 3

v = c

10.291

35.31 :

10.12

5

j

8.1

N

V = c

10.3li

G

36.33

10.31

n

!

civ 1

10.38 G

„ .33

10.21

!

-ocr page 78-

Date
local time

March 6
8
10

Sh

E

Sh

N

E

N

E

N

E
N
n
N
n

))
E
n
N
E
N
E
N

11 8.~
13 7.8

))

11. -

15

7.6

9.—

20

8.0

22

8.1

23

7.7

26

8.1

9.—

27

8.4

29

8.1

gt;y

April 1

8.6

gt;gt;

9.--

2

9.3

3

8.5

4

10.--

gt;j

9.4

9

10.—

July 27 14.4 :

29

14.4 i

Aug. 9

14.4 i

10nbsp;13.8

11nbsp;14.2

13nbsp;13.7

14nbsp;13.8

15nbsp;13.4

16nbsp;14.2
19 15.5
21 14.8
29 14.1
31 14.4

1 12.2

Sept.

Estimate

/ — 42
/ — 33
a 34

V 1

a 48

G
G
G
G
h
h d
G
h
G

G m t
d
G
h

G

j c 4.5 I\' 0.5 /
i / I 7J e2 V hi V V 4 g
\\ c5v0.5/
t 3 V h2 V V 3 g
gl.5v3h
g 0.5 v2 h
gO.5
V 1.5 Ji
c 5
V 2/3.5 g
V e v3 f c4v
V = c
c2v3fnbsp;\\

v2 cnbsp;i

c2v3f I
h5 vl c \\

v3 c

M
m
c

V 4 p

v = c
be v2 c

v3 c

a8 V

b5v2c
V ^ cnbsp;V 5 e

a7 V 3.5 c
b 4 V 4 c
b 5 v2 c
b5 v2 c
b 4 v3 c

Vnbsp;0.5 c

Vnbsp;= c
c3.5 v2 f
c4vl.5f

c4v = f vl f

Vnbsp;= /

b 4 v2.5 c
b 2.5 V
2.5 c
bl v 4 c

Remarks
see

Obs.

M

c 17
c 16
c — 39

10.33
10.37
9.83
10.73
9.90

10.71
11.05

10.72
11.19
11.28

11.25

11.26
10.68

!I0.76
110.31
10.44

10.14
10,. 44
10.21

10.15
10.29
10.17

10.09
10.15
10.43
10.00
10.03
10.15
10.15
10.07
10.27
10.31
10.60
10.64
10.70
10.76

10.10
10.03

9.87

c4 V
c — 39

G

G
G
c

G m
G M
M
M

G M
G m

J. D.
G. M. T.

8737.59
39.67
41.85
42.3
,, .76
44.31
-4

46.31
.. -3

51.32

53.33
54.31

57.33
. .3

58.34
„ .34
60.33
„ .33

63.33
-3 i

64.38

65.34
66.4 i
„ .38 :
71.4 ;

8880.59 ■
82.59 i
93.59 J

94.57nbsp;^

95.58nbsp;•

97.56

98.57
99.55

8900.58
03.64
05.61

13.58

15.59
16.50

I Remarks
see
page 76

M\'

10.24
10.28

9.74
10.53
9.81

10.71
10.85

10.72
10.99
11.28

11.25
11.261
10.68
10.56!
10.31
10.27\'
10.14!
10.271
10.041

I 9.951
:10.12!
10.171
9.89
10.15
10.23
lO.OOi

lo.osi

10.15i
10.15^
10.07!
10.27!
10.311
10.60^
10.64
10.70
10.76
10.10
lo.os;

9.87!

15

15

16

17

18

18

-ocr page 79-

Date

Obs.

!

i Remarks

J. D.
G, M. T.

local time

Estimate

! ^

see
1 page 43

M\'

Sept. 7 11.4

n

V d a4 V 1 I

9.75

8922.47

9.58

8 12.

E

v4 c a6 I

H 9.98 iG

23.5

9.78

„11.4

n

a 3 V 1 h

9.69

1

„ .47

9.52

14 11.--

E

v3 c

10.11

IG u

29.4

9.91

15 11.0

N

V = ht V3 c

; 9.90

i
!

30.45

9.90

18 13.6

gt; gt;

b 3.5 V 2.5 c

10.08

M

33.56

10.08 i

20 13.4

)}

V = c

10.31

G M

35.55

10.31i

21 14.6

b 5 v2 c

ilO.15

G M

36.60

10.15 !

25 11.1

gt;gt;

V f

!I0.76

G m

40.45

10.76

26 15.9

gt;gt;

flv4g

10.85

g m

41.65

10.85

28 12.9

) J

c4v \\ f

ilO.67

43.53

10.67

30 12.8

J)

c3 v3 f

10.53

G

45.52

10.53

n

c3vl.5 f

10.54

G !

„ .52

10.37

Oct. 1 11.—

E

civ v3 e v3 f

10.63

1

46.4

10.431

^ „ 12.4

N

c3v3 f

10.53\'d

„ .51

10.531

2 15.3

i

cl.5v4f

10.43 G

47.63

10.43

n i

1

c3 v2 /

10.51

\\ 1

.. .63

10.34

6 11.4

N 1

b 4 V 4 c

10.03

j

51.47

10.03

n

be v2 c

10.17

.. .47

10.00

! 7 12.6

gt;)

be v2 c

10.17

52.51

10.oo;

9 13.5

E :

v3 c v3 p aS V

10.12

54.52

9.92|

12 13.0

N 1

b 4 V 5 c

10.00 b D

57.53

10.00

i gt;) J)

n i

b 4 v2 c

10.13 D

„ .53

9.96

13 11.3

N

b2 v4 c

9.94|G m w

58.46 1

9.94

gt;gt;

n

b4 vl.5 c

10.16

„ .46

9.99|

14 10.-

E

v3 c v3 p

10.10

G m i

59.4 \'

9.90

,, 14.1

N

b2 v3 c

9.98

G m 1

„ .58

9.98

n

b4 vl c

10.19

G m

„ .58

10.02

15 13.3

N 1

b3v4c

10.00

GMwdl

60.55 :

10.00

20 12.9

gt;y

b = V 5 c

9.82

G M d

65.53

9.82\'

22 11.6

b2 V 4 c

9.94

G M

67.47

9.94

23 13.6

h3 v3 c

10.03

m

68.55

10.03

24 10.5

h3v3 c

10.03

69.43

10.03

26 10.--

E 1

vie

10.31

g u

71.4

10.11

28 10.—

y.\'

C 1 t.\' V d

10.54

g

73.4

10.34

1 „ 9.7

N

b 4 v2.5 c

10.10

„ .40

10.10

30 10.

E

v2 c V = d

10.39

G u

75.4

10.19

Nov. 2 14.5

N

b 4 v2 c

10.13

G

78.59

10.13

}} })

n

V = c

10.29

G

,, .59

10.12

jRemarks

see
page 76

19

19

14

-ocr page 80-

Remarks

see
page 43

J.D.
G. M. T.

Remarks i

see
page 76 !

Obs.

Estimate

M

M\'

6

9.—

8

13.3

10

10.—

11

9.2

14

12.9

19

9.8

20

15.6

21

9.3

22

12.9

33

3 3

23

8.—

3 3

11.4

25

13.6

3

8.—-

4

13.6

7

13.4

))

33

9

14.8

11

13.3

13

13.7

18

7.6

19

14.1 i

20

7.—

21

12.7

24

7.3

25

7.—

26

8.2

3 3

33 \\

27

6.2 1

30

6.9

1

j

11.6

2

8.—1

33

E
N

9.—
7. —I
12.5 i

c2 V

vie

c3 V

vie

c3 V

be vl c
b3 v4 c
b2 v5 c

Vnbsp;- b

b2 V 4 c

Vnbsp;b

b4v2c
V 3.5 c v2 p
b4v3 c
b5v3c
v2.5 c v3 p c
b
4.5 y 1.5 c
b 5 vl.5 c
b4v3 c

Nov. 4 9.—

y 4 e 110.57
|10.22

Vnbsp;3 e !I0.67

10.22

Vnbsp;3 e\\l0.67

110.23
ilO.OO
I 9.92
: 9.76
I 9.96
\'9.76
10.13
a8 V ilO. 14
10.08
10.11
a1 V ^10.12
10.17

:io.i8

10.07
10.31

G
G
G
G
b
G
M

M c
GM3\'
G m
G m
G m
G

G m
G
G
b

m

Vnbsp;= c

1911
Jan.

lt;v 4 c
\\v 5 c
\\v3 c

G m
m d

^ V =

cl.5v 4 j

IlO

.43

m

c

c3v2 j

10

.58

M

c

/2.5 v2.5 g

10

.98

G

M

/2.5 v2 g

11

.00

M

= / e2 V y 4 g 11,

.07

G

/3 v2g

111.

.02

h

m

c4 v2 f

iio,

.61

V v3 e

|io.

67

b3 V 3.5 c

10.

01 1

V = c

10.

29 1

b 4 v2 c

10.

13 1

G

b2 V 4 c

9.

96

b3v4c ilO.Ol
v4p a6y;i0.00
a6 v\\ 9.93
v3 /) !10.10
7) 4 c i 10.00

8980.3

81.55

82.3

84.54

86.4

87.37
90.53
95.40
96.64

97.38

98.53
„ .53
99.3
.. -47

9001.56
09.3

10.56

13.55
,, .55
15.61

17.54

10.37
|l0.22
10.47
ilO.22
10.47
10.23
10.00
9.92
9.76
: 9.79
9.76
9.96
9.94

9.91
9.94

9.92
10.00
10.01
10.07
10.31
10.43
110.58
10.98
11.00
10.87

ill.02
10.61
10.47
10.01
10.12
9.96:
9.79

14

14

19.56
24.31
25.58
26.2
27.52
30.30
31.2
32.33
.. .33
33.25
36.28

9.84
9.80
9.73
9.90
10.00

14

38.47
39.3
41.3
46.2
.51

E

N
E
N
E
N

n
N
n
E
n

E
n

N

E
N
n

n
E

33

N

-ocr page 81-

Date
local time

j

Jan. 13

6.1

i 22

9.—

23

7.

27

8.

28

8.—

29

11.5

30

6.7

31

7. --

sgt;

7.2

Febr. 2

7.8

3

9.6

8

9.5

9

7.9

15

8. ■

8.3

19

9.6

gt; gt;

22

8.—

}}

7.9

gt;)

26

7.8

} .1

quot; 1

27

8.--

March 1

7.3

2

8. - -

3nbsp;10.—

4nbsp;8. —

5nbsp;8.—

„ 7.9
17 9.--

19nbsp;8.2

20nbsp;7.6

: „ 10.-
\' 22 8.5
24 10.—
27 10.—
29 7.9
April 1 10.—

N
E

n

3 gt;

E
n
E
n

N

gt;}

E
N

JI

n
E
N
n
N
n
E
N
E
gt;)
}!
J)

N
E
N
n

))
E
n
E

gt;)
n
E

v2
c3
c 1
V 1

c

b 4.5 v2 c
V4 c al v

b 1.5 V 5 c

V = b
b -- V 5 c
V 5 c a6 V v5 p
b3v3c
6 3 y 3.5 c
h3v2c
cnbsp;V 5 e

bS v3 c ,
b 5 vl.5 c

v2 c
cl v3.5 f
c3
V v3 e V 5 /
vie
v3 f
v2 f

G

vie
\\v 1 e
\\ el
V

el V flv

c3.5v2.5f 110.57
v2enbsp;c2wll0.67

C 4: V
c5 V

g

V 1 /!10.99
y 4 ^111.06

G
G
m
G

G t

10.05
10.13
10.21
10.11
10.16
9.93
9.89
10.00 h t
9.89 iG

G u

G
G

b4 v3.5 c
b 4 v2 c
b5 vl c

v3 c
b 4 vl.5 c

Vnbsp;5 cnbsp;a^v

Vnbsp;5 cnbsp;a5 v

h2v3c

Vnbsp;5 cnbsp;a5 V

Obs.

Estimate

10.14 I G
y 3 \'10.06 :G W
j 9.91IG
9.76 G
9,82 i G
9.92 iG

M
M

10.03
10.01 4
10.09
10.27
10.03
10.18
10.14
10.37
10.63
10.22
10.80
10.83

M

G

„ .29
70.28
71.39
76.39
77.32
83.3
.. .33
87.39
.. .39
90.3
„ .32
.32

94.32
„ .32
95.3

97.30

98.3

99.4
9100.3

01.3
. .32

13.3

15.33
,, .33

16.31
. .4

18.34

20.4
23.4

25.32
28.4

; Remarks
M i see
i page 43

J. D.
G.M. T.

M\'

b \\ V 5 c

V 4 e

b 5 v2 c
b 5 vl c

9.85 IGMdS.S\'^

9050

.24

9

.85

v2 p 10.20 G !

59

.3

10

.00

V 4/:10.63 g

60

.2

10

.43

£? ,10.52 IG

64

.3

10.

.32

y4^^10.42^g I

65

.3

10.

,22 1

IO.I5IG 1

66.

,47

9.

,98 1

10.21 G

67.

27 ^

10.

,04

a 7 tJ !10.09 ^G w

68.

2

9.

89

Remarks

see
page 76

9.97
9.86
9.74
9.76
9.82

9.72

9.90
10.01
10.09
10.07

10.03
10.01
10.14
10.20
j
10.43!
10.22!
10.60
10.63
10.79
10.86
10.57
10.47
10.05

9.96

10.04

9.91
9.99

9.73
9.69
9.83
9.69

11

20

-ocr page 82-

8.9

8.4

8.5
8.3

gt;! yy

13 8.6

15 8.8

„ 10.-
Jiily 27 14.2

29nbsp;14.0
Aug. 4 14.5

6nbsp;14.3

yy yy

7nbsp;14.4

8nbsp;14.4

9nbsp;14.2

11nbsp;14.3

12nbsp;13.7

13nbsp;13.4
17nbsp;14.8
20nbsp;13.5

yy yy

24nbsp;14.2

25nbsp;13.9

27nbsp;14.8

30nbsp;14.3
Sept. 21 12.0

yy yy

22nbsp;13.1

yy yy

23nbsp;13.2 I

26nbsp;11.0

28nbsp;12.4
Oct. 1 10.9

8nbsp;15.1

9nbsp;13.5

14nbsp;9.6
16 13.0

April 3

5

6
11

Estimate

b2 c
b2.5 v2 c
b3
V 2.5 c
bS v4 c
h 3 v2 c
b I V 4.5 c
6 3 w 3 c
V 0.5 c
v2 c vZ p a S V
b 1 V 5 c
bl v6 c
b4v2c
b3v3c

Vnbsp;1 c

Vnbsp;= c
c2 v4 /
cS v2 /

c 6 V 0.5 /
- /

^ - /
c 3 t; 2 /
b 1 V 4 c
b2v2 c

Vnbsp;= b

aZ vZ b
aZ v2b
a 2.5 v3 b
b3 v2.5 c

Vnbsp;= c
b 5 v2 c

b 5.5 V 1.5 c
,, ^ b 5.5 V
0.5 c
E \\ v2 c v2 d a7 v\\
b2v3c
bl v4.5 c
a3 vl b
a2 V 1.5 b
cnbsp;a4v^

Vnbsp;= bnbsp;\'

Obs.

n
N

y 3

n
N

u

n
E
N

n

N

n

yy
yy
yy
yy

N
n
N
n

n

E

n

Remarks

see
page 43

i10.00 G M
\'10.07 G m
10.06 G m
!10.00 G d
;10.09 G d
^ 9.86 G M
I 10.03
■ 10.25
I 10.16 G
i 9.85 d
1 9.84 G
10.13|d
10.03

10.2o:

i10.31;
10.46iM
110.58 M
I 10.73 G M
10.76 G M
10.76 G M
10.58 G m
9.87 d m c ?
10-05 ,, „ ,,
9.80
9.58
9.62
9.56 G
10.06
10.29|
10.15
10.19|
10.25
10.09ig
lO.OOj

9.89 G I
9.69 G M d ^
9.61 G M
9.85lG \'
9.80 m

M

J.D,
G. M. T.

9130.36
I 32.34
I 33.35
38.33
j ,, .33
I 40.35
42.36
„ .36
„ .4
9245.58

47.57
53.59
55.59
„ .59
56.59
57.59

58.58
60.58

61.56
62.55
66.61
69.55
„ .55

73.58

74.57

76.61

79.59
9301.49

„ .49

02.53
„ .53 I

03.54
06.42
08.51
11.45

18.62

19.55
24.36
26.53

Remarks
I see
\'page 76
I

M\'

9.83
I 9.90

!i0.06
10.00
I 9.92

9.86
110.03
10.08

9.96
9.85

9.84
10.13
10.03
10.03
:10.31
10.46
10.58
10.73
10.76
10.76
110.58 \'

9.87

9.88
I 9.63

9.41
9.45 ,
9.39
10.06
10.12
10.15
10.02
10.08 i

9.89
9.83
9.72:
9.52 :
9.44
9.65
9.63

21

-ocr page 83-

I Remarks
M j see
page 4.3

Date
local time

J. D.
G. M. T.

Remarks

see
page 76

Obs.

Estimate

M\'

18nbsp;9.3

„nbsp;14.2

20nbsp;13.6

23nbsp;9.1

24nbsp;11.8

gt;gt; gt;gt;

26 11.8

28 9.3
,, 13.0
31 9.0
,, 14.4

1 12.3

7

16
20
21

27
29
4
8
9
11

E

Dec.

7.9

9.3
9 13.2

12 15.8
8.1

8.4
8.8

24nbsp;13.6

25nbsp;8.8
8.8
9.6

12.5
9.2
8.6

13.6

N
n

14

15

E
n

E

7.3
8.5
.. 11.-
17 11.9
23 7.7

29nbsp;6.—

30nbsp;13.6

Oct.

E
n

E

N

n

N

n

E

N

E

N

n

N

n

N

E

n

) J

E

Nov.

cnbsp;a5v

b 4: V 2 c
h
5.5 vie
c v3 d a 8 V

Vnbsp;0.5 c
cl
V 4 f

v3 c

Vnbsp;~ c

Vnbsp;5 e

Vnbsp;5 e

V C

\\ cl V
c3 V

Vnbsp;2 c
civ

Vnbsp;2 c

Vnbsp;= c
h2 v3 c

cnbsp;aQv

oi3vlb
a 3.5 vlb ■
v5 cnbsp;a5
V

cnbsp;a5 V

a 5 y 0.5 b
\\ h2 v2 c

b2.5v2.5c
\\v 4 cnbsp;a8v

Inbsp;v3 c

\'lt; b 4 v2 c
Inbsp;c2 v4 f

I t\' 1 c
b3v2c
b3vlc
b3 v I.b c
b2v2 c
^ 5 cnbsp;a6v

h 0.5 V 4 c \\

y = 6 ? I

a3 Vnbsp;V 5 c\\

V ^ anbsp;i

9.85

10.13
10.21
10.12
10.27

! 10.36
10.05
10.29
10.45
10.31
10.54

10.14
10.38
10.14
10.29

9.98
9.901

9.69

9.70
9.85^
9.81
9.76

10.05
10.05
10.02
10.06:
10.13
10.41 I
10.20 I
10.091
10.171
10.131
10.05
9. 90
I
9.85 I
9.80 I
9.76\'
9.36

G

i

G
G

G m

G

G

m
m
G
! G
M

G m
G
gt;G

G
G

G u
G m u
M d
M

G M

m

m

G

M
M

c h d
G m
c m

9328.34
„ .58
30.56

33.34
34.48

.48
36.48
„ .48

38.35
„ .53
41.33
„ .59
„ .59
42.50

.50

46.32

48.35
50,54
53.65

57.30

61.31

62.36
65.56

66.36

68.33

70.37
I 75.51

79.37
80.35
82.56
I
„ .56 I
85,29
I
86.35
„ .4
88.49
94.31
9400.2
01.56

I 9.65
; 9.96i
10.04;
9.92:
10.27
;10.19:
10.05
:10.12
10.25
10.31 j
10.34:
10.14
10.21
10.14
10.12
9.98
9.70

9.52

9.53
9.65
9.61
9.59
9.88;
9.881
9.82
9.86\'
9.961

10.24
10.03
10.09
10.00
9.96
9.88
9.70^
9.68
9.63
9.56
9.19

14

-ocr page 84-

Date
local time

Obs

Estimate

I
1

j M

Remarks

see
page 43

1 J. D.

1 G. M. T,

M\'

Remarks

see
page 76 i

1912

1

1

Jan. 6

6.8

E

\\v3 c a8 I

\' 10.08

\'1 g

19408.24

9.88

14

7

9.5

n

h4:v2c

10.13

1 G

09.38

i

9.96

8

8.3

E

\\ V 4. c v3 p a8 V

\' 10.07

G

^ 10.30

9.87

14

14

5.9

n

i c2v3f

110.44

16.24

10.27;

15

8.1

E

\\v2 e v3 f c4v

i10.72

\' G

17.29

10.52

17

6.8

yy

\' v2e f c4 wi 10.74

G

19.24

10.54

gt;gt;

6.8

n

I c4v3 f

10.50

b

,, .27

10.33 j

18

6.2

E

i v2 e vS f c5 V

10.75

G

20.22

10.55

22

7.4

yy

w = c v2 p

10.28

G

24.27

10.08

26

7.3

n

V ^ b

9.80

G m

28.29

9.63 i

27

7.0

i

yy

aS v2 b

9.62

G m

29.28

1

9.45

8.0

E

V 5 c V lt;6 p a 5 V

9.86

i G m

„ .29

!

9.66

28

12.3

n

a 2.5 v2.5 b

9.58

m

30.50

9.41

Febr. 2

6.9

yy

a2v2b

9.58

1 G M

, 35.28

9.41

4

7.6

yy

a3.5vlb

i 9.70

1 M h

37.31

9.53

5

7.3

E

\\v 5 c a1 V vQ p

9.92

g

1 38.26

9.72

7

7.6

n

b0.5v5c

9.84

i 40.31

i

9.67 \'

8

7.0

n

b2 V 5 c

9.94

b

41.28

!

9.77 ^

9

7.0

yy

b3 v4 c

10.01

42.28

9.84

10

9.8

yy

b2.5 v2.5 c

10.05

^ h

43.40

1

9.88:

11

11.7

} y

b 4 v2 c

10.13

44.48

9.96

12

10.4

yy

h4v2.5 c

10.10

45.42

j

9.93 !

14

9.7

E

v3 c

10.06

b c u

! 47.36

j

9.86 ^

18

9.4

yy

v2 c v3 p a 10 V

10.17

G

51.35

9.97

14;27 :

21

7.4

1

N

vO.5 c

10.27

G m

54.30

10.27

Marchs

1

y} 1

7.5

n

y)

c2v3 f
b2.5 v2.5 c

10.44
10.05

G m
M

„ .30
65.30

10.27^

i 9.88: ll

6

7.2 1

yy

b \\ V 4 c

9.90

G

68.29

9.731

7

7.3

yy j

a4v\\b

9.71

G

69.29

9.54\' J

10

7.8

yy

a2v2b

9.58

c

72.32

9.4F

12

8.1

E

V 5 c a5 V vQ p

9.86

G

74.29

9.66

17

9.4

^ i

bl v3 c

9.92

79.38

9.75

i

19

7.6

yy 1

bl V 4 c

9.90

81.31

9.73

21

8.2 1

yy

bl.5 v2 c

10.01

m

83.33

9.84

April 1

9.2

N

vie

10.22

G M ^

94.37

10.22

3

7.6

y gt;

V = c

10.31

G t

96.31 1

10.31

9

8.7

,) gt;

v = c

10.31

G

9502.35

10.31 1

10

8.4

i

y y

V 1.5 c

i

10.18

1

G

03.34 1

10.18!

j

i

-ocr page 85-

I Remarks
M j see
I page 4.3

Date
local time

J. D.

G. M. T.

Remarks

see
page 76

Obs.

Estimate

M\'

Aug.

gt;gt; gt;gt;

n

V = b

23 8.5

N

a3 V 1 b

25 8.5

) !

a2v2h

. 6 14.9

)gt;

bl c

9 14.7

n

a4v\\b

16 14.1

))

\\ a 4tv 1.5 b

18 14.3

gt;)

\\ v ^ b\'i a 3.5 vO.5 h

19 15.0

n

1 V ^ b

27 15.0

j a2 V

. 4 14.3

N

v2 c

12 12.7

) lt;

c3.5v2f

14 15.6

I vl.5 c

» ))

n

c2 V

15 13.0

■ N

V = c

n

cl V2 f

17 14.7

N

b 4 v3 c

n

i 5 57 1 C

19 12.9

1!

\\ b3vl.5 c,b3.5 v2 c

20 12.6

1)

h2 v2.5 c

21 11.2

1 E

vQ c a5v

„ 13.4

n

b2v3 c

22 14.2

a4vlb

24 12.8

\' 1 i

a2v2h

26 14.1

alv3h

27 13.5

11 j

via

2 12.2

i

V 1 a

3 13.3

: ) 1

V a

4 13.4

11

al.5v2h

5 12.8

1 )

a2v3h

7 11.3

quot;

a2.5 vl.5 b

8 10.3

E I

v5 c a 5 V

„ 11.8

n

a4:v0.5 b

9 13.6

11

v0.5b 1

10 13.8

V ^ b 1

12 15.3

gt;1

bl V 5 c

14 15.3

11

6 2.5 y 1.5 c

15 9.0

E 1

1

y 4 c a7 V v5 p

!

10.42
9.56
9.80
9.66
9.56
I 9.86
9.71
9.68
9.77
9.80
9.53
10.14
10.60
10.18
10.46
10.31
10.41
10.07 :
10.22
10.12 :
10.02
9.83 i
10.00 I

9.71 I
I 9.58;
\' 9.47!
9.27]
9.27|
9.36
9.55
9.54
9.64

9.87nbsp;,
9.75^
9.76!
9.80 I

9.88nbsp;I
10.11 I

10.00 I

G

Gnbsp;d

Gnbsp;d
m

Gmt d

mnbsp;D

mnbsp;d

h c ? b

M d
m h d

G
G

9503.34
14.35
» .35
16.34
18.34
9621.61
24.60

31.58

33.59
34.62
42.62
50.58

58.52
60.64
„ .64

61.53
„ .53

63.60
. -60 .
65.53 !
66.51
67.42
„ .55
68.58

70.53nbsp;;
72.58 i

73.55nbsp;I
78.50 I

79.54nbsp;I

80.55nbsp;I
81.53 ^
83.46 !
84.39

.48

85.56

86.56
88.63
90.63 !
91.33 !

10.25
9.56!
9.63
9.66
9.56
9.85
9.54
9.51
9.60
9.63
9.36
10.14
10.60
10.18
10.29
10.31
10.24
10.07
10.05
9.95
9.85
9.63
9.83
9.54
9.41
9.30
9.10
9.10
9.19
9.38
9.37
9.47
9.67

9.58

9.59
9.63
9.71
9.94
9.80

28

G c
G

M D
M D
G M
G m
m

G m

Oct.

G
G

G
G
G

L.

-ocr page 86-

Date

Obs.

Remarks

J. D.

G. M. T.

local time

Estimate

M

see
page 43

M\'

Oct. 15

14

.1

n

b3 v2 c

10.09

j

9691.58

9

.92;

17

12

.2

J J

b 5 V 1 c

10.21

93.50

10

.04|

}}

N

v3 c

10.05

i

„ .50

1 10

.05^

27

10

.6

JI5

\\ v b V 5 c

9.82

Mh d

9703.43

9

.82:

31

14

.6

n

a 4 V 1.5 b

9.68

m

07.60

9

.51 i

Nov. 3

8

.6

1

a3v2b

9.62

10.35

9

.45!

14

8

.1

\\ E

V 4 c aS V

10.03

iG

21.30

! 9

.83^

20

14

.0

i N

V 0.5 c

10.27

M c

27.58

10

.27

27

7

.2

; c5v0.5f

10.72

M h

34.29

10

.72

28

12

.5

gt;gt;

c5v2f

10.63

|M

35.51 :

10

.63

Dec. 2

7

.7

gt;)

V 2.5 c

10.10

39.31

10

. 10

!

1J

n

V 0.5 c

10.25

„ -31 !

10.

.08

3

7.

.2

gt; gt;

b 4 V 1 c

10.19

40.29 1

10,

,02i

5

7,

.7 1

jj

b2v2c

10.05

42.31 I

9,

,88

6

6,

.7

E

V 6 c a8 V

9.94

G w

43.24

9.

,74

9

7.

2

n

a4 vO.5 b v3.5 c

9.87

i 46.29

9.

,70

12

7.

5

gt;gt;

a3 v2h

9.62;

a5 b3c

49.30 ;

9.

,45

16

12.

7 !

))

a4 V 0.5 b V 4 c

9.84

m

53.52

9.

,67

18

12.

9

))

a3 V1 b a3 V 4 c

9.72

M

55.53

9.

55

25

13.

9

N

a3 v7 c V = b t

9.70

M d

62.57

9.

70

29

6.

9

n

bl v3 c

9.92

66.28

9.

75

30

6.

2

E

V 4 c a8 V

10.01

G i

67.22

9.

81:

7.

0

n

bl .5 v3 c

9.96

h

„ .28!

9.

791

Remarks

see
page 76

14

bZ v3 c
b 3 v2 c
6 2.5 v2 c

V 4 c
b3 v2 c

b3 v3 c
b2v3 c

b3v3c
b 3 v2 c
b 3 v2 c

V — c
v2.5 c

1913
Jan.

12.5
7.4
8.0

7.8
9.4

9.9
11.4

8.3
10.4

7.8

6.9
8.0

10.05
10.09
10.07

9.97
10.09

9.98
10.05
10.00
10.03
10.05
10.09

10.09
10.29

10.10

n

9.88
9.92
9.90
9.97
9.92
9.78
9.881
9.83
9.83
9.88;
9.92
9.92
10.12
10.10

N
n
E
n

) J

E
n

9

gt;gt;

10
15

24

25
28
31

Febr. 6

V 5 c

G

G m
G m
G M
c d

a 8 V

V 4 c

a8 V

14

N

71.51
72.30
76.32
„ .32
77.32
„ .35
78.40
83.47
92.30
93.42
96.32
99.28
9805.34
„ .34

-ocr page 87-

Date

local time

Ob

Febr. 8

6.8

N

I jgt;

yy

n

12

7.6

E

13

1

8.2

yy

14

10.9

N

18

8.2

Br

i

) gt;

8.3

B

19

7.0

N

20

7.1

N

9.4

B

21

6.9

N

gt;gt;

yj

n

9.2

Br

jj

9.1

B

22

7.4

n

i quot;

8.8

B

\' gt;

8.9

Br

23

7.6

n\'

24

7.7

y\'

1

8.9

B

26

9.0

9.2 1

Br

March 1

7.6 1

n

2

8.9 i

i

yy

11

9.0 i

B

))

9.1 i

Br

12

7.8 1

N

y)

yy i

n

18

9.8

B

yy

9.9

Br

19

7.8

N

23

8.5

yy

gt;)

yy ;

n

25

8.4

N

yy

8.9

B

gt;\'

9.3

Br

26

7.5

N

April 2

8.7

yy

yy

}y

n

Estimate

I . v2 c
civ

V 4 enbsp;c 4 y

v4 enbsp;c4:V

y 0.5 c
c2.5vnbsp;v3.5 f

c4vnbsp;v2 f

c2v2 j
c\\v2 f
k0.5ynbsp;v4.5j

Inbsp;v3 c

Inbsp;V ^ c

\\vl cnbsp;V4 f

\\v2 cnbsp;v4.j

6 5^1 c
v2.5cnbsp;v4.5/

v2 cnbsp;v4f

h 4 vl c
b 4 v2.5 c-
v3 cnbsp;v5 f

Vnbsp;5 cnbsp;vl f
v3 c vQ f

h2v3 c
h3v3c

Vnbsp;4 cnbsp;vl f
f 1.5 c V 4.5 /

bl.bv4c
b2 V 2.5 c
vienbsp;vl f

v2 cnbsp;v 5 f

b3v2c
y 1.5 c
civ
c3vlf
c5.5vnbsp;f3v

cQv e2 V f 4v
v^f
b3.5v3c
b3 V 1.5 c

! Remarks
M I see
! page 43

10.141
10.38
10.59iG
10.59
10.27

10.45
10.59
10.53

10.46
10.31

h u

b h

26

m c ? d

b u

M

31

10.05 G M
10.29 G M
10.27j
10.21

10.21nbsp;G

10.17

10.22
10.19
10.10
10.12

9.92
10.09
10.00

10.05
10.02
10.23

9.91
10.02
9.82

10.18
10.09
10.18
10.38 I
10.65;
10.89 Ih d
10.99|
10.76

10.06
10.13

J.D.
G.M. T.

Remarks

see
page 76

M\'

10.14|
10.21
10.39
10.391
10.27j
10.321
10.46i
10.53
10.46|

I 10.181

10.05!
10.12
i10.14i
10.08
I 10.04

10.04
10.091
10.021

9.93 i
9.991

9.79\'

9.96
i 9.83
9.88!
9.89
10.10!
9.91:
9.85
9.69

10.05
10.09
10.18
10.21
10.65
10.76
10.86
10.76

10.06
9.96

9807.27
.27

11.27
12.30
13.44
17.32
17.36

18.28

19.29
„ .37
20.28
„ .28
,, .36
.. -36

21.30
» .34

.35
22.30
23.30
„ .35

25.35
» .36
28.30

29.36
38.35
.. -36
39.32
„ .32
45.38
„ .39
46.32
50.34
„ .34

52.34
„ .35
,, .36
53.30

60.35
„ .35

G m
m

M b
M b
G M
G M
G M

-ocr page 88-

Date
local time

April 7 8.0

9nbsp;8.4

13nbsp;8.1

20nbsp;8.6

Aug. 14nbsp;15.1

/4 V

/3 V
vS f

gt;y

13.3

n

7

14.0

8

14.4

gt;)

9

15.5

))

12

14.8

gt;gt;

15

13.8

N

16

13.1

n

gt;!

N

19

13.5

))

23

10.5

E

V

24

13.6

N

n

25

13.0

))

))

N

26

12.8

gt;gt; \\

n i

27

10.5

E

V

gt;)

14.5

N

28

13.2

29

11.8

1)

4 /

b 5 v2 c
cl.5v2 f
c2vl f
cl.5v4f
c2.5 v2.5 f
c 3 y 1 /

c3 y 3 /
c2v2f
c3 y 3 /

22 14.4

24nbsp;14.4

25nbsp;13.1

26nbsp;13.7

27nbsp;11.1

28nbsp;13.0

29nbsp;15.0

30nbsp;11.3
„ 14.5

Sept. 4 11.1
„ 14.1
6

Obs.

b 2 v2 c
b2 V 4 c
b2.5 vi c
bSvSc
b4: V 2.5 c
civ

c4 vl.5 f
fl v3g
/0.5 v2.5 g
fSvl g

g 1 V 1 h
v 0.5 g

f4vlg

c3.5 v2 f

vie
c2v2f

V = c
hQvl c
bQvlc
bQ vl.5 c
6 3 t\' 3 c
b2vlc
b3 vZ c
63 y 3 c

n
N

N
n

N

E

N
gt;}

E

N
E
N

-ocr page 89-

Date
local time

Sept. 30 14.1
Oct. 3 13.5
5 9.5
9 9.2
„ 14.4

16 11.9

19 14.6

25nbsp;11.2

}}

26nbsp;14.5
quot;
gt;gt;

28 13.3

gt;y J)

Nov. 3 13.7

5nbsp;8.5

6nbsp;14.8
11nbsp;13.6
13nbsp;14.2
18nbsp;6.5

13.3
20 9.4

22 11.7

gt;gt;

24 7.2

Dec. 1 11.8

quot; }}

6nbsp;9.0

7nbsp;13.6

18 8.2
» 8.9

jgt; )gt;

19nbsp;8.7

20nbsp;8.0
24 13.3
26 6.4

Estimate

N I . c 3.5 v2 f
c3
V 1.5 f
\\vl e c4: V v4: f
\\v3.5 enbsp;c3 V

vie
I cl v3 f
h4v3 c
h4v2 c
Inbsp;h5v3 c

Vnbsp;= c

Vnbsp;^ c
h5 v3 c

vie
cl.5v2 f
c2 V I / \'
v — c
v2.5 e v3 f c4:V
cBvSf
f2 vlg .
\'f 3 vlg
V = enbsp;V = f

Vnbsp;= /

v2 e v3 f c4v
c 3 w 1 /
c2 v2.5 f
v 4r e V 5 f c 4 V
h5 v2 c
civ

Vnbsp;= c
b 4 V 0.5 c

b3v3c
v3 e V 4 f c4v

Vnbsp;= c
cl v2 f
c2v2 f

Obs.

M

10.60
10.61
10.68
10.57
10.23
10.38
110.07
10.13
10.10
10.29
10.29
10.10
10.22
10.45
10.54
10.31
10.66!
10.53
11.05
11.09
10.88
10.76
10.68
|10.57
110.51
\'10.58
10.15
10.38
10.29
10.24
10.03
10.63
10.31
10.41

10.48
10.31
10.53

10.49nbsp;^
10.83
I

E

jy

N
n
N

yy

n
N

n

yy

N
E
N

E
N
E
n
N
E
N
n

yy

N
E
N
n

gt;y

N

Vnbsp;^ c

yj

E

c3 v3 f
c2v3 f \\
V e v2 f cS v\\

Remarks

see
page 43

G

G 1
G
G
G

M d
M d
d
d
G
G

G
G
G
b

G M

M B

G W

m

G

G

G

G

G

G

M

G
G
G

G

J. D.
G. M. T.

0041.58
44.55
46.35
50.34
.. .59
„ .59
57.49
60.60
66.46
» .46

67.60
„ .60

69.55
„ .55

75.56
„ .56
77.31

78.61

83.55
85.58
90.23
.. .55
92.35
94.48
,, .48
96.26

0103.48
.. .48
08.37

09.56
,, .56
20.30
„ .36
,, .36
21.35
„ .35
22.32
26.54
28.22

Remarks

see
page 76

M\'

10.60
10.61
|10.48
110.37
;10.23
110.21
i10.07
10.13

lio.io
10.12
10.12
10.10
10.22
10.28
|10.37
|10.31
10.46
|l0.53I
11.05
11.09 ;
10.68
10.76

10.48
10.40
10.51:

:10.38
!I0.15
10.21
10.12
110.07
10.03
10.43
10.31
10.24
10.31
10.31
10.53

10.49
10.63

14

-ocr page 90-

I JS

§ $ O
^ œ feiO

CM

Ph

S
«

ooooooooooooooooo

CM O co

lO

O O O

O O

O\'OOOOOOOiOOOO

O O co
œ co lO

«ot^t^iocaœi—((M^oo

CMgt;OiO(MCMCO-^COClt;|iOiCi

H

C» t- 00 O CM

co T^ lO »0

CM
CO

co
: co

co co

O

^^CMCOlOîOnbsp;OOO

-050000nbsp;-Or-i
clt;j
O

3nbsp;rO r^nbsp;gnbsp;®

ïï cn

Inbsp;S O

anbsp;œ M

Dnbsp;oä

O O

O O O O O O

m

O

O

lOi-HCOCOO^i—ICMUÏClt;IC0
OOOOOOOOOOO

t- co
iO lO

O O O

Glt;J I-H ïO lo lO

Si

co

ic

cn

S)

s
lo

co

co

co

1—1

co

co


lO

sgt;

O

co

O

O
PH

iq

CM

Si

lO

lO

lO

sgt;

»

(M

1—1

s.

d

Clt;l

rH

ïi

il

CM

d

—1

co

co

TH

iO

II

r-H

\'O

co

d

\'O

lo

S

CO

rJS

to

co

co
co

-O

co

CM

I-)

co

00

t--

lo

CM

r-i

QO

co

lo

io

1—i

lo

lO

ÏO

iO

Oi

CR

C51

lO

co

1—1

CM

CM

(M

O

O

O

O

O

O

O

O

O

O

O

O

O

O

O

1—1

1—1

rH

1—1

1—1

1—1

1—H

1—1

nH

I—1

1—i

Î5

CM

CM

r—1

00

fcuO

Si

co

r—1

CM

CM

CM

^

1—1

■O

O

Éi

Si

II

d

»O

co

»

Glt;J

CO

lO

lO

co

lo

d

\'O

1—i

\'O

lO

- ^nbsp;io

!M

G w

COOnbsp;Ol-CM ^rt^CO^^^rJ^O^OOOrH ^OÏTt^cOOOaO CMOOCOCS

i- W t- t- 00 O QC co ^ ^ OO co X oo\' t^ t^ ^ t^ O oei quot; oo\' ocJ oo\' t^ ^ O oo\' t^ 00

m
Xi
O

^ O

\' co

CM O CM co t--
-H CM (M

O
CO

: lo rH IC Ci

; O CM co
Ol lt;M CM

; CM O I—I co

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co

: co 00 CM igt;

r-l rH (M Clt;l

O
Oj

CJ

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p

ö

p-t c

Ci rt

CU

-ocr page 91-

Date
local time

Remarks

see
page 43

J. D.
G. M. T.

Remarks
! see
page 76

Obs.

Estimate

M

M\'

March 29 9.9
31 8.6

April

n

8.9
9.9
8.2
9.5

n

N

14 8.0
16 8.7

18nbsp;9.1

19nbsp;8.7

20nbsp;8.8
22nbsp;8.9

Aug. 2 14.5
4 14.9

gt;gt;nbsp;)}

11nbsp;14.6

12nbsp;13.6

13nbsp;14.0
17nbsp;14.2

19 14.1

gt;1
n

N

Sept.

13.8

3nbsp;14.5

4nbsp;13.8

6nbsp;14.0

7nbsp;13.4
9 13.2

15 13.9
20 12.8

22nbsp;14.0

23nbsp;15.5

24nbsp;14.4

gt;)

25nbsp;12.8
30 11.5

E

N

n.

N

E

N

n
N

i gt;
n
N

gt;1
) j

n

y 1

N

^^

3

4
6

12

c V 4: p a 15
b4 c
b 4 V 1 c
bZvScSf
c v4p «10
6 2.5 y 4 c
vie
civ
b 4 vl c
b 4 v2 c
cO.5 V
c3v3/
c2 v2 /
c I V3 f
c
3 3 /
b 4 v I c

Vnbsp;= c

Vnbsp;2.5 c
c3 v3 /■
c3v2 f

c3.5 v2 f
v2 c

Vnbsp;= c
b3 v2 c
b2 v2 c
b3vlc
b2 v2 c

b3 v2.5 c
b 4 v2.5
c
h4v2.5c
c2v2f
fl v2g
c2.5 vl.5 f
cl v3 f
vl.5 c

Vnbsp;= c

Vnbsp;^ c
bl.5 v2 c

b2v4c

10.20
10.10

10.19
10.06
10.12

9.97
10.22
10.38

10.20

10.13
110.33
10.53
10.53
10.42
10.53
10.19
10.29
10.10
10.53

10.58
10.60

10.14
10.29

10.09
10.05

10.17

10.05

10.06
10.10!

10.10nbsp;I

10.53 1
10.91

10.59
10.42

10.18
10.29
10.29
10.01

9.94

m
m

iG m d
g m
m

G t
\'G t d
IG t d
^bdl
it

IG1D4.5
G 1 d
G t
G t d
G t d
G m
G m
G m
G m
G m

G M
G M
G M d
G M d
M

M d
m b
G
G
G

G M
G M

0221.37

23.35
„ .35

26.36

27.37
29.33
35.39
„ .39
37.33
39.35
„ .35
41.37

42.35

43.36
45.36

0347.59
49.61
„ .61
56.60

57.56

58.57

62.58
,, .58
64.58
77.57
79.60
80.57

. 82.57
83.55
I
85.54
91.57
96.52
98.57
99.64
0400.59
„ .59
01.52
06.47
„ .47

10.00
10.10
10.02
il0.06
9.92
9.97
10.22
10.21
10.20

10.13
10.16
10.53
10.53
10.42
10.53
10.02
10.12
10.10
10.53

10.58
10.60

10.14
10.12

9.92
9.88
10.00
9.88
10.06
10.10 I
10.10 j
10.53 I
10.91 I

10.59nbsp;!
10.42 I
10.18 ^
10.12
10.12

9.84
9.94

14

14

-ocr page 92-

Obs.

n

)gt;
}}

E
n

Date
local time

Oct. 6 13.9

11nbsp;12.9

12nbsp;13.0

13nbsp;9.-
Nov. 11 11.8

12 11.6
13 13.6

16nbsp;14.7

17nbsp;8.—

Estimate

b2v2c
b I v2 c
bl v2 c

v2 c
bl.5v2c
b2.5 v2.5 c
b3v2.5c
b3 v3 c

a 10 V

E V 4 c

Dec.

) )

13

.1

n

b3v3c

21

12

.3

gt;3

63 y 2.5 c

22

8

.3

gt; gt;

b3v2c

28

13

.1

N

\\ b3v3c

1

12

.8

b 4 v2 c

3

11

.2

b 5 vl.5 c

5

8,

.0

gt;gt;

V 1.5 c

10

6

.5

E

c 5 V V 2 e

14

8,

,4

n

b4v2 c

16

15.

.0

gt;gt;

63 y 2.5 c

20

7.

0

bl v3.5 c

21

10.

0

E

V 4 c (

14.

2 \'

n

bl V 4 c

24

12.

4

V ~ b

25

7.

5 :

\\

a6 vO.5 b

V5 f

M

Remarks

see
page 43

J. D.
G. M. T.

Remarks !

see
page 76

M\'

G M d
G m
m h
G c

0412.57
17.53
18.53
19.33
48.48
49.47
50.56

53.60

54.29
.. .53
58.50

59.33
65.55
68.52
70.45
72.32
77.23

81.34

83.61
87.28
88.37
„ .58
91.50

92.30

9.88
9.79

9.79
10.00

9.84
9.88
9.90
9.88
9.88
9.88
9.90
9.92
|10.03 !
Il0.13
il0.18 i
|10.18
ilO.45 \'

9.96
I 9.90 !
: 9.74 I

9.80nbsp;!
9.73 I
9.63 !
9.59

G

G
G

14

M d
G M d
G M

G

14

10.05
9.96
9.96
10.20
10.01
10.05
i10.07
10.05
10.08
: 10.05
10.07
10.09
10.03
10.13
10.18
10.18
10.65
10.13
10.07
9.91 m
10.00!
9.90\'
9.801 G
9.76 ! m

2

13.6

n

i b1 v2 c

9.96

M

D

jj

N

vlb

! 9.67

! M

D

8

10.5

n

b 4 V 2.5 c

110.10

i

11

9.1

jj

V = c

10.29

gt;gt;

}}

N

b3v3c

110.03

^ G

12

11.4

n :

bQ V 1.5 c

! 10.19

G

c

16

8.6

M

b 5 vl.5 c

10.18

gt;)

N

b 5 v2 c

10.15

17

8.

E

c2v v5 h

110.55

G

18

10.5

n 1

V = c

110.29

))

N ;

h5 v2 c

110.15Î

22

6.8

y) ;

b3v3 c

10.03

m

n

b 4vl c

10.19j

ni

1915
Jan.

0500.55
„ .55
06.42
09.36
„ .36
10.46
14.34
„ .34
15.29
16.42
» .42
20.27
„ .27

9.79
,9.67
\' 9.93
10.12
10.03
10.02
10.01
10.15
!10.35
10.12
10.15
10.03
10.02

22;26

-ocr page 93-

Date
local time

Obs.

Estimate

M

Remarks
see

page 43

Jan. 27

8.0

N

b 1 V 4 c

---—

9.87

G M d

29

10.1

n

V = h

9.80

M D

Febr. 4

8.1

6 3 w 3 c

10.05

5

10.9

h2v3c

10.00

6

11.

E

v5 c a5 V

9.87

G

8

7.9

n

b2.5 v3 c

10.02

11

12.4

gt;gt;

b2 vl.5 c

110.08

m c ? h

13

8.

E

V = c

10.34

b d

gt;;

10.2

n

b 4 V 1 c

10.19

15

10. -

E

V 5 c V 4 p alO V

10.07

g

16

7.0

n

b 5 Vl c

110.21 i

m

18

7.0

3)

6 4 w 0.5 c

To.24

G rn

21

7.6

N

V — c

10.31

m

25

7.6

yy

V =/

|l0.76

M

26

9.2

yy

c3v2f

10.58

M

28

7.4

})

cO.5 v3.5 f

110.37

M

March 1

9.4

yy

vie

10.22

G M

2

7.1

v2 c

10.14

M

!J

n ;

c2v •

10.46 i

M

8

8.9

ygt;

bl.5v3 c

9.96 :

20

7.4

yy

bl.5v2 c

10.01

m d j

21

7.3

yy

b2v3 c

10.00

G m 1

23

10.0 i

N ;

V = b

9.76 1

m d 1

26

9.0

yy 1

v = b 1

9.76 ;

GMD

28

7.7

n

b2v2 c

10.05 i

G M i

29

8.2

yy

V =■ c

10.29 !

M D

N

b 4v 4. c

10.03 1

M D

30

7.5

yy :

b3v3 c

10.03 i

G M d

31

7.7

yy

b 4 V 4 c

10.03 !

G M

gt;)

n

b3vlc

10.17 \'

G M !

April 4

7.7

N 1

b4 v2.5 c

10.09

d

7

8.1

yy

b5v2.5c

10.13

11

7.8

yy !

b 4 V 4 c

10.03 \'

G t d :

gt;!

n i

b2 vl.5 c

10.08 \'

G t d

14

8.4

i

quot; .1

b2v2c

10.05|1 d

J. D.
G. M. T.

Remarks

see
:\' page 76

M\'

0525.32

27.41
33.33
34.45

35.42

37.32
40.51

42.29
„ .42
44.37
45.28
47.28
50.31
54.31

55.37

57.30

58.38
59.28
.. .28
65.36
77.30

78.30
80.40
83.36

85.31

86.33
„ .33

87.30

88.31
„ .31

92.31

95.32
99.31
„ .31

9.87
9.63
^ 9.88

9.83
9.67
9.85
9.91

10.14
\'10.02

9.87
10.04
10.07

ao.3i
10.76
10.58
10.37
10.22
10.14
10.29
9.79

9.84
9.83
9.76
9.76

9.88
10.12
10.03
10.03
10.03
10.00
10.09
10.13
10.03

9.91
9.88

14

-ocr page 94-

REMARKS.

{j c stands for deviation from tiie light-curve. See p. 78).

1.nbsp;The two photometric measurements differ by O\'^.il.

2.nbsp;This value seems to be discordant. The curve gives 11\'quot;.04.

3.nbsp;Enebo\'s observations of J D 7611 and 7612 oblige us to draw the

curve at a distance of 0^^.20 above the photometric result 11.86
on J D 7614.

4.nbsp;Ten days later Haynes gave an estimate for the star\'s brightness of at

least 2\'M7 fainter than c, and at least r^79 fainter than /. This
would give the following result: JD 7686.6 var. lt; 12\'quot;.45; which
would be the lowest value recorded throughout the whole history
of the star\'s light-variation.

5.nbsp;The two photometric measurements differ by 0quot;\'.40.

6.nbsp;From lack of observations between J D 7837 and 7853, the intermediate

minimum on J D 7846 is uncertain both in time and brightness.

7.nbsp;In the observations grouped around the maximum on JD 7945,

a systematic difference L — E seems to prevail to an amount of
about 0
quot;.2, which causes an uncertainty as to the star\'s brightness
at this maximum.

8.nbsp;The curve shows a very steep rise to maximum brightness; the mean

increase per hour beingnbsp;The secondary curve in the descent

IS not established by a sufficient number of observations.

9.nbsp;The two photometric measurements differ by 0quot;\\46.

10. The secondary curve in the ascent, between the minimum on J D 8320
and the maximum on J D 8340, is established without ambiguity
by 14 points.

-ocr page 95-

11. Observation made with the 4i inch refractor; the reduction for the
3 inch being — 0\'M7, the reduction for the 4i inch has been taken,
somewhat arbitrarily, as —O\'^.IS.
12-13. These points lie 0\'quot;.45 below and 0\'quot;.32 above the curve, causing
an uncertainty in the position of the maximum on J D 8612.
14. The last estimate has been given half the weight of the other obser-
vations, in accordance with the observer\'s intention.
16. Discordant results. If / were to be read for c, and c for
a, the values
would become 10\'quot;.43 and 10quot;.50, in perfect agreement with those of
the other observers; though the photometric measurements would
in that case show differences of 0\'quot;.34 and 0™.48 respectively.

16.nbsp;The curve shows, after the minimum on J D 8752, a very steep rise

of 1\'^.04 in 5 days.

17.nbsp;This estimate has been reduced, as if it had been recorded as c 5 w 2 /;

c 5 V 5.5 g.

18.nbsp;For the magnitudes of the stars p and a, which have not been used

on other nights during this season, the mean values 10™.40 and
9\'quot;.38 (see p. 29) have been adopted.

19.nbsp;There would be a better agreement if for n we were to read N.

20.nbsp;The gap of 12 days, lying between this observation and the preceding

one, causes the minimum on J D 9105 to be only roughly deter-
minable.

21.nbsp;There are no observations to estabhsh with certainty the curve between

the maximum on J D 9279 and the minimum on J D 9301.

22.nbsp;For h the same magnitude has been adopted as was derived for the

season 1909—10; and to the last estimate half the weight has been
attached. Still, under the influence of this comparison star, the result

deviates from the light-curve by an

amount of 0quot;\\24.

23.

/J

c = 0\'quot;.21

28.

/ƒ c = 0™.26

33.

/I c =

.33

24.

J)

= 0. 22

29.

„ = 0. 27

34.

„ = 0.

40

25.

= 0. 23

30.

„ = 0. 29

35.

„ = 0.

42

26.

= 0. 24

31.

„ = 0. 30

27.

gt;gt;

= 0. 25

32.

„ - 0. 32

-ocr page 96-

CHAPTER IV.

The light-curve.

The values of the brightness of the variable, taken from the second
division of the hst given on pp. 44-75, were plotted on squared paper on a
scale of 1 mm. equalling 0.5 day and 0.01 magnitude; and a smooth curve was
drawn through the points. In connection with this curve the following
particulars should be noted: —

Total num_ber of pointsnbsp;1222

Number of points above the curvenbsp;595

below „nbsp;627

Recurrences of the sign of the deviationnbsp;592

.. .. .. „ „ .nbsp;629

Mean deviation of a point above the curve = 0™.057

^^ ... below „ ^^ = 0\'quot;,058

In a few cases the deviation of an observed brightness exceeded 0\'quot;.20-
these cases are particularly mentioned on pp. 76-77, which contain also the
remarks to which the process of curve-drawing gave rise.

The ordinates of the hght-curve were read off for each five days

(Greenwich mean noon), and the results are given in the first and third

columns of the hst on pp. 79-86. The dates of maximum and minimum

brightness are inserted, the phase in each case being indicated, in the second

column, by M and m respectively. The details of these phases will be given
later on.

-ocr page 97-

JD
241

phas(

M

corr

M\'

L

JD

phas(

ï M

corr

M\'

L

m

!

7455

10.45

— .31

10.14

46

7615

m

in

11.66

m

—.83

m

10.83

24

60

10.33

—.33

10.00

52

20

10.95

—.84

10.11

47

65

1

10.22

— .34

9.88

59

2\'5

10.73

—.85

9.88

59

68

M

10.20

— .35

9.85

60

30

M

10.69

—.87

9.82

62

70

10.21

—.36

9.85

60

35

10.73

.88

9.85

60

75

10.27

—.38

9.89

58

40

ilO.85

—.90

9.95

55

80

10.33

—.39

9.94

56

45

11.05

—.90

10.15

46

85

10.39

— .40

9.99

53

50

111.23

—.91

10.32

39

90

10.45

—. 42

10.03

51

53

m

:ii.28

— .91

10.37

37

95

10.48

—.43

10.05

50

55

11.25

— .92

10.33

39

96

m

10.48

— .43

10.05

50

60

10.83

— .92

9.91

57

7500

10.42

— .44

9.98

53

65

10.79

—.92

9.87

59

05

M

10.24

— .46

9.78

64

67

M

10.79

— .92

9.87

59

06

10.24

— .47

9.77

65

70

10.80

— .91

9.89

58

10

10.27

—.48

9.79

64

i 75

10.84

—.91

9.93

56

15

10.40

—.50

9.90

57

i 80

10.94

— .91

10.03

51

20

10.52

— .51

10.01

52

25

i

10.69

—.53

10.16

45

7785

9.90

— .57

9.33

97

30

10.82

—.55

10.27

41

88

: M

9.86

— .56

9.30

100

1 32

m

10.85

—.56

10.29 !

40

90

9.88

—.55

9.33

97

35

10.80

—.57

10.23

43

95

9.99

—.53

9.46

86

! 40

10.47

—. 59 1

9.88

59

7800

10.15

—.50

9.65

72

45

M

10.29

—.60 ■

9.69

70

05

1

10.35

—.47

9.88

59

48

10.27

—.61

9.66 1

72

1

1 50 1

10.28

.62 1

9.66 1

72

7825

M

10.29

— .34

9.95

55

55 1

10.39

—.64 :

9.75

66

30

10.35

—.32

10.03

51

1 60 i

10.57

—.65 i

9.92 1

56

35

10.47

— .30

10.17

45

I 65 1

10.72

—.67 \'

10.05

50

40

10.61

— .27

10.34

38

1 70

10.80

— .69

10.11

47

45

10.69

—.25

10.44

35

71

m

10.80

—.69

10.11

47

46

m

10.69

.24

10.45

35

75

10.76

— .70

10.06 i

50

50

10.64

—.22

10.42

36

80 i

M

10.66

—.72

9.94 i

55

55

10.45

— .19

10.26

41

84

10.64

—.73

9.91

57

60

10.13

.......-.17

9.96

54

85 1

10.65

—.74

9.91

57

65

9.93

—.15

9.78

64

90

10.70

—.76

9.94

55

70

M

9.89

— .13

9.76

66

95 i

10.83

— .78

10.05

50

75

9.99

—. 10

9 89

58

7600

10.98

— .79

10.19

44

80

10.21

— .08

10.13

46

05

11.10

— .80

10.30

40

7905

10.14

.03

10.17

45

10

11.29

—.82

10.47

34

i

08

M

10.12

.04

10.16

45

-ocr page 98-

J D phase

M

M\'

L

JD

corr

M

phase

M\'

L

corr

9.67

9.43

9.43

9.44
9.55
9.77

10.19
10.35
10.33
9.96
9.70
9.64
9.63
9.66 i
9.72 I
9.82
9.94 I

10.05nbsp;I

10.06
10.05 i

9.82 I
9.60 i
9.53
I
9.53 ^

9.57
9.75 I

10.14 I
10.59 \'
10.70
10.56 ;
9.65 .
9.32 \'
9.31
9.36

9.58
9.89

10.14
10.14

7910
15
20
25
30
35
40

45

46
50
55
60
65
67
70
72
75
80
85
90
95

8000
03
05
10
15

19

20
25
30
35

40

41
45
50
55
60
65
70

10.14
10.40
10.66
10.70
10.60
10.13
9.85
9.78
9.78
9.84
10.00
10.19

10.30

10.31
9.75
9.49
9.54
9.78
9.92 i

10.06 i
] 0.32
10.92
11.01
10.97
10.00
9.51
9.45 I

9.45nbsp;I

9.54nbsp;I
9.78

10.03

10.15

10.16
10.12

9.64
9.47
9.43

9.46

9.55

.05
.07
.09
i .10

I .12

1 .14
I .15
i .17
I .17
: .19
.21
j .22
i .23
.23
: . 24
.24
.25
.26
.27
.27
.28
.29
.30 I
.30 I
.31
.32
.33
.33
.33
.34
.35
.35
.35
.36
.36
.37
.37
.37
.37

10.19
10.47
10.75
10.80
10.72
10.27
10.00
9.95
9.95

10.03
10.21
10.41

10.53

10.54
9.99
9.73
9.79

10.04
10.19
10.33
10.60
11.21
11.31
11.27
10.31

9.83
9.78
9.78
9.87

10.12
10.38

10.50

10.51
10.48
10.00

9.84
9.80
9.83
9.92

44
34
26
25
27
41

52
55
55
51

43
36
32
32

53
67
64
51

44

39
30
17
16
16

40
61
64
64
59
47
37
33

33

34
52
61
63 i
61
56 !

8075

8135
37
40
45
50
55

59

60
65
70

75

76
80
85
90
95

8200
03
05
10
15 :
20
21
25
30
35
40
43 ,
45
50

55nbsp;!

56nbsp;I
60
65
70

75nbsp;\'

76nbsp;i

.37

.39
.39
, .39
.39
. 39
I .40
i .40
.40
. 40
.40
.40
.40
.40
.40
. 40
. 40
.40
.40

10.04

9.82

9.82

9.83
9.94

10.16
10.59
10.75
10.73
10.36
10.10
10.04
10.03
10.06
10.12
10.22
10.34

10.45

10.46

51

62
62
61
55
45
30
26
27
38
48
51

51

50
47
43
38
35

34

35
43

52
56
56
54
46
32 I

21nbsp;I

19

22

51
69
69
66
54
41
32
32

m

M

i M

m

»e

m

M

M

m

.40 jlO.45
.40 ;i0.22

m

.40
.40
.40
.40
.40

10.00
9.93
9.93
9.97
10.15

M

M

•40110.54
.40 ilO.99

m

.40
.40
.39
.39
.39
.39
.39

11.10
10.96
10.04
9.71
9.70
9.75
9.97

m

M

.39 10.28

.39
.39

10.53
10.53

m

-ocr page 99-

M

9.96nbsp;I

9.57
9.49 I

9.49nbsp;i

9.50nbsp;1

9.58nbsp;i
9.72 I

9.97
10.24
10.41

9.84
9.66
9.47
9.35

9.44
9.70

9.86
10.04
10.15
10.14

I 9.51
9.43
9.43

9.45
9.56

9.87
10.27
10.66
10.67
10.23

JD

phase

M\'

L

JD

corr

phase

m

10.13
10.13
10.10

9.86
9.76
9.83
9.99

10.19
10.51
11.01
11.05
10.98
10.35
9.92
9.83
9.83

9.87
10.22
10.59
10.77

10.77
10.59
10.21

9.94
9.91
9.94
10 32
110.72
\'10.97
11.07
11.06

10.78
10.36
10.19
10.18
10.25
10.46
10.72 i-
10.80 -

8280
85
90
92
95
8300
05
10
15
20
25
30
35
40
45
50
55
60

64

65
70

75

76
80
85
90
95

8400
01
05
10

15

16
20
25
30

8505
10

.39
.39
.39
.39
.39
.38
.38
.38
.38
.38
.38
4- .38
.37
.37
.37
.36
.36
.35
.34
.34
.34
.34
4- .34
.33
.32
.31
.31
4 .30
.30
.29
.28
.27
.27
.26
.25
4- .24

10.35
9.96
9.88

9.88

9.89
9.96

10.10
10.35
10.62
10.79
10.22
10.04

9.84
9.72
9.81

10.06
10.22
10.39
10.49
10.48

9.85
9.77

9.77

9.78
9.88

10.18
10.58

10.96

10.97
10.52

9.91
9.77
9.76

9.79
9.87
9.95

38
54
59
59
58
54
48
38
30
25
43
51
61
68
62
50

43
37

33

34
60
65
65

64
59

44

31
22
21

32
57

65

66
64
59
55

8515
16
20
25
30
35
40
45
50
55
57
60
65
70
75
77
80
85
90

95

96
8600

05
10
12
15
20
25
30

34

35
40
45

50

51
55
60
65
70

m

M

M

m.

m

M

M

m

m

M

M

m

m

9.63
9.50
9.49
9.53
9.62
9.71

M

M

4- .11
.10

9.67
10.10

71
48

m

9.56
10.00

M

corr

M\'

L

m

m

------

.09

10.22

: 43

.09

10.22

43

.08

10.18

45

4 .06

9.92

56

.06

9.82

62

4- .05

9.88

59

.03

10.02

51

.02

10.21

43 1

00

10.51

33

—.01

11.00

21

—.02

11.03

20

.03

10.95

22

— .04

10.31

39

—.05

9.87

59

— .06

9.77

65

— .07

9.76

66

—.08

9.79

64

— .09

10.13

46

—.10

10.49

33

— .12

10.65

29

—.12

10.65

29

— .14

10.45

35

— .15

10.06

50

— .16

9.78

64

— .17

9.74

67

— .18

9.76

66

—.19

10.13

46

— .20

10.52

33

— .21

10.76

26

—.22

10.85

24

-.22

10.84

24

-.23

10.55

32

-.24

10.12

47

-.25

9.94

56

-.26

9.92

57

-.27

9.98

54

-.28 ;

L0.18

45 1

-.29 ]

10.43

35

-.30 ]

1

[0.50

33

i

-ocr page 100-

JD

phas(

î M

corr

M\'

L

JD

phase

; M

corr

M\'

L

!

8675

m

10.68

1 m

- .31

m

10.37

37

8935

m

10.26

m
. 18

ioro8

49

80

i

10.52

.32

10.20

44

40

10.77

— .17

10.60

1 30

85

!

10.40

— .33

10.07

49

41

m

10.79

— .17

10.62

: 30

89

1 M

10.35

— .34

10.01

52

45

10.54

— .16

\'10.38

37

90

i

10.35

! .34

10.01

52

50

10.11

— .15

1 9.96

54

95

10.45

—.35

10.10

48

55

9.98

— .13

9.85

60

8700

i

10.63

—.35

10.28

41

60

i 9.94

— .12

9.82

62

05

10.85

— .36

10.49

33

63

M

1 9.94

— .12

9.82

62

10

11.05

.37

110.68

28

65

9.95

.10

9.85

60

12

m

11.09

— .37

10.72

27

70

10.00

.09

9.91

57

15

11.05

— .38

10.67

28

75

10.14

— .08

10.06

! 50

20

10.65

— .38

10.27

41

80

10.31

— .07

10.24

42

25

10.19

—.39

9.80

63

84

m

10.37

.06

10.31

39

30

9.99

— .39

9.60

76

85

10.36

— .06

10.30

40

32

M

9.98

— .39

9.59

77

90

10.11

— .05

10.06

50

35

10.08

-.40

9.68

70

95

9.88

— .04

9.84

61

40

10.40

—.40

10.00

52

9000

1 9.83

—.03

9.80

63

45

10.81

—.40

10.41

36

01

M

9.82

— .03

9.79

64

50

11.21

— .40

10.81

25

05

1

9.85

—.02

9.83

61

52

m

11.27

—.41

10.86

24

10

9.95

—.01

9.94

56

55

11.17

— .41

10.76

26

15

10.26

00

10.26

41

60

10.16

—.41

9.75

66

20

10.70

.02

10.72

27

64

M

10.05

—,41

9.64

73

25 i

11 .00

.03

11.03 1

20

65

10.05

—.41

9.64

73

26 ^

m !

11.02

.03

11.05

20

70

10.15

— .40

9.75

66

30
35

i

10.65
9.87

.04
.05

10.69
9.92

28
56 1

8880

M

10.00

—.29

9.71

69

40

(

9.78

.06

9.84

61 \'

82

9.99

—.28

9.71

69

41

M

9.78

.06

9.84

61 !

85

10.00

— .28

9.72

68

45

9.81

.07 1

9.88

59 1

90

10.04

— .27

9.77

65

50

9.90

.08 1

9.98

53 :

95

10.15

— .26

9.89

58

55

10.05

.09 1

10.14

46

8900

10.50

—.25

10.25

42

60

10.27

.10 i

10.37

37

05

m

10.75

— .24

10.51

33

62

m

10.31

.io!

10.41

36

10

10.41

— .23

10.18

44

65

10.20

.11

10.31

39

15

9.98

.22

9.76

65

70

9.84

.11

9.95

55

20

1

M

9.66

.21

9.45

87

75

9.75

.12

9.87

59

22

9.61

—.20

9.41

90

78

M

9.74

.12

9.86

60

25

9.66

— .20

9.46

86

80

9.75

.13

9.88

59

30

9.87

— .19

9.68

70

85

9.84

.14

9.98 ^

54 1

i

-ocr page 101-

phase

M\'

L

JD

corr

M

M\'

L

corr

9090
95
9100

05

06
10
15
20
25

9245
50
55
60
62
65
70
75

79

80
85
90
95

9300
01
05
10
15 !

19

20
25 I
30 I
35

40nbsp;!

I

41nbsp;I
45 i
50

54nbsp;i

55nbsp;I

10.01
10.25
10.66
10.84
10.84
10.70
10.10
9.75
9.67

9.82
9.90
10.10
10.72
10.77
10.72
10.13
9.45
9.40
9.40
9.48
9.75
10.04
10.15
10.15
10.03
9.73

9.51

9.45

9.46
9.60
9.90

10.18
10.26
10.26
10.13
9.58

9.52
9.52

.16
.17
.18
.18
.18
.19
.19
.20
.20

.31

.32
.32
.33
.33
.34
.34
.34
.35
.35
.35
.35
.35
.36
.36
.36
.36
.36
.36
.36
.36
.37
.37
.37
.37
.37
.37
.37
.37

10.17
10.42
10.84
11.02
11.02
10.89
10.29
9.95
9.87

10.13
10.22
10.42

11.05
11.10

11.06
10.47

9.79
9.75
9.75
9.83
10.10
10.39
10.51
10.51
10.39
10.09
9.87

9.81

9.82
9.96

10.27
10.55
10.63
10.63
10.50
9.95
9.89
9.89

45
36
24
20
20
23
40
55
59

46
43

36
20

19

20
34
64
66
66
61
48

37
33
33
37
48
59
63
62

54
41

32
29
29

33

55
58
58

9360
65
70
75

79

80
85
90
95
98

9400
05
10
15

19

20
25
30
32
35
40
45
50

54

55
60
65
70
73
75
80
85
90

9625
30
35
38
40

9.59
9.75
9.95
10.13
10.18

10.17
9.88
9.63
9.57
9.56
9.56
9.65
9.93

10.36
10.48
10.47
10.06
9.45
9 .39
9.42
9.70
9.96

10.18
10.27
10.27
10.12

9.85

9.50
9.47

9.51
9.72
9.89

10.04

9.78
9.57
9.42
9.40
9.42

.38
.38
.38
.38
.38
.39
.39
.39
.39
.39
.40
.40
.40
.40
.40
.40
.40
.40
.40
.40
.40
.40
.40
.40
.40
.40
.40
.40
.40
.40
.40
.40
.40

.40
.40
.40
.40
.39

9.97
10.13
10.33
10.51
10.56
10.56
10.27
10.02
9.96

9.95

9.96
10.05
10.33
10.76
10.88
10.87
10.46

9.85
9.79
9.82
10.10
10.36
10.58
10.67
10.67
10.52
10.25

9.90
9.87

9.91
10.12
10.29
10.44

10.18
9.97
9.82

9.80

9.81

54
46
39

33
31
31
41
51

54

55
55
50
39
26

23

24

34
60
64
62
48
38

31
28
28

32
42

58

59
57
47
40

35

44
54
62
63
62

m

m

M

m

m

M

M

m

m

M

M

m

M

M

-ocr page 102-

JD

phast

M

corr

M\'

L

JD

phasf

i M

corr

1 M\'

L

9645

m

9.63

m

.39

m

10.02

52

9805

m

10.11

m

.08

m

10.19

44

50

10.10

.38

10.48

34

10

10.28

.07

10.35

38

55

10.59

.38

10.97

22

15

10.46

.05

10.51

i 33

57

m

10.60

.37

10.97

22

17

m

10.49

4- .04

10.53

32

60

10.50

.37

10.87

24

20

10.25

4- .03

10.28

41

65

9.88

.37

10.25

42

25

9.88

.02

9.90

57 i

70

9.42

.36

9.78

64

30

9.84

.01

9.85

60 1

75

9.12

4- .35

9.47

85

i 33

M

9.83

1 00

9.83

61 1

77

M

9.10

.35

9.45

87

35

1 9.83

^ 00

9.83

! 61

80

9.25

.34

9.59

77

40

9.87

— .01

9.86

60 \'

85

9.61

.33

9.94

56

45

1 9.98

.02

9.96

54 1

90

9.89

.32

10.21

43

50

ilO.21

.03

10.18

45

94

m

10.01

.31

10.32

39

54

m

î10.76

.05

10.71

27

95

10.00

.31

10.31

40

55

10.72

—.05

10.67

28

9700

9.87

4- .30

10.17

45

60

10.04

— .06

9.98

53 !

05

9.59

.30

9.89

58

65

9.90

—.07

9.83

61

10

9.45

4- .29

9.74

67

11

M

9.45

4- .29

9.74

67

9995

10.15

—.21

9.94

^ 56 1

15

9.51

.28

9.79

64

242

20

9.73

4- .27

10.00

52

0000

10.27

—.22

10.05

50 i

25

10.08

.26

10.34

38

05

10.74

— .22

10.52

32 i

30

10.57

4- .25

10.82

25

08

m

11.22

— .22

11.00

21 II

33

m

10.73

.24

10.97

22

10

111.15

.22

10.93

22 II

35

10.70

4- .24

10.94

22

15

10.45

—.23

10.22

43

40

10.08

.23

10.31

40

20

10.08

—.23

9.85 j

60

45

9.67

.22

9.89

58

25

9.99

—.23

9.76

65

50

9.55

.21

9.76

65

26

M

, 9.99

—.23

9.76

65 1

52

M

9.55

4- .20

9.75

66

30

10.02

— .24

9.78

64 1

55

9.57

4- .19

9.76

65

35

10.28

— .24

10.04

51

60

9.64

4- .18

9.82

62

40

10.58

—.24

10.34

38

65

9.75

4- .17

9.92

56

42

m

10.61

—.24

10.37

37

70

9.87

4- .16

10.03

51

45 :

10.55

— .25

10.30

40

75

m

9.94

4- .15

10.09

48 i

50 i

10.26

—.25

10.01

52

80

9.82

4- .14

9.96

54

55

10.12

—.26

9.86

60

85

9.73

.13

9.86

60 1

60

10.07

— .26

9.81

63

87

M

9.72

4- .12

9.84

61

61

M

10.07

—.26

9.81

63

90

9.74

.11

9.85

60

65

10.09

.26

9.83

61 :

95

9.83

4- .10

9.93 !

56 j

70

10.19

.26

9.93

56 i

9800

9.95

.09

10.04 i

51

75

10.34

— .26

10.08

49

-ocr page 103-

JD

1

phas

e M

corr

M\'

1

L

JD

phas

e M

corr

M\'

L

0080

m

10.58

m

—.27

m

10.31

39

1

i 0350

m

ilO.12

m

— .15

m

9.97

54

85

11.10

—.27

10.83

24

55

10.47

—.15

10.32

39

86

i m

11.10

—.27

10.83

24

1 ^^

m

10.56

—.14

10.42

36

90

10.65

—.27

10.38

1 37

1 60

10.41

.13

10.28

41

95

10.36

—.27

10.09

! 48

65

1 9.98

.13

9.85

60

0100

10.20

— .28

9.92

56

70

9.91

.12

9.79

64

05

i M

10.11

—.28

9.83

61

73

M

9.90

—.12

9.78

64

10

10.08

—.28

9.80

63

75

9.91

—.11

9.80

63

15

10.13

—.28

9.85

60

1 80

9.95

.11

9.84

61

20

10.29

—.28

10.01

52

85

10.08

— .10

9.98

54

25

10.54

—.28

10.26

41

90

\'l0.40

.10

10.30

40

28

m

10.57

—.28

10.29

40

95

10.88

---09

10.79

25

30

10.56

— .28

10.28

41

! 96

m

10.91

— .08

10.83

24

35

10.26

— .28

9 .98

53 j

0400

10.25

— .08

10.17

45

40

i

10.09

—.28

9.81

63

05

9.92

—.07

9.85

60

45

M

10.06

—.28

9.78

64

10

9.83

— .07

9.76

65

46

10.06

—.28

9.78

64 1

15

9.81

— .06

9.75

66

50

10.07

— .28

9.79

64

18

M

9.80

.06

9.74

67

55

10.20

— .28

9.92

57

20

9.81

— .05

9.76

65

60

10.39

—.27

10.12

47

25

9.84

— .05

9.79

64

65

j

10.61

.27

10.34

38

67

I m

10.66

.27

10.39

37

0450

9.88

00

9.88

59

70

10.61

—.27

10.34

38

53

M

9.86

.01

9.87

59

75

M

10.09

—.27

9.82

62

55

9.87

.01

9.88

59

80

10.02

—.27

9.75 i

66

60

9.91

.02

9.93

56

85

10.10

—.27

9.83

61

65

9.99

.03

10.02

52

90

10.32

.27

10.05

50

70

10.14

.03

10.17

45

95

10.65

—.27

10.38

37

75

10.41

.04

10.45

35

0200

10.93

—.26

10.67

28

76

m

10.42

.04

10.46

34

Ol

m

10.95

— .26

10.69

28

80

10.12

.05

10.17

45

05

10.72

.26

10.46

34

85

9.79

.05

9.84

61

10

10.20

—.26

9.94

55

90

9.65

.06

9.71

69

15

10.07

— .26

9.81

63

93

M

9.62

.06

9.68

71

20

M

10.04

— .26

9.78

64

95

9.63

.07

9.70

69

22

10.04

—.26

9.78

64

0500

9.72

.08

9.80

63

25

10.04

—.25

9.79

64

05

9.94

.09

10.03

51

30

10.07

— .25

9.82

62

10

10.09

.10

10.19

44

35

10.15

—.25

9.90

57

14

m

10.12

.11

10.23

42

40

-- ____

10.31

—.25 ;

10.06

50

15

1

10.11

.11

10.22

43

-ocr page 104-

JD

phase

M

corr

M\'

L

JD

phase

M

corr

M\'

L

0520

m

10.01

4-

m
.12

m

10.13

46

0565

m

9.83

4-

m
.16

m

9.9^

53

25

9.82

H-

.13

9.95

55

70

9.78

.16

9.94

55

30

M

9.74

.14

9.88

59

74

M

9.77

4-

.16

9.93

56

31

9.73

.14

9.87

59

75

9.77

4-

.16

9.93

56

35

9.76

-h

.15

9.91

57

80

9.80

4-

.16

9.96

54

40

9.85

.16

10.01

52

85

9.95

4-

.16

10.11

47

45

10.05

.16

10.21

43

90

10.11

4-

.16

10.27

41

50

10.35

-h

.16

10.51

33

92

m

10.12

.16

10.28

41

54

m

10.66

-1-

.16

10.82

25

95

10.10

.16

10.26

41

55

10.65

.16

10.81

25

0600

9.92

.16

10.08

49

60

10.05

4-

.16

10.21

43

i

i

1

The hght-curve is of a very pecuhar form, and up to the present time
may be regarded as unique. The secondary variation, mentioned by
Enebo
(see p. 6), which in the following pages we shaU caU quot;the long periodicityquot;,
is of a very marked character; and round this quot;curved central hnequot; the prin-
cipal variation winds itself m a more or less regular fashion. The recurrence
of the maxima and minima, in periods practically amounting to 39 days,
(see p. 93) is to a certain extent regular. In fact, our first examination of the
curve exhibits this as its most regular phenomenon. All the other phenomena
seem to be irregular. The values of maximum and minimum brightness
fluctuate to such an extent, that (even after ehminating the long periodicity)
the least maximum brightness is equal to the greatest minimum brightness,
and the form of the curve between the principal phases is continually changing.
Moreover the maxima and minima (but especially the former) are sometimes
sharp, and at other times flat. The ascending as well as the descending branches
in some instances show a secondary curvature, displaying degenerated minima
or maxima.

It is obvious that the principal variation can be studied in detail the
better, after it has been freed from the long periodicity; this being a pheno-
menon which we shall have to consider as an isolated feature. Though this
long periodicity is more manifest in the maxima, a glance at the light-curve

-ocr page 105-

teaches us that the minima are affected by the same disturbance. This view
is supported by a consideration of the amphtudes. When we adopt, as the
amphtude of the hght-variation, the difference in brightness between a maximum
and the
preceding minimum, and plot its consecutive values {as is done in
Fig. 1) we at once remark that the amphtude is sensibly constant; and this

constancy may be considered as an indication that the long periodicity is
a phenomenon apart, affecting all the phases of the principal variation. We
have given on PI. II (a) the curve of the long periodicity as derived from the
observed maxima, which exhibit it better than the minima. This curve gives
us the means of quot;levelingquot; the observed hght-curve, i. e. of reducing it to a
horizontal central line. We have chosen for this purpose the line 9\'^.80;
and we have constructed a table which gives for each 5 days the amount
of the necessary reduction. This table is given in the fourth column of the hst
on pp. 79-86, and the reduced magnitudes are given in the next column.
For reasons which will be obvious, from considerations advanced in the fol-
lowing chapters, these reduced magnitudes are changed in the sixth column into
light-intensities, the brightest magnitude being equal to the hght-intensity 100.

The values of the fifth and sixth columns form what we shall call the
leveled light-curve. This hght-curve is given on PI. I; its ordinates are expressed
in intensities. It shows all the characteristics of the principal variation,
unaffected by the influence of the long periodicity. These characteristics may
once more be summarised under the following heads:

1. The successive maxima, as well as the successive minima, are for the
most part unequal, but they show now and then periods of approximate equality.
In the cases of inequahty of successive minima we may roughly speak of a
Lyrae type, though in fact only an irregular succession of principal and sec-

-ocr page 106-

. ondary minima is observed. In the case of equality we may roughly speak
of a C
Geminorum rather than of a «5 Cephei type, since the steep rise to
maximum, followed by a slow descent, which is an essential feature of the latter
kind of hght-variation, seems to be absent. The greatest likeness to the
Lyrae type is presented during the period marked ^^ on the Plate, and
again during the period marked whereas the ?
Geminorum type is best
represented during the period marked C.

2.nbsp;The order of succession of deep and shallow minima is frequently
reversed. Thus, for instance, the minima numbered 39, 64 and 69 in the hst
on
p. 92 are what the observers have called quot;principalquot; minima.

3.nbsp;The form of the ascending and descending branches varies frequent-
ly, and sometimes deviations in the ascending and descending processes have
been observed.

4.nbsp;The quot;durationquot; of a maximum or minimum is far from constant, and
as a rule that of the maximum is the longer.

All these characteristics suggest the existence of a com.pound variation,
with perhaps some fluctuations in the amphtudes of the components. If this
suggestion is right, the principal variation must have a period of about 39
days, and an amplitude much exceeding that of the other. In order to get an
idea of the period of the latter component, a series of about 16 compound
vibrations, as given by two tuning forks of different periods of vibration,
has been registered. To one of these forks was attached a sooted glass plate,
while the other one bore a metal pen. The result of this investigation was that
the combination of two periods, standing in the proportion of 1 to 1.4, gave a
curve which bore a strong resemblance to the observed light-curve, especially
in the way in which a
Lyrae\'\' type was changed into a Geminorumquot;
type, and in the different forms of the ascents and the descents. This proportion
would make the second period, if it existed at ah, about 54 days; and so it
was decided to undertake a search for a second periodicity.

In order to check the 39 days\' period, and the more problematical one
of 54 days, we have chosen to cover, in our search, the whole ground between
the extreme limits 35 and 60 days. The result of this investigation will be given
in chapter
VI.

-ocr page 107-

CHAPTER V.

The maxima and minima.

The fohowing pages contain a hst of the observed dates of maximum
brightness. The first column gives the number of the epoch, the second the
date, and the third the number of days elapsed between two consecutive
maxima. The fourth column contains the values 0-C, which result from a
comparison of the
observed dates of maximum with those calculated upon the
supposition of a constant mean period of 39.267 days (see p. 93). The last
column contains a few remarks in connection with the type of maximum, and
the degree of certainty with which it is given.

List of maxima.

E

JD

241

7468.0
7506.5
7548.0
7584.0
7630.0
7667.5
7788.0
7825.0
7870.0
7907.5
7945.5
7972.0
8019.0
8060.0

0
1
2

3

4

5
8
9

10
11
12

13

14

15

-ocr page 108-

E

JD

P

O-C

REMARKS

17

8137.5

d

d

—1.7

Uncertain

18

8176.0

38.5

—2.5

19

8221.0

45.0

3.2

20

8256.5

35.5

—0.5

21

8291.5

35.0

—4.8

22

8340.0

48.5

4.4

23

8375.5

35.5

0.7

24

8416.5

41.0

2.4

27

8530.0

—1.9

!

28

8576.5

46.5

5.3

29

8612.5

36.0

2.1

Uncertain. See Rem. 12—13 ]

30

8651.0

38.5

1.3

31

8689.5

38.5

0.5

Flat

32

8731.5

42.0

3.3

33

8764.5

33.0

—3.0

36

8882.5

—2.8

Uncertain. Very fiat

37

8922.5

40.0

i 2.1

38

8962.5

40.0

—1.3

Flat

39

9001.0

38.5

2.1

40

9041.0

40.0

—1.4

41

9077.5

36.5

—4.1

46

9279.0

1.0

47

9319.0

40.0

1.8

48

9354.5

35.5

—2.0

49

9398.5

44.0

2.7

Flat

50

9432.5

34.0

—2.5

Steep

51

9472.5 i

40.0

—1 .8

55

96:37.5 1

6.1

Not quite certain

56

9676.5 i

39.0

5.9

Very steep

57

9711.0

34.5

1.1

58

9751.5

40.5

2.3

59

9787.0

35.5

—1.4

60

9833.5

46.5

5.8

Very flat

242

65

0026.0

2.0

66

0061.5

35 5

—1.8

67

0110.0 i

48.5

7.4

68

0146.0

36.0

4.2

69

0180.0

34.0

—1.1

Not quite certain

-ocr page 109-

1

E

JD

P

0-C

REMARKS

70

0222.5

d

42.5

d

2.1

Very flat

74

0373.0

—4.4

Flat

75

0417.5

44.5

0.8

Flat

76

0453.0

35.5

3.0

Flat. Good

77

0493.0

40.0

—2.2

78

0531.0

38.0

—3.5

79

0574.0

43.0

0.2

Flat

If we are justified in considering the differences in the observed periods
as residuals from a mean period, this period and the date of a normal maximum
can easily be derived by the method of least squares. For this purpose the nor-
mal maximum was supposed to have occurred on
J D 8922.5 a; (E = 37),
and the mean period to be 39.286 y days. The observed maxima then
yielded 59 equations of condition.

Solving the normal equations we get

X = 2^06nbsp;y ^ 0^0013

Mean period = 39^2873 0^0199 (m.e.)

In the following pages the minima have been treated in the same way.

-ocr page 110-

List of minima.

JD

REMARKS

Very fiat

Not quite certain

Uncertain. Amplitude

Uncertain. See p. 76. Very steep

Good

Uncertain; nearest observations 9
before and 7\'^ after the minimum
phase.

Same uncertainty as above
Good

Very steep. Good
Good

Not quite certain
Steep. Good

Good

Steep. Good
Flat

Steep. Good

0-C

241

■quot; quot;quot; quot;

-1--

d

0

j 7496.0

1 d

1.7

1

1 7532.5

! 36.5

I —1.1

2

! 7571.0

38.5

1 —1.8

3

1 7615.0

1 44.0

2.9

4

1 7653.0

38.0

1.6

9

7846.0

1 —1.7

1

1

11

7925.0

—1.2

12

1 7966.5

! 41.5

1.0

13

8003.0

36.5

—1.8

14

8041.5

38.5

—2.5

17

1 8158.5

j

--3.3

18

8203.0

! 44.5

1 1.9

19

1 8243.0

40.0

2.6

20

8276.0

33.0

3.6

21

8320.0

44.0

1.1

22

8364.5

44.5

6.3

23

8401.0

1 36.5

3.6

26

8516.0

1

0.8

27

8557.5

41.5

i 3.0

28

1 8596.0

38.5

! 2.2

29

1 8634.0

\' 38.0

1.0

30

8670.0

36.0

2.3

31

8712.5

42.5

0.9

32

8752.5

40.0

1.7

36

8905.0 !

—2.9

37 1

8941.5

36.5

—5.7

38

8984.0 1

42.5

2.4

39

9026.5 1

42.5

0.8

40

9062.0

35.5

—3.0

41

9105.5 I

43.5 1

1.3

45

9262.5

1.2

46 i

9300.5

38.0

—0.1

47 1

9340.5

40.0

0.6

48

9379.0

38.5

—0.1

49

9419.0

40.0

0.6

Uncertain
Good

Very steep

Not quite certain
See Rem. 20 p. 77

-ocr page 111-

REMARKS

E

JD

O- C

Steep. Not quite certain
Steep. Good

Very flat. Amplitude 0™.20!
Good

Very steep

Very steep
Good

33.5
43.5
43.0
39.0
34.0

38.5

38.0
40.0
38.5

Not quite certain
Good

Very steep. Not quite certain

Flat

Good

d

35.5

37.5
39.0
41.5
42.0
37.0

d

-3.2
3.0
1.2
1.0
3.2
5.9
3.7

1.1
—4.7
—0.4
3.3
3.0
—2.2
—3.3
—4.1
—2.6
—3.9
—3.1
—3.9

50

55

56

57

58

59

60

64

65

66

67

68
69

73

74

76

77

78

79

9454.5

9657.0

9694.5

9733.5

9775.0

9817.0

9854.0

242

0008.5

0042.0

0085.5

0128.5

0167.5

0201.5

0357.5

0396.0

0476.0

0514.0

0554.0

0592.5

Supposing a normal minimum to have occurred on J D 8941.5 jt;
(E = 37), and the mean period to be 39.286 y days, we get 54 equations.
Solving the normal equations, we get

«- 5^68nbsp;.y=—0^0387.

Mean period = 39^2473 0^0181 (m. e.)

Taking the mean of this period, and of that resulting from the foregoing
consideration of the maxima, we get
39.267 days. Starting from the norm-
al dates of maximum and minimum, and using the mean period just
obtained, (which is compatible with the mean errors stated above), we
arrive at a list of calculated maxima and minima, which differ from
the observed phases by a number of
days given in the fourth columns of the
two preceding lists. In the next chapters we shall have occasion to see whether
the adoption of a mean period, as obtained above, is justified.

-ocr page 112-

CHAPTER VL
T
he Periodogram.

In the Monthly Notices of the R. A. S. Vols. LXXI p. 686 and LXXIV
p. 678, E. T. W hittaker and D. Gibb have given an account of the wav in
which they were able to undertake a search (within certain Hmits) for possible
periodicities in the light-variation of SS Cygni1). The method is a simphfication
of that frequently used by A.
Schuster in his search for periodicities in magne-
tic and solar phenomena.

When we wish to discover whether a periodicity of, say, 40 days is
quot;activequot; in a series of, say, 3200 values of a certain quantity, obtained at equal
mtervals of time, the method consists in writing these values down in rows
of 40, and taking the sum of the 80 values of each column. Suppose these sums
to be
5i, Sa, ... .5^0; then, according to Whittaker, the difference between
the greatest and smallest values of the quantities 5, measures the quot;activityquot;

of a 40 days\' period. Schuster analysed the whole sequence 5i......by

means of simple harmonics, and measured the same quot;activityquot; by a function
of the two coefficients.

The latter method is the more accurate, but the former, which is the
shorter, gives satisfactory results in cases where there are very pronounced
periodicities.

It is evident that, instead of taking the sums of the numbers of each
column, we may as well take their mean values; and where, as in the case of
R V Tauri, many gaps occur, we are even obliged to do so.

1nbsp; Another example is treated in detail by G. A. Carse and G. Shearer in no. 4 of the
Edinburgh Mathematical Tracts: quot;A course in Fourier\'s Analysis and Periodogram Analysis
for the Mathematical l.aboratoryquot; London 1915. G. Bell and Sons Ltd. This example is
apparently based upon a fictitious light-curve, which is to be regretted.

-ocr page 113-

39 i 40

35

36

37

38

41

42

43

44

45

46

47

47-51 43-53 45-49

61-66

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58-62

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51-56

49-55 49-54

48-52

47.8

47.9
47,7
47.7
48.0
47.6

47.6

47.7
47.7-
47.7

47.7

47.8
47.8
48.8
49.6

49.6

49.7

49.8

49.8

50.0

50.1
49.7

49.3

49.2

49.5

48.9

48.6
49.1

49.1

49.4

49.2
48.9

48.7
48.7
48.6
48.1
48.1

48.0

48.1
48.0
47.9
48.0

48.0

48.1
48.1

1
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U
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48.8
I 48.6
; 48.5
\' 49.1
49.2

48.8
48.6

48.2

47.9
48.4

48.1

48.4
48.6
48.9

49.6

49.5
49.4

49.4

49.5

49.3
48.5

48.2
47.9
47.8

47.8

47.7

47.9
48.0
48.2

48.4

48.7

48.8
49.0

48.9
48.8

47.3
47.6

48.1

48.2

48.3

48.4
49.0

49.0
49.3

49.6

49.8

50.3

50.4

50.2

50.3

50.2

50.3

50.1

50.3

50.2
50.1

49.7

49.4

48.9
48.6
47.9

47.5
46.9

46.8

46.3
46.0

46.6

47.0

47.1

47.2
47.0

49.2

49.3

49.1
49.3

49.3

49.8
49.6

49.9
49.6

49.2

49.6

49.7

49.0

48.8

48.4
48.2

47.9
47.6

47.2

47.1

46.8
46.6

46.5

46.6
47.6
48.0

48.6

48.7

48.9
49.4

49.3

49.2

49.3
49.2
48.6
48.9
49.0

45.4

45.4
45.9
46.2
46.7

47.1
47.6

48.0

48.2

48.3

48.5

49.1
49.5
49.9

50.5

50.6

50.7
51.5
51.3
51.1
51.3
51.1

50.7

50.8

50.7
50.3
50.3

49.9
49.5
48.9
48.5
47.9
47.3

46.8
46.3

45.9
45.7
45.3

40.2: 49.6
40.3| 49.6

49.2

49.4
49.6
49.6

49.6

49.5

49.6

49.7

49.8

49.7

49.5

49.6
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49.4

48.8
48.8

48.8

48.5
48,2

48.4
48 9

48.5
48.4

48.0

47.9
47.8
47,8
47.8

47.6

47.6
47.4

47.1

47.4

47.5

47.5

47.7

47.7

48.6

48.8

48.9
48.9

49.8
49.8
49.8

49.6
49.8

49.7

49.7

49.8

49.7

49.6

49.1

48.8

48.7

48.2
47.4

47.8
48.1
48.0

48.3

48.0
47.7

47.4

47.1

46.9

46.7

46.8

46.9
46.6

46.6

46.5
46.9
48.0

48.3

48.7

49.0

49.6

49.7
49.9

50.4
50.3

50.1
50.0

47.7
47.1
46.9

47.1

46.8

46.9

47.2
47.4

47.6

47.7

47.6

47.4

48.1
48.0

48.0

48.5

48.7
48.7
48.9
49.4

49.3

49.2

49.2

49.3

49.2

50.3
50.2

50.1

50.1
49.9

49.6

49.4

49.5
49.5

49.2
49.2
49.0
49.0

49.0
48.9

48.7
48.4

48.1

50.2
51.7

52.2

52.5
52.4

52.6
53.1

53.0
52.9

52.7
52.9
52.7
51.9

51.3

50.4

50.1

49.2

48.3

47.4

47.5
46.7

45.5
44 9

44.4
44.2
43.7

43.7

43.6
43.6
43.9

44.8
45.1
45.8

46.1
46.6

47.2
48.]

48.5
48.8
49.2

49.5

49.6
50.2
50.6

48.9
48.6
48.6

48.4

48.3

48.5

48.4
49.0
49.0

49.3

49.5

49.5

50.0

50.1

50.0

49.6
49.6

49.6
49.5

49.1

49.0

48.7
48.5

48.5

48.6

48.4

48.1

47.5
47.1

46.8

46.9
46.9
46.9

47.1

47.4

47.6
48.0

48.2

48.5
49.0
48.9

48.6
48.9
48.8
48.6
48.8

49.8
50.3
50.3

50.3

50.4

50.2
50.1
50.0
49.7

49.3

48.9
48.3

48.0

47.7

47.5

47.1

47.8

47.9
47.5

47.0
46.9

46.7

46.8
46.8
46.8

47.1
47.1
17.1

47.1
47.7
48.0
48.3

48.5
48.7

49.0

49.2

49.3
49.3

49.3
49.2

49.4

49.6

50.1

49.7

49.5
49.7
49.7

40.6

40.5

40.6

40.8

41.0

41.6

42.4

43.5

45.7

46.9

48.1

49.8

51.6

53.2

54.6
55.8

56.7

57.4

57.8
58.0

57.7

57.3

56.9

56.0

54.8
53.7

52.3

51.5

50.1

48.7
47.1

45.4

44.1

42.8

41.9

41.2

40.6

49.6
50.3
50.5
50.0
49.9
49.8

49.8

49.7

49.3
49.0

48.5
48.0

47.6
47.2

46.8
46 4

46.4

46.9

47.0

47.1

47.1

46.7

47.2

46.9

47.4

47.8

48.3

48.9
49.3
49.3
49.3
49.3

49.6

49.5
49.5

49.7

49.8
49.8

6.2 17.8

1.9

4.4

3.4

4.1

2.7

3.9

3.5

9.5

2.5

3.3

3.7

-ocr page 114-

48

45-47 43-47

49.3
49.1
48.6

48.71 48.3
48.8i 48.3
49.0 48.0

49.4

49.5

49.0

49.0

49.1

48.8
48.3

48.2
48.0

47.9
47.8

49.3 48.2

48.5

48.3
48.0
47.8

47.4
47.3

47.3

47.4

47.5

48.4
48.4

48.7

48.5
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48.6

48.6

48.7
48.5
48.5

48.4

48.5

49.8
49.7

49.7

49.6

49.5
49.3

49.6
49.1

49.8

47.8f 47.8
47.7| 48.2
47.91 48.4
47.9| 48.6
48.4! 48.6
48,4! 48.6

49.1
49.0

48 4; 48.7
48 4; 48.8

48 4

48.4

48.5

48.6
48.6
48.6

48.6

49.0
48.9

49.1

49.0

48.7

48.5

48.1
48.1
49.1

49.6
49.1
49.0
41-45 40-45

41-47

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48.8
48.5
48.7

45.5

45.0

44.6

44.3

44.7
44.5

44.8

45.4

45.9
46.4
46.9

47.4
47.8

48.1

48.5

48.7

49.2

49.8

50.6

51.3

51.7
52.0

52.4
52.7

52.5
52.0

51.9

51.7

51.6

51.8

51.7
51.5
51.0

51.5
51.4

50.9
50.2

49.6

49.4
49.0
49.0
48.0

47.5

46.8
46.5
46.2

45.7

47.9
48.4

49.1| 48.4
49.7\' 49.1
50.3, 49.7
50.5i 50.0
50.7; 50.3
50.7 50.3
50.31 50.1

50.1

50.0
49.8
49.8

49.8
49.7
49.6

49.4

49.5

49.1

48.9

48.6
48.1

47.7

47.5

47.6

47.4

47.1

46.8

46.5

46.2

47.2

47.1

47.4

47.5

47.3

47.3
47.5

48.4

48.5

48.7

48.8
48.7
48.7
48.7

48.9
48.7
48.5
48.5

48.2

53

54

55

56

38-45

39-43 38-42

37-42

48.4
48.9

49.0
49.3
49.3

49.2

49.3

49.1

49.2
48.9
48.6
48.6

48.6

48.8

48.9

48.7

48.3
48.3

49.3

49.5
49.2

49.1

49.2
49.1

49.1
48.9
48.9
48.7
48.0

48.4

48.2
48.0
47.9

47.4

47.7

47.5

47.8

47.9
48.2

48.4

48.6
48,6

48.6

48.5
48.5

48.7
48.7

48.0

48.1

48.2
48,0
47.8

47.5

47.8

47.9
48.0
47.9

48.3
48.7
48,9

50.4

50.7

50.8

50.9

51.0
50.9

50.8

50.6
50.3

50.1

49.5

49.5
49.3

48.7

48.6
47.81

47.9
47.5

46.2

47.3
47.2
47.2

47.1

47.5
47.9

48.2

48.4

48.6

48.8
49.0

48.7

48.8

48.3

48.5

47.4

47.3
47.1
46.8
47.1

46.4
46.3

46.3

47.7

48.4

48.8

49.5

50.0

50.4
51.3

51.1

51.5

51.2

51.1

51.0

50.8

50.5

50.2

49.9
49.7

49.3

49.1

48.7

48.6

48.8

48.2
48.0

47.9

48.0

48.1
48.0
47.8
47.8
47.8
47.8

47.7

47.8
47.8
47.8
48.0
48.0

48.4

48.7
.48.0

47.8

49.0

49.1

49.0

49.4

49.5

49.4
49.3

49.2

49.1
49.0

48.3
48.3
48.3
48.3

48.3

49.0

49.2

49.5

49.6

49.6

49.7

49.8

49.5

49.4
49.2

48.8
48.4
48.4

47.9

47.1
47.0
46.61

47.0
46.7
46.9

46.2
46.4

46.3
46.9

47.1
47.7

48.6
49.0

49.7

50.9
51.0

51.0

51.1
51.1

51.0
50.9

50.5

50.1

49.6

49.2
48,6

48.2
47.4

47.0

46.4

46.1
45.9
46.8
46.8
47.1
47 .\'4

47.5

47.8

48.1
48.0

48.3

48.3

48.4

48.3
48.0

47.6

47.4

47.2

46.9
47.0
47,0

47.5

48.0
48.4

48.8

49.1

49.2
49.0

48.9
48,9

48.7

48.9

49.3

49.2
48.9

48.6
48,0
47,8

47.7
47.7

47.7

47.4
47.4
47,4

47.8
48.0

48.3

48.9
49.6

50.3
50.6

50.8

50.6

50.9

50.4

49.7

49.5
49.0
48.3

47.8
48.0
47.8

47.2
46.7

46.6
46.0

46.3

46.7

47.0

47.5

48.1

48.7

49.6
48.6

49.4
49.6

49.2

48.8

49.4
49.4

49.4

49.6

49.8
50.0
50.0
50.2

49.9
49.9

49.7

50.2
49.9
49.7

49.6

49.3

48.5
48.5

47.2
47.9

47.7
48.0

48.3

48.5

48.8

49.0

49.1
49.1

48.6
48.1

47.7
47.3

46.9

46.3

46.4
47.0
47.0
46.9

47.0

47.6

47.7
47.3

47.8

48.1

47.5
48.0
48,3

47.9

48.2

48.3

48.4

48.8

48.5
49.3
49.7
50.3

50.6
50.5
50.3

50.0

49.5

49.1

48.6

48.2

47.9
47.9

47.7

47.3

47.0
46.3

46.7

46.8
46.7

46.9
47.5
47.9

48.5
48.9

49.2

49.3

49.6

50.1
50.1

50.0

49.7

49.8

49.9

50.1
49.5

50.2

51.0

51.1

50.2
49.8

49.8

49.4

49.1

48.9

48.6

48.2

47.5

47.7

47.6

48.3

48.2

48.3

48.3

48.4

48.4

48.5
49.9

49.7

49.4
49.3

49.8

49.6
49.3
49.3

48.8
48.3
48.2
48.2
47.8
47.8
48.0
48.2
48.2
48,2

48.5
48.5
48.5
48.5
48.0
47.8

-ocr page 115-

For convenience\' sake, and also for the reason explained on pp. 40—41,
the first observation was considered to be that of J D 7501. The
daily values
of the intensity were taken from PI. I; they were written on wooden cubes,
as advised by
Gibb {Op. cit. p. 680), and arranged in 88 rows of 35 cubes and
1 row of 20 cubes, the gaps being filled by blank cubes. After having obtained
the sums, and the number of observations contained in each column, with the
aid of a comptograph, the material was re-arranged in rows of 36, then in rows
of 37, and so on, until in the final arrangement the rows contained 60 cubes*).

The process is, even with this practical arrangement, a very laborious one quot; the
number of cubes which must be picked out from one row and placed in a higher one increasing
from 1 to the number given by the trial period.

-ocr page 116-

The result is stated in the preceding table. The first row gives the

abscissae of the periodogram; the second row contains the limits of the numbers

n, by which the sums 5 had to be divided; and the following rows contain the

mean values M = S:n. The last row gives the differences between the greatest

and smallest values of M which appear in each column, i. e. the ordinates of

the penodogram.1)The latter is given in Fig. 2. It shows, contrary to what had

been expected, two secondary peaks instead of one. They occur at 44 and 50

days respectively, with ordinates of about half the value of that of the principal
periodicity.

J8

So

lit

n

10

3S

SS

The process used is, however, a rough and, to some extent, a precarious
one; and we should exercise great care in deducing results from it. The first
question which arises is, whether we are obliged to extend the periodogram
beyond the hmits 35 and 60 days. The lower limit was chosen simply in order

-ocr page 117-

to start the process at a certain distance from the high peak, which a priori
could be expected at 39 days; and the higher limit, to conclude it at a certain
distance from the secondary peak, which was anticipated at about 54 days.
Now this peak did not show itself; but, instead of it, two peaks appeared at 44
and 50 days. Since the ordinates of the three periodicities which manifested
themselves measure together about 37 units, whereas (neglecting the extreme,
and rarely observed, values of the brightness, and taking 80 and 20 as the
ordinary hmits) the amplitude of the light-curve is about 60 units, we should
be inclined to say that, with the three periodicities we have found, the observed
amount of amplitude is not yet exhausted; so that we have either to consider
some of the smaller peaks as so many periodicities, or to extend the periodogram
for further researches.

With regard to the first of these points, the following criterion is available.
Not only does the difference between the greatest and smallest values of
M
give us an idea of the amplitude of a hidden periodicity, but the whole curve
of the quantities
M forms an image of that periodicity.*) Schuster used to treat
that curve by harmonic analysis; a necessary process in the attempt to discover
periodicities which were not very prominent. But if, in the process we have
used, and in view of the marked periodicities which we expect, the curve of
the quantities
M is fairly smooth and regular, we are justified in considering
it as the image of a real periodicity. If such a periodicity is absent, the curve
of the quantities
M will be an irregular line. This graphical process, of which we
shah speak more in detail in chapter VII, displayed regular single curves only
for the arguments 39, 44 and 50 days; and so the three peaks mentioned
above stand unrivalled.

Therefore we must consider the other alternative, viz. a search for other
periodicities beyond the hmits 35 and 60 days. But, as this would mean a
considerable, and in fact an unlimited amount of additional work, we have
not felt obliged to undertake it even to a small extent. The fact that the three

-ocr page 118-

periodicities we have found do not, in their sum, yield the necessary amplitude,
may be wholly due to the number of rows which we have used. It would seem,
at first sight, as if any increase in this number would reveal a periodicity more
clearly; but, as a matter of fact, the result of such an increase may be the
quot;washing outquot; of the whole oscillation. To show this, let us consider the fol-
lowing example:

If, in an extensive series of daily values, there exists a periodicity of
exactly 40 days, there is an advantage in taking a large number of rows, since
this will allow the peak to come out more clearly above the general level;
and this without any corresponding disadvantage. But if, in the same arrange-
ment, the constituent period is not exactly 40 days, an increase of the number
of rows will necessarily introduce a danger. Let us suppose, for instance, that
the true period is 40.4 days. In that case, the trial period being 40 days, the
maxima will almost immediately begin to shift slowly from their column,
until, after 50 rows, minimum values take their place, causing such a marked
diminution in the height of the peak that it may fail to draw attention. A
further increase of 50 periods will give an equal distribution of all the phases
of the light-variation
in each of the columns, i.e. the effect of the periodicity
will have vanished entirely. After that, the chance of getting a high peak pre-
sents itself again; but the preceding 100 rows have been not only useless, but
even a disadvantage, since they have caused a rise of the general level (which
is proportional to Vn).

This reasoning finds its analytical expression in the fact that the am-
phtude of a periodicity
p\' will be zero when

P\' =p {I ± y)

n

in which formula p is the trial period, and n the number of periods (i. e. the
number of rows) involved in the process. Thus in our case, since = 39 and
P\' = 39.25 (see p. 108), the high peak in Fig. 2 would have disappeared if we
had used a number of rows in the neighbourhood of 156.

Many authors, who apphed the method of periodogram-analysis, have
repeatedly advocated an increase in the number of rows, under the false im-
pression that it will run strictly parallel to an increase of the resolving power

-ocr page 119-

in spectrum-analysis. Though both the process by which the results are reached,
and the formulae which can be derived from it, suggest a close analogy betweeri
periodogram-and spectrum-analysis, there remains this striking difference
between the two, that in spectrum-analysis we are not concerned, a
prion, with
the period, while in periodogram-analysis we are. In spectrum-analysis the
periods are given in advance; in periodogram-analysis they must be sought
for. This essential difference materially affects the details of the comparison.
An increase of resolving power, for instance, increases the purity of the whole
spectrum, whereas an increase of the number of rows affects the different
unknown periods in a variety of ways, and, in fact, may even occasionaUy
vitiate the results.

According to the above formula, each number of rows n is connected
with two periods p\' in the neighbourhood of the trial period (/gt; x w = the
total number of observations), the existence of which cannot be detected
unless a new arrangement is expressly made for the purpose. In the case of
R V Tauri p x n = 3100; for p = {n = 59) the formula gives p\' = 52.10
and 53.90; but since = 52 and 56 = 54 have been examined, there is a very
small probabihty that the two other periods, which differ so httle from them,
have any existence. Doubtful cases, however, arise when p\' falls about midway
between two of the trial periods used in the periodogram. In the following hst
these cases are numbered 1—9.

li

no.

! p

\\

n

P\'

no.

P

n

11

|| 1

\\ 35

89

34.60

35.40

14

48

! 65

47

.26

48

.74

2

! 36

86

. 35.58

36.42

15

49

^ 64

i 48

.23

49

.77

3

_ __

! 37

! 83

36.55

37.45

i 16

! 50

62

1 49

.19

50

.81 j

4

: 38

81

37.53

38.47

17

1 51 :

61

50

.16

51

.84

5

i 39

79

38.51

39.49

1 18

! 52

60

1 51

.13

52,

.87 1

6

40

77

39.48

40.52

1 19

53

59

i 52,

.10

53

,90

7

41

76

40.46

41.54

I 20

54

57

53,

,05

54.

,95

8

1 42

74

41.43

42.57

21

55 ,j

56

54.

02

55.

98 1

9

43

72

42.40

43.60

22

56 !

55

54.

98

57.

02 |i

10

44

70

43.37

44.63

23

57 i

54

55.

94

58.

06 ii

11

45

69

44.35

45.65

24

58

53

56.

91

59.

09

12

46

67

45.32

46.68

25

59 1

53

. 57.

88

60.

12 !

13

47

66

46.29

47.71

26

60 !

52

58.

85

61.

15

——^

—......---

------- -- -

---------- -

■ -

- —

__________

_____

_________

... !

-ocr page 120-

As will be seen later on, the course of the work led to a special considera-
tion of the periods 38.5, 39.5 and 43.5. Of the other doubtful periods, 40.5,
41.5 and 42.5 have been examined, but with a negative result. The existence of
periodicities smaller than 38 days, with amplitudes large enough to be detected
by periodogram-analysis, seemed to the writer to be very improbable, and no
special investigation regarding their existence has been undertaken.

Having once established the fact that the sum of the amphtudes given by
the periodogram is certainly less than that of the true ones, we have not extend-
ed the search for periodicities beyond the hmits of 35 and 60 days; and we
have contented ourselves with gathering from the periodogram, as a prehminary
result, the fact that, in the phenomenon shown by the leveled light-curve of
R V Tauri, three periodicities are active, namely those which occur in the
neighbourhood of 39, 44 and 50 days. The possibility of a period in the neigh-
bourhood of twice the principal periodicity will be considered on
p. 112.

-ocr page 121-

CHAPTER Vn.

a closer examination of the three periods.

The prehminary result arrived at in the preceding chapter, makes it

an attractive and interesting inquiry to discover whether the whole leveled

light-curve can really be built up by three single curves. This problem requires,

in the first place, a more accurate knowledge of the lengths of the periods. In

order to obtain this, the time-interval had to be taken as 0.5 instead of 1

day. This is usually done, in a search for a periodicity of ^ 0.5 day, by

arranging the material alternately in rows of ^ and 1 numbers, and by

neglecting the last numbers of the longer rows. In other words, where in the

arrangement for p p l days the first columns would contain the
observations numbered:

1 p \\ 2p I Zp \\ 4.p I etc.

^ 2 2/gt; 3 3/) 4 4/) 5 etc. respectively,
the first column in the arrangement for ^ 0.5 day contains the observations
numbered:

1 p l 2^ 2 Zp 2 4p 3 etc.

In our examination of the doubtful periods, mentioned in the preceding
chapter, we have used this method with great advantage; but, in considering
the true periods, we have preferred to foUow a more correct course, by
doubling the number of cubes, and interpolating between each two values used
in the prehminary research. Where this interpolation did not give a whole
number, the nearest even number has been taken. In the determination of the
ordinate for 38.5 days, each row thus consisted of 77 cubes; in that of the ordinate
for 39 days of 78 cubes, and so on. In order not to extend the amount of work

-ocr page 122-

in an unnecessary way, and with the hope of getting a greater intensity (see
p. 100), the whole available materialhas not been used in this closer examination;
but such a number of days has, in each case, been chosen as would guarantee
the values of w being of the same order for the three periods. Starting from
J D 7501 for aU three periods, the investigation of the 39 days\' period has been
carried to J D 9490 (1990 days); that of the 44 days\' to J D 9848 (2348 days);
and that of the 50 days\' to J D 0230 (2730 days). The results are given in the
following tables, which are arranged in the same way as in the preliminary
research. The separate parts of the periodogram, which they estabhsh, are
given in Fig. 3.

-ocr page 123- -ocr page 124-

45.0

X =

43.5

44.0

44.5

45.0

46

48.9

44.4

47.9

48.9

47

48.8

44.1

48.0

48.4

48

48.7

43.8

48.0

48.3 1

49

48.6

43.7

48.3

48.1

50

48.7

43.5

48.5

47.9

51

49.1

43.2

49.3

47.7

52

49.0

43.1

49.3

47.6

53

48.8

43.1

49.4

47.5

54

48.7

43.1

49.4

47.6 i

55

48.6

43.1

49.6

47.6

56

48.6

43.2

49.7

47.4

57

48.6

43.2

49.7

47.4 i

58

48.5

43.5

49.7

47.5

59

48.3

43.7

49.9

48.0

60

48.3

44.0

49.9

47.9

61

48.4

44.4

49.9

47.8

62

48.9

44.6

49.9

47.7

63

48.8

44.8

50.0

47.7 :

64

48.9

45.2

50.6

47.8 î

65

49.2

45.4

50.7

47.5

66

49.2

45.6

50.6

47.6

67

49.0

45.8

50.8

47.6

68

49.0

46.2

51.0

47.6

69

48.9

46.3

51.1

47.6

70

48.8

46.5

51.2

47.2

71

48.7

46.8

51.6

47.0

72

48.6

47.1

52.0

47.1

73

48.2

47.8

52.1

47.1

74

48.0

48.0

52.1

47.1

75

48.0

48.1

52.3

47.0

76

48.0

47.9

52.4

47.0

77

48.0

48.0

52.4

47.1

78

48.0

48.2

52.5

47.1

79

48.1

48.3

52.2

47.0

80

48.2

48.5

52.0

46.9

81

48.2

48.6

51.9

46.9

82

48.2

48.2

51.8

46.9

83

48.2

48.5

51.7

46.9

84

48.0

48.9

51.5

46.9

85

47.8

49.2

51.2

47.0

86

47.5

49.3

50.8

46.9

87

47.4

49.6

50.5

46.9

88
89

49.7

50.2

46.9

50.3

46.6

90

46.9

y

2.9

9.3

9.4

4.1

43.5

44.0

44.5

ri; =

1

2

3

4

5

6

7

8
9

10
11
12

13

14

15

16

17

18

19

20
21
22

23

24

25

26

27

28

29

30

31

32

33

34

35

36

37

38

39

40

41

42

43

44

45

47.3

47.2
47.0
47.0
46.9
46.8

46.8

47.4

47.3

46.9
46.8
46.8

46.5
46.5

46.4

46.5

46.3

46.4

46.5

46.6
47.0
47.2

47.5

47.7

47.8

48.0

48.1

48.2
48.4

48.6

48.3

48.4
48.1
48.0
47.8

47.7

47.7
47.6

47.6

47.8

47.7

47.8
47.8
47.6
49.0

50.0
50.2
50.5

50.8
51.0

51.2

51.3

51.5

51.7

51.9
51.9
51.9
52.0
51.9
52.0

52.2
51.9

51.8
52.0

52.4

52.4

52.3

52.2

51.9

51.3
51.0

50.7
50.3

50.0

49.6

49.7

49.1

48.8

48.2

47.8

47.2
47.1

46.5

47.3

46.9

46.4
46.0
45.4
45.0
44.7

50.0

49.6

49.1

48.7
48.3
47.9
47.5
47.1

46.5

46.1
45.7
45.3

45.0

44.6
44.3
43.9

43.7
43.5
43.3

43.2

43.1
43.1

43.5

43.3

43.3

43.6

43.7

43.8

43.7

43.8
43.8
43.8
45.1

45.1

45.4
45.6
45.8

45.8

45.9

46.2
46.6
47.0

47.3
47.6
47.8

47.1
47.1
47.1
47.1
47.1
47.1
47.1
47.1
47.6
47.1

47.1

47.2

47.1

47.2

47.2
47.1
47.1
46.9
47.1
47.0

47.3

47.6

47.7

47.8

48.0

48.3

49.6

49.7

50.5

50.6

50.6
50.5

50.7

50.5

50.4

50.3

50.1
50.1
50.0

50.0

49.9

49.6

49.4

49.1
48.9

-ocr page 125-

.r =

49.5

50.0

1 50.5

1

X =

49.5

50.0

: 50.5

.t; =

]

49.5

1 50.0

50.5

1

49.6

45.0

i

j 48.5

35

45.7

49.1

! 51.1

69

49.0

51.1

46.9

2

i 49.2

44.7

48.7

36

45.7

49.5

i 51.0

70

49.3

50.7

46.9

3

49.0

44.6

1 48.9

37

45.9

49.9

50.9

71

49.5

50.6

1 46.8

4

48.8

44.4

1 48.9

38

46.1

50.4

i 50.8

72

50.9

50.3

46.5

5

48.7

44.2

49.2

39

46.4

50.8

50.8

73

1 51.1

50.0

46.2

6

48.6

44.0

, 49.4

40

46.4

50.9

50.7

74

51.3

49.7

46.1

7

48.2

44.0

49.6

41

46.5

51.2

50.9

75

51.6

49.4

46.0

8

48.0

44.0

49.8

42

46.7

51.5

50.5

76

51.9

49.4

46.0

9

47.9

44.6

50.0

43

46.8

51.6

50.5

77

51.8

49.3

45.6 î

10

47.6

44.2

1 50.3

44

46.9

51.9

50.2

78

51.9

49.0

45.8

11

47.4

44.2

50.4

45

47.0

52.1

49.8

79

52.1

48.8

45.6

12

47.3

44.4

i 50.5

46

47.1

52.2

i 49.5

80

52.1

48.9

45.6

13

i 47.1

44.6

1 50.6

47

47.2

! 52.4

: 49.2 1

81

52.0

48.5

45.5

14

i 46.8

44.9

50.7

48

47.4

52.4

48.9

82

52.2

48.3

45.3

15

46.6

! 45.1

50.3

49

47.5

52.3

48.5

83

52.1

48.0

! 45.4

16

I 46.2

45.3

1 50.4

I

50

47.6

52.1

48.1

84

52.3

47.8

45.0

17

1 45.9

45.5

! 50.4

51

47.6

51.9

47.9

85

52.4

47.6

45.0 il

18

î 45.7

1 45.8

50.1

52

47.5

51.9

47.8

86

52.7

47.3

45.4 i

19

45.5

46.0

50.2

53

47.4

51.8

i 47.5

87

52.6

47.0 :

45.2

20

45.7

46.2

50.2

54

47.3

5], 7

47.2

88

52.3

46.7

45.2

21

45.6

46.4

: 50.0

55

47.5

51.5

47.0

89

52.2

46.7 !

45.2

22

45.5

46.6

49.9

56

47.5

51.4 i

46.8

90

51.9

46.5

46.2

23

45.5

46.8

49.7

57

47.4

51.3

46.8

91

51.4 1

46.4

46.3

24\'

45.5

46.9

49.5

58

47.3

51.1

46.8

92

51.3

46.4 i

46.4

25

45.4

47.1

49.6

59

47.4

5] .4

46.7

93

51.1

46.2

46.6

26

45.3

47.3

49.7

60

47.5

51.5

46.4

94

50.9

45.9

46.9

27

45.3

47.3

49.7

61

47.5

51.3

46.2

95

50.6 1

45.7 i

47.0

28

45.2

47.6

49.6

62

47.7

51.1

47.4

96

50.4

45.6

47.3

29

45.9

47.8

49.7

63

47.9

51.0

47.3

97

50.2

45.4

47.4

30

45.9

47.6

50.2

64

48.1

50.7

47.2

98

49.9

45.2

47.6

31

45.8

47.9

50.2

65

47.9

50.5

47.1

99

49.6 1

45.1

47.9 1

32

45.8

48.2

50.9

66

48.1

50.3

47.0

100

45.0

48.2

33

45.7

48.5

51.0

67

48.4

50.6 1

46.9

101

48.3

34

45.7

48.9

51.0

68

48.8

51.0

_______________]

46.9 :

i

1

i

!
i

i

y =

i

7.5

8.4 1

6.1

-ocr page 126-

The ordinates for the trial periods 39 and 39.5 days, and again those for
44 and 44.5 days, are almost exactly equal to each other; and we may conclude
from this that the true periods will not differ much from the mean values 39.25
and 44.25 days. This conclusion tacitly assumes that, since the time-interval
is only 0.5 day, we may consider that the ordinates within that interval change
proportionately in the neighbourhood of the true period. Using the same
assumption in the case of the third period, we get 49.85 days as the most
probable value of the true period.

As an illustration of what has been said about the amphtude, we may
remark that in the preliminary research, when 3100 days were used, the height
of the 39 days\' peak was 18.7 units, whereas in the second research, using 1990
days, the height of the peak rose to 26.6 units. In the case of the other two
periods the increase of amplitude is not so striking; a fact which may partly
be due to the smaller diminution of the resolving power.

We have now to consider the phases of the three periodicities at the
starting point J D 7501. As we have remarked on
p. 99, the curve of the quan-
tities
M is the image of the periodicity to which they belong; its maximum
is the first maximum which occurred after J D 7501. We have drawn on PI. II
(b, c, d) the six curves belonging to the trial periods 39
.0, 39.5, 44.0, 44.5,
49.5 and 50.0 days. 1)

The curves for 39.0 and 39.5 days are very characteristic. Even when
we take the ordinates
M to two decimals, the points lie almost exactly on a
very smooth and regular curve. There is one discontinuity, which occurs in
these and all the curves, at the moment marked x, in which the extreme
maximum at J D 7788 sets in with the intensity 97 (see
p. 79). Its influence
is very perceptible, especially when it occurs on a descending branch.

As an illustration of the abrupt way in which the image of a marked
periodicity, such as we encounter here, appears and disappears, we have drawn
on the same scale the graphs of the values of
M for the trial periods 38.5
and 40.0 days (PI. II e and f).

1nbsp; For cJearness\' sake we liave preferred to reproduce only the points through which
the curves ought to be drawn. In the diagrams c and d small lines indicate the continuity
ot the curves at the points of their intersection.

-ocr page 127-

On the hne of the abscissae the number 1 means J D 7501, and we see
at a glance that the epoch of maximum of the trial period 39.0 days is J D
7518.6, and that of the trial period 39.5 days, J D 7505.0. The difference is
13.6 days; and as the true period lies midway between the two trial periods,
we are justified in fixing its epoch of maximum at J D 7511
.8.

The curves for the other two periodicities are not so regular as those
for the first one; a fact which will be fully understood later on. The epochs of
maximum of the curves for 44.0 and 44.5 days being J D 7494.5 and 7509.0,
the true periodicity of 44.25 days will have a maximum on J D 7501.8.

The curves for 49.5 and 50.0 days are not similar to each other, since
they he at unequal distances from the true period. The 50.0 days\'curve, which
is lying nearer to the true curve, is the more regular of the two. The maxima
he at J D 7543.0 and J D 7524.5, from which it follows that the 49.85 days\'
periodicity had a maximum on J D 7530.0 (and 7480.2).

It will be perceived that the conclusions arrived at in the two preceding

chapters, do not aUow us to say more than that the leveled hght-curve of

R V Tauri is very probably in some way a combination of the fohowing three
periodicities:

Maximumnbsp;M_m

I J D 7511.8 39.25 E 27 ]
II J D 7501.8 44.25 Enbsp;10 or more (see p. 102.)

Ill J D 7480.2 49.85 Enbsp;9 )

If the difference between the trial period and the true period is m days, and if the

number of periods involved in the process is the change in phase isnbsp;x m days.

2

-ocr page 128-

CHAPTER VIIL

The three periodicities combined, and the possibility of

a solution with only two periods.

We have seen on p. 86 that the observed hght-curve has a curved central
hne. By the quot;levehngquot; process we transformed this into a straight Hne, which
we shall now call the quot;axisquot; of the leveled light-curve. The ordinates of this
curve (PI. I) are expressed in intensities; in that scale the mean value of the
maxima is 64, and that of the minima 30; from which it follows that the axis
coincides approximately with the intensity 47. In what follows we shall assume
its value to be 47
x.

Each ordinate of the hght-curve, diminished by this amount, is the sum
of the simultaneous ordinates of the three single curves. If we consider these
to be sinusoids with amphtudes y^, y^ and y.,; and if the phases on J D 7500
(intensity 53, see p. 79) are cf^ and cp^ respectively, the relation between
the unknown quantities is at this starting point:

yi sin y^ sin yg sin = 6
Five days later, the phases are advanced with amounts
a, b and c,
which are known from the periods.

If we put:

y, cos (f., =nbsp;(k =1,2,3}

we get from the intensities, given for each five days in the hst on pp. 79-86,
449 equations of the form:

cos na z/ sin na cos nb sin nb cos nc z^\' sin nc = I

=0.1.2,............)

which must be solved by the method of least squares.

For this purpose we have, for the sake of accuracy, enlarged the scale

-ocr page 129-

of the mtensities, 1000 being now the greatest intensity instead of 100, and
470 being the intensity of the axis. Moreover we have thought it best not
to treat the material as a whole, for the following reason.

We have on p. 100 referred to one circumstance which requires some care
in the practice of periodogram-analysis; but there is another pit-fah which,
so far as we can see, has escaped the attention of previous investigators. This
is the possibility that a peak in the periodogram is not the result of any perio-
dicity, but of a non-periodical quot;outburstquot;, or of a number of intermittent
outbursts which reinforce each other. In the former of these cases (e.
g. a new
star) a high peak will occur
whatever may he the trial period- and this charac-
teristic of the peak wih directly point to its origin.1) In the latter case, it will
be important to locate the outbursts as accurately as possible; and this can
only be done by dividing the material. For our present purpose we have taken
12 groups, each of which consists of about 6 periods of 39 days.

13

10

11

12

14

Amplitudes

Interval

a;

Phases

Maxima

no., Limits

Cen- I
tre

/Il

J m

: .y2

Mx

M,

M,

(fi

(P2

(jPs

7500—7680

7590
7899
8128

7785—8000
8005—8240
8245—8430 8338:
8505—8690
8695—8985

8598

88481:

9113|j

93881

9700

9980

0248

0516

9
10
11

12

8990—9290
9295—9480
9485—9800
9805—0115
0120—0410
0415—0600
47
—11
—16
1 11
—21
66
—24
—34
37
32
62
33
7504.8

—0.10
0.02
0.04
—0.02

89
271
147
132
195
155
165
173
203
149
121
153

50
257
28
60
74
87
18
41
104
30
53
64

16
171
16
43
81
68
37
25
50
36
62
54

- 3
-18
-16
—35
■48

.87
.83
.00
.33
.50
.47
.36
.45
.65
.66
.25
.55

50
225
191
90
178
110
305
307
320
99
182
87

.70
.00
.58

288
58
257

.32
40
00
83
67
64
06
95
17
40
05
33

7510
11
11

13
15
10
12
12

14

15
14

7510

.2
.9
.5
.7
.1
.7
.4

.75 257

0.05
—0.14

.33
.11

.30
.75
.25
.98
.62
.51

282
204
130
51
351
56,
274.
148.

0.06
0.08
—0.08
—0.07
—0.13
—0.07

-23
—24
43

-47

—38
- 4

7522.3

7504.4
7476.9
7526.6

7523.2
7484.1
7494.4

7505.3
.97513.7
.8j7504.6
.6 7474.5
.3 7491.9

7483
7487
7499
7533
7497
7473

.4
.5
.5

.57517.5

7515
7498
7488
7500

1nbsp; For an illustration see the discontinuity in all the curves of the quantities M (p. 108)

-ocr page 130-

The results of this computation are given above. The first three columns
give the number, the hmits and the quot;centrequot; of each interval; the latter differing
from the mean of the interval, since the 12 groups do not exactly coincide with
the observational seasons. The fourth and fifth columns give the quantity
a;
by which the intensity 470 (magn. 10\'quot;.12), assumed for the axis, has to be
corrected, both in the scale of intensities and in that of magnitudes. The
columns 6—8 give the amphtudes of the three waves, whereas 9—11 give the
phases on J D 7500. And, finally, the columns 12—14 give the dates of the
initial maxima derived from these phases. It wih be noted that for the and
waves these dates do not always give the maxima next to JD 7500. The
reason for this will be given later on.

A glance at the last three columns of the preceding table, shows us that
the first wave, which has a period of 39.25 days, may alone be considered as
relatively stable; the 44.25 and 49.85 days\' periods being decidedly unstable.
This being so, it seems advisable, before starting to investigate the character
of these unstable waves in detail, to make sure that no solution presents itself
in which a
single additional wave, with a period lying beyond the periodogram-
limit of 60 days, can replace them with the same degree of accuracy. Roughly
speaking, the appearance of a kind of
3 Lyrae variation always suggests the
influence of a period of about twice the principal one; i. e. in our case, of a period
in the neighbourhood of 78.5 days. A study of the aspect of the light-curve
gives the impression that, at intervals of, say, about 940 = 12 x 78.5 days,
the same character presents itself again; a repetition which might be ascribed

to the existence of an interfering period of 78.5 (1 ± days.

1 2

In order to test this, the 39.25 days\' curve was alternately combined
with two curves having periods of 72 and 85 days respectively. After a
consideration of the different values of the maxima and minima, in those parts
of the light-curve where the
[i L.yrae type was most prominent, ampli-
tudes of 80 units were assigned to the additional waves. The amplitude of
the stable wiive was kept constant at 159. These two combined curves
were compared with the observed one, and this resulted in the rejection
of the 85 days\'period. As to the 72 days\'period, the computations were sim-

-ocr page 131-

plified by taking equal numbers of days from 6 different seasons, and by starting
each season with its own phase. By doing so, the 6 sets of normal equations
had the same coefficients throughout, and could be solved very quickly.

The result was, that the suspected 72 days\' periodicity would have
had maxima on the fohowing dates, falhng about the middle of each season:

1.

8135.7

386.6

2.

8522.3

326.7

3.

8849.0

377.1

4.

9226.1

395.0

5.

9621.1

393.8

6.

0014.9

But we should recall the fact that our hypothesis required a 72 days\'
curve which should be continuous. This would mean that the 6 maxima, derived
from the partial investigations, would be maxima of the continuous curve as
wen. Since, however, this does not appear, the hypothesis must be rejected.

The following is an analytical criterion of the existence of a single
additional periodicity:

If the first period is exactly known, and if, from a certain starting-
point (phases cp and i//) we take the ordinates of the combined curve, at distances
which exactly equal 120° of the known period, each interval of three of these
periods will yield the following 6 equations:

sinnbsp; y sinnbsp;= I,

X sin 120) y sin (,/, a) - 4

^ sin ((p 5.120) y sin {^p 5a) - 4

-ocr page 132-

In these equations a° is the equivalent of 120° for the second periodicity,
and the quantities I are the ordinates of the combined curve.

If we put:

i W =/

a; cos qi = Z2

these equations become:

—nbsp;I A2 cos a z/ sin

—nbsp;i z^fz^ cos 2a z^ sin 2a = 4

z^\' cos 3a Z2\' sin 3a = l.^

—nbsp;4 fz^ z/ cos 4a sin 4a ^

y sin xp ^ z/
y cos ij) = Z2\'

(1)
(2)

(3)

(4)

(5)

(6)

a =

—nbsp;—A2 -^i\' cos ha sin 5a = 4

cos a =■

From these equations we can ehminate and by subtracting (4)
from (1), (5) from (2), and (6) from (3). We then get 3 equations with 2 unknown
quantities and z^), giving rise to the following determinant:

h-

-k

sin 1 a

cos 1 a

-h

sin ^ a

cos 1 a

= 0

sin 1 a

cos I- a

whence:

(4 4) — (/a h)

2 {h—k)

Since each of the nine observed seasons contains 3 groups of 3 periods
of 39.25 days, each value of cos
a in the following table is the mean of three.

Season

I

cos

a

1

Season

cos a

Season

^ cos

a

1

1

0.

07

4

—0.51

7

0.

........

60 !

2

—0.

01 \'

5

0.52

8

0.

13

j 3

7.

40

6

—0.80

9

1.

01

-ocr page 133-

The result is again entirely negative. We have made another arrange-
ment, advancing 180° of the first period instead of 120°, but without success.
This means that we are justified in leaving the possibihty of ow^ additional
period out of further consideration, and may proceed to a more detailed analysis
of the three waves, which we had previously discovered.

-ocr page 134-

CHAPTER IX.

A detailed analysis of the three waves.

I.nbsp;The correction of the assumed axis.

The quantities a; must be considered as resulting from the errors made in
the course of the quot;levelingquot; process; and we may use them to correct the curve
of the long periodicity. The curve thus corrected is represented by the dotted
line on PI. II (a). It has 2 maxima, which occur after an interval of 1210 days,
and 3 minima, occuring after intervals of 1170 and 1350 days respectively
(mean 1260 days); whereas the rising branch crosses the line 9\'quot;.80 at inter-
vals of 1130 and 1465 days (mean - 1292 days). From these numbers we
conclude that the long periodicity is a more or less regular wave with a period
of about 1250 days.
M — m is about 1\'quot;.2*), and its value seems slightly to
decrease.

The observations do not extend over a period long enough to give a
more detailed knowledge of this interesting element in the process of the star\'s
light-variation.

II.nbsp;The amplitudes.

The amplitudes of the three waves,taken from the table on p.lll^ have
been plotted in Fig. 4. The principal feature of this representation is the re-
markable rise between J D 7600 and 7900, which, considering the light-curve
itself, must have been even more abrupt than could be gathered from the
smoothening process of computation . The exact outbreak of the disturbance,
which must have caused this abrupt rise of amphtude, has not been observed!
A glance at the curve of the long periodicity, shows us that the observations

See Appendix.
See also p. 130.

-ocr page 135-

280

2 0

300

160

IZO

do

I

4-0

n

EI

I

7S00

700
600
500
400
300
ZOO
100

esoo

8000

9500

OSOO

Fig. 4. The amphtudes of the three periodicities.

i. Period = 39\'^.25 II. Period = 44\'^.25. III. Period = 49\'^.85.

-ocr page 136-

are not contrary to the hypothesis that the date of the outbreak, and the date

on which the curve of the long periodicity began to rise, have been nearly
simultaneous.

After the outburst in group 2, the amphtudes did not again attain the same
large values; but they were far from constant. A glance at the upper part of
Fig. 4 shows, not only that their changes were not arbitrary, but also (roughly
speaking) that, for all three waves, they seem to have gone through the same
periodical process. This caused them to attain maximum values in the 5th and
9th groups, and minimum values between groups 7 and 8, and again between
groups 10 and 11. This fact betrays itself stiU more clearly when, for the 12
centres as abscissae, we plot the
sum of the amphtudes of the three waves,
which is done in the lower part of Fig. 4. Here we see that, apart from the heavy
outburst mentioned above, the amphtudes of the three waves have gone
through periodical changes, the period being about 1000 days.

in. The phases.

In the computations, which led to the results given on p. Ill, we took for
granted the constancy of the periods. If this supposition was correct, we
should have found that, within the hmits given by the mean errors, the values
for the phase at the starting point
J D 7500 were the same, whether they
resulted from one group or from another. The following table contrasts the
mean deviation of the phase-values Ap (expressed in days) with the mean
value of the separate mean errors (m. e.).

1

Wave

Ap

1

I

1 .5

II

9.2

III

11 .6

m. e.

2.0
2.5
3.7

It shows that there is no reason to doubt the constancy of the 39 days\'
period, whereas the 44 and 50 days\' periods are apparently unstable. At first
sight this result seems strange, since in the method of periodogram-analysis

-ocr page 137-

the constancy of the periodicity is tacitly assumed; and it proves once more
that this method ought to be handled with some caution. We have already
said, on p. Ill, that, from the appearance of a peak in the periodogram, we need
not necessarily conclude that some periodicity has been active during the whole
interval of time under investigation. It is, moreover, obvious that when a
periodicity has been active during separate parts of the interval only, the
appearance of a peak will depend upon its amplitudes. For instance, let us
consider an extreme value of the amplitude of the second wave, i.e. the value
104 in group 9. Since, in the periodogram, we get the double amplitude, and
since we have used in its construction a 10-fold smaller scale, the amphtude 104
is equivalent to a peak of 21 units. But if it has been active only during an
interval of about 200 days, (and this seems to have occured here), then, since
the total interval which has been analysed is 2348 days, the height of the peak,
belonging to the periodicity which was active in the 9th group, would have
been about 1.7 units, i.e. wholly imperceptible.

The same reasoning holds good for the other groups. The fact that the
phases possess different values, means that the vibration made itself felt through
the different groups with a constantly changing period; and in the majority
of cases these periods were not able to develop a peak in the periodogram.
The same may be said of the 50 days\' vibration. Apparently only those periods
could manifest themselves in peaks, which reinforced the outburst in group 2.
If this outburst had not taken place, it is practically certain that no attention
at all would have been drawn to the additional periodicities. The result of
this would have been, that the attempt to investigate the star\'s hght-changes
by means of periodogram-analysis, would have failed.

Turning to the problem presented by the star\'s behaviour after the
outburst, the continually changing phase-values at first presented a serious
difficulty, since they lead to periods which vary in an irregular way, from
about 4 days less to about 4 days more than the mean periods. But it proved
possible to make a hypothesis by which the values of the periods, though they
increased in amount, yet changed in a regular way, and along a curve which
ran parallel to the 1000 days\' curve of the amphtudes. We shall proceed to
show this
in extenso for the second wave.

-ocr page 138-

The phases, as given in columns 9—11 of the table on p. 111^ resulted
from the computations without any ambiguity ; and from them we are in-
chned to derive the corresponding divergences from the mean period, by
combining the adjoining maxima (or other characteristic points) in such a
way that the resulting changes in phase wih be as small as possible. The follow-
ing table shows the results. Its first column gives the number of the group;
the second, the phase-angle; and the third, the nearest value of the maximum.
Thus for instance, the normal maximum as derived from group 8 is found to
be either 7517.3 or 7473.1. The nearest value to J D 7500 has been adopted.

Group

lt;i

p

1

1 M

AM

M\'

i AM\'

! m

. e. i

3

191

.58

7487

.5

—13

.8

7487.5

1 —13.8

3

.8 :

4

90

.75

7499

«

.8

— 1

•5

7499.8

! 1.5

2

.2

5

178

.33

7489.

,2

—12

.1

7533.4

32.1

i 2

.2

6

110

.11

7497,

.5

3

.8

7497.5

i — 3.8

1

.5

7

305

.30

1 7517,

,8

16

.5

7473.5

—27.8

7

.5

1 8

307

.75

7517.

3

16

.0

7517.3

16.0

2

.4

9

320

.25

7515.

9

14

.6

7515.9

14.6

0

.2

10

99.

,98

7498.

8

— 2,

.5

7498.8

— 2.5

3

.0

11

I

182.

,62

7488.

6

12

.7

7488.6

—12.7

1

.7

12

87.

51

7500.

3

1.

,0

7500.3

— 1 .0

1

.9

1

i

L

7501.

3

i

-

7501.3

i
j

I
i

1 j

, 1

The fourth column gives the differences between these maxima and
their mean value. These differences do not follow a regular curve; and if we
were to adopt them, we should be forced to conclude that, after the outburst,
the star has been subjected to smaher disturbances in periods which appear
to change capriciously. This is net impossible, but a physical explanation
would be difficult; and it would be of great value if the maxima in the centres
of the groups could be combined, so as to represent
regular changes of the
periods,
even if the amount of the differences A M were to increase. Such a com-
bination has been arrived at by taking, in group 5, the following and, in group 7,

-ocr page 139-

the precedmg maximum. The new combination is given in the fifth column
of the same table. The sixth column gives the new values of the differences;
and the last column the mean errors of M\'. To obtain these we have made
a fair estimate of the mean errors of the quantities ^ and (p. 110); and, after
that, those of y and qj could be derived by computation.

In the same way, for the third wave we have to change two values
only in order to get similar results; and when the values AM\' for both waves
are plotted, they prove to foUow a curve which, roughly speaking,
is identical
with the
1000 days\' curve of the amplitudes\'\'). This relation is at once evident
from Fig. 5, in which all the points are surrounded by circles, with radii equal
to the mean errors.

For the 39 days\' wave, the changes in the phases are of the same order
as the mean errors, and this prevents an exact conclusion as to their periodical
character. We might be inclined to accept the probabihty that a wave, which
is unstable in amplitude, will also be unstable in phase; but the fact is that we
are not able to show it in a quantitative way.

Thus, from the analysis of the leveled hght-curve oiRV Tauri, we may
gather the following facts:

(1 ) the principal feature is a wave with a period of 39.25 days, which, so
long as we are in want of more precise knowledge, must be considered as stable;

(2)nbsp;apart from this principal wave, the star\'s light is constantly dis-
turbed by the influence of vibrations, occuring in periods which may be con-
sidered as being grouped around the values 44.25 and 49.85 days, but which
differ from these by amounts covering the whole distance from—4 to 4 days,
and from — 4.5 to 4.5 days, respectively;

(3)nbsp;the amphtudes of both (1) and (2) undergo periodical changes, the
period being about 1000 days;

(4)nbsp;each change of period is accompanied by a corresponding change
of amplitude;

-ocr page 140-

Amphtudes.

to
to

-ocr page 141-

(5) the star is occasionaJly subjected to an outburst, wliich affects tlie
amphtudes of all three mean periods.

We have already remarked that, without an outburst, such as that which
took place between J D 7687 and 7785, the waves mentioned under (2) would
have escaped detection. In the hght of the above results we may now conclude
that, if we had not taken the precaution to use a 10-fold extended scale of
intensities in the computations, it is exceedingly doubtful whether the facts
mentioned under (3) and (4) could have been laid down. Even now, the results
cannot pretend to a high degree of accuracy; for not only are the mean errors
relatively large, but the 1000 days\' curves do not show more than the general
progress of the periods and amplitudes. These circumstances make it hardly
possible to represent the observed hght-curve with precision.
A value of the
phase, taken from this curve, may have an error of several days; moreover
(and this is a material difficulty), for any particular day we get only the
stim
of the three amphtudes. The separate values cannot be given with anything
approaching to certainty.

We have devoted much time, and have tried in several ways, to solve
this problem, but without success. When we use fixed laws of variability, it
seems impossible to obtain a close approximation to the observed light-varia-
tion. The combined curves persist in differing from the observed one even in
their mere aspect. We have therefore desisted from a precise comparison
between the observed curve, and a curve based upon the results of our analysis,
and we have contented ourselves with showing:

I.nbsp;that both these curves, though of different aspects, are ahke in the
essential features, which may be taken to represent the character of any
combined vibration;

II.nbsp;the degree of instabihty which may be assigned to the calculated
curve (apart from unknown, and perhaps irregular, perturbations), owing to
the relatively large errors in the quantities which play a part in its contraction.

I. A hypothetical light-curve has been constructed in the following
way. The period of the first wave was kept constant at 39.25 days; its phase
on J D 7500 was the mean of the results for the different groups (see p. 111).

-ocr page 142-

For the second and third waves the values representing the phases
were plotted on a large scale, and, taking the mean errors into account, a
curve was drawn which seemed to represent, as accurately as possible, the
change in phase common to both waves. This curve was slightly different
from the curve of Fig. 5, in which both phases and amplitudes are represent-
ed. We preferred to adopt a curve
common to both waves, because this makes
the drawing of it less arbitrary. Its ordinates were read off for every 5 days,
and were applied as corrections to the Juhan dates.

The 1000 days\' curve of the amplitudes, mentioned before, gave the
correction to be apphed to the sum of the amphtudes. The question arose as
to which part of this sum had to be assigned to each of the waves. A glance at
Fig. 4 wiU show that it was impossible to treat the changes of amplitude for
the three waves separately; and the best thing to do seemed to be to divide
each corrected sum, in the proportion of the mean values of the amphtudes.
This proportion was as 3 : 1 : 1; and so, having obtained from the 1000 days\'
curve the total amount of amplitude, we assigned three fifths of it to the
principal wave and one fifth to each of the additional waves.

Finally, to the ordinates of the combined curve the quantity a; (see
p. Ill) has been apphed, so as to make the comparison with the observed
light-curve stiU more effective.

The results of this comparison are given in the following tabular form,
which contains 20 points of comparison, most of which do not need explanation.
Under the heading of quot;amphtudequot; we have, as before, taken the difference
between the brightness of a maximum and that of the
preceding minimum.

The numbers 10 and 11 contain the actually observed periods, without
regard to whether they resulted from maxima or minima.

The numbers 19 and 20 have the following meaning. For both curves a
mean period (no. 12) was adjusted to normal epochs of maximum and minimum
brightness by the method of least squares, and the residuals in the dates of
maximum and minimum brightness were recorded. For the observed curve
this had already been done when treating the hght-curve as a whole (see p. 93);
and now it was repeated for that part of the curve, which was observed after
the star\'s outburst (groups 3 to 12).

-ocr page 143-

Maximum

Minimum

nt

0

C

Element

0

i

C

1.

Highest

m

9 .41

m

9 .54

10.

Greatest

d

48 .5

d

43 .0

2 .

Lowest

10.03

10.01

Period

11.

Smallest

33.0

33.0

3.

Mean

9.79

9.80

Il2.

Mean

39.25

39.22

4 .

Highest

10.09

10.21

Duration

[ 13.

Longest

24.5

22.0

5.

Lowest

11 .10

10.94

of

14.

Shortest

11 .0

16.0

6.

Mean

10.64

10.50

Ascent i

f 15.

Mean

17.0

19 .2

7.

Greatest

1 .52

1 .40

Duration j

16.

Longest

30.0

22.0

8 .

Smallest

0 .25

0 .24

of

17 .

Shortest

16.0

15.5

9 .

Mean

0.83|

0 .72

Descent (

18.

Mean

22.3

19 .3

Residual \'

j 19 .

Greatest

7.0 :

5.7

1 20.

Mean

2.5 !

2.0

The comparison between the observed hght-curve and a hypothetical
one, based upon the results of our analysis and computations, proves, as might
be expected, that both curves present the same characteristic features. There
is but one exception; for the calculated curve the mean duration of the ascent
(element no. 15) must have the same value as that of the descent (no. 18),
since the constituent curves are sinusoids. The observed curve, however,
shows for the ascent a mean duration of 5.3 days shorter than that of the des-
cent. This would mean that, either the principal wave, or the secondary waves,
or all three, are of the
Cepheid type. In order to see how this compares with
the results we have already obtained, let us return to the curves of the quanti-
ties
M (PI. II), which should be the images of the periodicities. They show us
that, for the principal wave, the duration of the ascent (A) is a httle less than
that of the descent (D), viz. about 2 days. As to the additional waves, we get:

Trial period 44.0 daysnbsp;A — D = 7.0 days

44.5 „nbsp;= 10.3 „

,, 49.5 „nbsp;„ 3.5 „

50.0 „nbsp;„ 9.2 „

These numbers show that thenbsp;Cepheid type is distinctly seen in the
principal wave alone.

Element

-ocr page 144-

II. To show the influence of a change in the quantities by which the
hypothetical curve has been calculated, we must have recourse to the mean
errors. When we draw the curve of the amphtudes, so as to touch the mean
error-circles on each side alternately, we obtain perfectly legitimate corrections,
A a and — A a, which we shah have to apply to the sum of the amphtudes.
But it was less easy to obtain, in this way, the corrections which should be
apphed to the curve of the phases; since we have adopted a curve which is
common to both periodicities, and its mean error is a function of the individual
mean errors. We have therefore apphed to the ordinates of the 1000 days\'
phase-curve a correction Aqp of 5 days; a value, which, since it is larger in
many parts of the curve, wih ahow us to remain on the safe side.

Correction

; 1

! \'

Aa

Maxim.

1 Br. I

Maxim.

Br.

Maxim.

Br.

!

li

9395.0

m

9.98

9433 .5

ni

9 .65

9476.0

• m

9.59

--

, 9396.5

10.03

9434.5

9.79

9476.5

1 9.73

li

! 9399.5

9.84 ;

9435.5

9 .99

9472.5

\' 9.71 li

1

9399.5

9.93 \'

9435 .0

10 .04

9472.0

: 9.84

1

1 Observ.

9398.5

i 9.95

9432.5

9.79

9472.5

9.87

i Correction

i i

:| Aa

Minim.

Br.

Minim.

Br.

Minim.

i i

________1

1

1

9378 .0

m

10.37

9414.0

m

10.80

9455.5

i

11 .50

1

9378 .0

10.32

9413 .5

10 .58

9454 .5

10.88

9379 .0

10.92 i

9418 .5

10.49

9453.0

10.60 i

, -

9379 .0

10.68

9418.0

10.39

9453.0

10.46

Observ.

9379.0

10.56

9419.0

10.88

9454.5

10.67

The corrections A a and A can be combined in four different ways
according to their signs, and have been adjusted to an arbitrary part of the
calculated curve, extending from J D 9370 to J D 9485. In this interval 3
consecutive maxima and minima occur, whose dates and magnitudes will be

-ocr page 145-

changed under the influence of A a and In the preceding table the results
of an application of these corrections are given; the last row gives the values
as they appear in the
observed light-curve.

This table shows that, at least for this portion, the calculated curve is
very unstable, and that the differences between observation and calculation
may be due whohy to the fact that the constituent quantities of the latter are
deficient in point of accuracy.

If, to this inaccuracy, we add the facts:

(«) that we have considered the 39.25 days\' wave as perfectly stable in
phase; whereas it is uncertain whether it is not to a small extent unstable;

{[i] that we have considered the 1000 days\' curve for the 44.25 and
49.85 days\' periodicities as being regular and the same for both; two facts
which are not beyond doubt;

(y) that we have divided the total amount of amplitude in the pro-
portion 3:1 :1 throughout the whole interval considered; which however
is only a working hypothesis;

((5) that probably none of .the waves are sinusoidal;

(f) that, where such a marked outburst as that which occurred in group
2 has been noted, it is very probable that the more or less regular process
by which the calculated curve has been constructed, is liable to frequent
perturbations;

we need not be astonished that the calculated curve, while keeping as
a whole its essential features intact,
cannot be compared in any strict sense with
the observed light-variation.

-ocr page 146-

CHAPTER X.

On a possible interpretation of the results
of the analysis.

Though the aim of this volume has been merely to consider the light-
curve of F
Tauri, and not to attack the problem of its origin before the
analysis of the hght-curves of the two other stars
{R Sagittae and V Vulpeculae)
has been completed, we cannot resist the temptation to say a few words about
a possible interpretation of our results at the close of this part of the work.

If the 44.25 and 49.85 days\' periods had proved to be constant, a mechan-
ical interpretation, e.g. a triphcity of the star, would naturally have presented
itself. Since, however, we have found that these periods are constantly and
systematically changing, so that there are actually two light-phenomena with
periods from
40 to 48 and from 45 to 54 days, the idea of a triple star may
frankly be abandoned.

If, then, we consider the star to be single, the results obtained for the
quot;leveled light-curvequot; are not inconsistent with the following suggestions
concerning its origin:

(1) The principal feature is a wave with a constant amplitude, and a
constant period which represents the star\'s equatorial rotation. This feature
is a light-phenomenon belonging to the star\'s photosphere.1)

1nbsp; A tentative explanation would be that the rotating star has the form, either of an
apioid, or of a Jacobian elhpsoid. In the latter case the period of rotation nnist be con-
sidered as equal to twice tlie period of the liglit-variation.

-ocr page 147-

(2)nbsp;This photosphere, having exhibited immediately beforehand
(group 1) very small values for its light-variation, was heated through some
internal process, which caused the intensity to rise in an abrupt way to an
exceptionally high value, such as was never attained again during the interval
of 10 years in which the star has been under investigation.

(3)nbsp;The combined effect of two other light-phenomena which belong
to the star\'s atmosphere is superposed upon the regular wave (1). In this
atmosphere luminous matter, bursting from certain quot;weak spotsquot;, subsequently
travelled in different directions. These weak spots, i. e. the centres of activity
of the ejected matter are located at latitudes where the periods of rotation
equal 44.25 and 49.85 days respectively. If the equatorial rotation is 39.25
days, they may occur both in the same hemisphere, or each hemisphere may
contain one of them; if the equatorial rotation is 78.5 days, they must be locat
ed both in the two hemispheres. Let us consider, as the most probable case
that in which each of the hemispheres contains one centre of activity; then we
should have been able to fix the date of the star\'s outburst, on the supposition
that at that starting-point, for, reasons of symmetry, the phases of the two
waves differed by 180°. But such a supposition is not consistent with our
results. The outburst must have taken place between J D 7687 (see remark 4
p. 76) and J D 7785, and from the normal maxima given by the periodogram
we deduce that in that interval the phase-difference increased from 18° to
107°. This ehminates the possibility of the outburst having occured at
spots which are placed diametrically opposite each other; a position in
favour of which one would be inchned to have a certain prejudice.

(4) The luminous matter, after having made its appearance at the
centres of activity, travehed through the outer layers of the star\'s atmosphere,
probably (in connection with the repeated recurrence of the initial period)
in some cyclonic movement, and changed its brigthness in a fashion which
suggests a correlation with the latitude reached. If this hypothesis is right,
the starting-point of the 1000 days\' phase-curve (Fig. 5) should be the moment
of the outburst, i.e. the axis of this curve should coincide with the normal
maximum given by the periodogram, and the curve itself, when traced back-
wards, should meet the axis at a point, the abscissa of which is the date of the

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outburst. As to the 44.25 days\' periodicity, this suggestion is in perfect accord-
ance with our results. The axis coincides with the normal maximum J D
7501.3 (see p. 120), while the periodogram yields the normal maximum
J D 7501.8. And, when the curve is traced backwards it meets the axis at a
point, the abscissa of which is J D 7740. Moreover, the normal maximum of
group 2 (J D 7483; see the table on p. Ill) is in accordance with the same
hypothesis, since it hes very close to the curve. This means that in Fig 4
the points indicating the amplitudes of group 2 do not belong to the top of
the outburst, but to its decline.

As to the 49.85 days\' periodicity, the axis of the 1000 days\' phase-curve
does not coincide with the value given by the periodogram; and it would
have been more correct, on the hne of our present hypothesis, to reconstruct
that curve so as to make the mean value of the normal maximum coincide
with that which is given by the periodogram. We have, however, preferred to
keep the previous arrangement intact; in this way the computations have
been simpler, and the results have certainly not been in our favour.

(5) Apart from the phenomena described above, the star\'s light is
subjected to a long periodical disturbance (period about 1250 days), which
in ah probability rose to a maximum shortly before the outburst of the photo-
sphere.

Now, since we are acquainted with a quot;long periodicityquot; in the 11 years\'
sun-spot cycle, and since
Nijland\'s frequent colour-estimates oi R V Tauri
(mean value = 3?6) aUow us to consider this star as being of the solar type,
we are naturally led to draw a closer analogy between it and our sun.

According to Abbot (quot;The Sunquot; p. 125), the general character of the
solar rotation is expressed by the following data:

Latitudenbsp;0° 30° 60° 80°

Period of rotation 24^6 26\'\\3 31^2 35^53 or, usingproportion-
ahty factorsnbsp;1.00 1.07 1.27 1.44.

When we plot these values, and if we adopt the same curve to express
the law which rules the rotation of
R V Tauri, we learn that the period 44.25
days belongs to the latitude 41°, and the period 49.85 days to the latitude 60°.

-ocr page 149-

Assuming the greatest deviation from the last-mentioned period to be 4.6 days,
we derive 73° for the highest latitude which has been reached by the luminous
matter. This result suggests the fohowing interesting fact, with regard to
the position of the star\'s axis of rotation. If we can observe the rotation
of luminous spots at different latitudes, in both hemispheres, as periodical
phenomena, it is obvious that the inchnation of the star\'s axis to the hne of
sight must be greater than the highest latitude in which a spot can be seen.
In our case this means an inclination of at least 73°. It is, however, prob-
able that it is nearer to 90°, since the image of the 50 days\' periodicity
(PI. II) is but very little sharper than that of the 44. But, if, as a working
hypothesis, we assume the axis to lie in a plane which is exactly perpendi-
cular to the line of sight, it is interesting to note that the position of
the axis
of our sun is parallel to this plane.

For an answer to the question, whether there occur in the sun\'s atmo-
sphere centres of activity and currents of luminous matter such as we have
found (on a much larger scale)
irxRV Tauri, we may refer to an interesting
paper by F.
Henroteau quot;On convection currents in high regions of the solar
atmospherequot; (Monthly Notices of the R. A.
S. LXXVI p. 18). In this paper
the writer cahs our attention to the fact, 1. that the spectroheliographic studies
of the upper layers of the sun made by
Deslandres, 2. that Mascari\'s results
concerning the distribution of the faculae, and 3. that
Slocum\'s researches
on solar prominences, all clearly point to the existence of systematic move-
ments in the high regions of the sun\'s atmosphere. A detailed examination
of a number of sun-spots, associated with large regions of faculae, led
Hen-
roteau
to deduce the course of these movements with stiU more certainty,
and to show that the area of the luminous matter underwent changes during
the progress. The movements proved to follow a meridian; but the number
of groups examined seems too smah as a basis for generalisation.

Slocum\'s results,1) based upon the examination of 1094 prominences,
are of special interest to our present problem, inasmuch as they show that the

1nbsp; F. Slocum. quot;Circulation in the solar atmosphere as indicated by prominences.quot; The
Astrophysical Journal XXXIII
p. 108.

-ocr page 150-

conditions are not the same in the two hemispheres. In the northern hemisphere
for instance, the tendency of movement towards the pole has a maximum value
at the latitude 33°; in the southern hemisphere such a maximum occurs at the
latitude 52°.

If now, with Henroteau, we admit the existence, in the outer layers
of the solar atmosphere, of convection currents, which carry luminous matter
from one latitude to another; and if the brightness of this matter differs from
that of the general mean, and its extension changes in its progress; then we have
in a quahtative sense the same phenomenon as that which a disclosure of the
complex hght-curve
oiRV Tauri has brought to hght. In the star the process
is even more regular, since we have found the brightness (which, as a working
hypothesis, we may regard as proportionate to the extension 1) distinctly
correlated with the latitude. Thus the difference between the san and the star
is only a
quantitative one, i.e. the difference between the brilliancy of the travel-
hng matter and that of its surroundings must be much greater in the star
than on the sun. There can be no
a priori objection to this assumption.

Conversely, if RV Tauri only presents an extreme case of solar varia-
tion, the disclosure of its hght-curve may perhaps encourage the detailed study
of those two phenomena, to which the attention of astrophysicists has been
strongly drawn during the last years, viz. the movements of the sun\'s outer
gases and the variabihty of its radiation.

1nbsp; Smaller brightness may just as well be due to greater depth.

-ocr page 151-

APPENDIX.

The technical side of the problem which has been considered in this
volume, gives rise to the following observation, which is worth noticing.

When, for the purpose of analysing a compound hght-curve into its
smgle curves, the combined brightness has been expressed in intensities,
and the amphtudes of the single curves have been obtained in the same scale
it is natural that we should wish to translate these results back again into terms
of stehar magnitude.
This, however, is impossible, since only the sum of the axes
of the single waves is known; their individual values cannot be given. Thus,
in the case of
R V Tauri, we have, in general, found the fohowing mean results,
expressed in intensities:

Combined axisnbsp;= 485

Wave I Amphtude {a^) =159 (Axis = x^)

IInbsp;.. {a^) = 55 ( „ = x^)

IIInbsp;M = 44 ( „ = X,)

If, now, we should wish to know the values M — m, which express the
difference between the maximum and minimum brightness in the magnitude-
scale, we discover that the problem is an indefinite one. A few suppositions
as to the values of the three axes (which measure together 485 units) wih not
only yield us totahy different results, but they wih also teach us that, though
«1 much exceeds
a.^ and a^, the corresponding values oi M m may very well
be of the same order.

-ocr page 152-

case.

The axes have the same values in the intensity scale

X\\ — x^

:— Xz -

-- 162

Then we

have

4- «1 =

Xi -dj, =

321

3

M,

fUj

= 10\'quot;53
= 15.63

M,

-^nii =- 5quot;?10

Axis =

■ 13quot;!08

X^ -f- CI2
Ct^ —

217
: 107

W2

= 10°?96
= 11.73

M2

— W2 = 0quot;^77

=

m35

Xz dz ~
Xz ~

206
118

Mz
ntz

= iiquot;:oi
= 11.62

Mz

— W3 = o\'^ei

,, Xz =

11\'quot;32

2quot;\'* case.

has 73,

and

have Ve of the total intensity.

Then:

x^ a^ =
X\\ — a^ =

482
164

M,

W]

= 10quot;!09
= 11 .26

M,

— = m7

Axis X, =

10\'quot;68

%2 ~

136
26

M2
m^

= 11°?47
= 13.30

M2

W2 = l\'quot;83

12^^38

=
Xz =

125
37

Mz
mz

= 11^56
= 12.88

Mz

— mz = 1quot;?32

12quot;\'22

case.

The

three axes have the same value in the

: magnitude-scale.

Then:

Xi a, =

— a-i^ =

364
46

M,

Wj

= 10quot;^40
= 12.65

M2

— m, = 2quot;^25

Axis Xi =

11 quot;^52

X2 a^ —

197
87

ma

= ll\'quot;06
= 11.96

M2

— m,, = O\'^OO

11^^51

Xz \'
X3 Uz

182
94

Mz

Mz

= ll\'^lS
= 11.87

Mz

— mz =0quot;f72

))

-ocr page 153-

The results of this case have been derived in the following way:

The well-known relation between intensities and magnitudes gives
rise in our case, where 9^30 has the intensity 1000, to the following equalities:
1000 = {x a) p\' —nbsp;(x — a) pc /Im = jpc

in whichnbsp;p = 2.512

c = ^ — 9°?30 and

I = the equivalent of X in intensities.

Hence:

{x «) {x~a) = P.
If X^ = X^ ^ we thus get, besides the relation
a^i X2 x^ = 485 the
two relations

— a\\ = x% — a\\ = — a\\.

A short way to solve these equations, is to start from the supposition
x^ — x^.

We then get

= 205nbsp;= 140.

By trial and error the values of and ATg which render the quantities
X exactly equal to each other, proved to be = 142nbsp;= 138.

We gather from a consideration of these 3 cases (which all lead to the
same combined effect) that, in the language of stellar magnitude, it is not certain
(though of course highly probable) that wave I is the principal one; and
that, in each case, waves II and III have values
M — w, which are greatly
in excess of what a study in intensities might have anticipated. The fact
that the relation between the intensity-and magnitude-scales is a logarithmic
one, necessarily leads to an under-estimate of the importance of the lower-
leveled waves.

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SUMMARY.

The variable stars R Sagittae, V Vulpeculae and R V Tauri exhibit
irregular light-curves, with mean periods of about 35,37 and 39 days respectively.
The variation is of an unusual character, but seems to be ruled by some
complicated law, which may be the same for each of the three stars. A thorough
investigation of the observed hght-variation is therefore justified, and it has
been preferred for various reasons to devote attention first
to RV Tauri.

In chapter I the observations of 8 observers have been reduced to a
photometric scale of comparison stars, whose brightness has been determined
by the writer with the polarizing photometer of the Utrecht Observatory.
Nearly ah the observations could be reduced to one observer (chapter II);
and, as a result of this, a strictly homogeneous hght-curve was drawn, based
upon 1222 estimates of magnitude. These estimates are given in chapter III
(pp. 44—75).

The hght-curve is described in chapter IV, and its ordinates are given
in tabular form on pp. 79—86. It exhibits, when plotted, a more or less regular
quot;principal variationquot; winding itself round a quot;curved central hnequot;, which
indicates a long periodical secondary variation. This quot;long periodicityquot;
(PI. II a) has been treated as an isolated feature, and its ordinates were used
to reduce the observed light-curve to a horizontal central hne. In this way
the principal variation was obtained in the form of a quot;leveledquot; hght-curve.
Since-the characteristics of this curve suggest the existence of some compound
variation, the magnitudes were changed into intensities, and the new curve
(PI. I) was submitted to periodogram-analysis.

-ocr page 155-

The resulting periodogram is given in chapter VI (p. 98); it shows three
peaks, which occur at 39, 44 and 50 days. This chapter contains some remarks
and criticisms on the method of periodogram-analysis.

In chapter VII the same analysis is repeated for a few trial periods
in the immediate neighbourhood of those mentioned above; the time-interval,
which had been 1 day in the first investigation, being now taken as 0.5 day.
This resulted in fixing the definitive periods at 39.25, 44.25 and 49.85 days
respectively. For each of these waves a date of normal maximum could be
derived by a graphical process (PI. II b, c, d).

The periods now being known with sufficient accuracy, they could
be used, in chapter VIII, to give the progress of the three waves per five days
m 449 equations, in which the amphtudes and the initial phases constituted
6 unknown quantities. A seventh unknown quantity was added, by assuming
a correction which must be applied to the quot;levelingquot; process. In the solution
of these equations, the material, which covered an interval of 3100 days,
was divided into 12 groups; and the scale of intensities was enlarged 10-fold.

The results of this computation are given in a table on p. 111. It shows
that the 39.25 days\' wave is relatively stable, whereas the two other waves
are unstable. It seemed advisable, before entering into the details of these
unstable waves, to investigate the possibility of a solution with a single
additional periodicity. This has been done both graphically and analyticahy
(p. 113), but the result was negative.

Chapter IX treats of a more detailed analysis of the three periodicities
given by the periodogram. The general results of this can be summed up as
follows:

I.nbsp;The amplitudes are small in group 1 and very large in group 2,
suggesting some quot;outburstquot;. They are again smaller in group 3—12, in which
groups they pass through periodical changes; the period being roughly 1000 days.

II.nbsp;The phases are fluctuating, but to an extent which, in the case
of the 44.25 and 49.85 days\'periodicities only, exceeds the mean errors. For
these waves the fluctuations fohowed the 1000 days\' curve of the amphtudes.

III.nbsp;When the results found under I and II were used to derive a
hypothetical combined hght-curve (C), this could not be made to represent

-ocr page 156-

the observed hght-variation (O) satisfactorily. It could, however, be shown
that in respect of 20 essential features, the curves C and O did not appreciably
differ (p.l25), and that the differences O—C may be smaller than the uncer-
tainty in C (p. 126).

In chapter X a tentative explanation is given of the results of the
analysis. The colour-estimates of the star and the long periodicity suggest
some analogy with our sun. This analogy is extended by the fact that the
adoption of a law of rotation, common to both objects, leads to reasonable
latitudes for the periods 44.25 and 49.85 days, if the period 39.25 days is
supposed to represent the star\'s equatorial rotation. The results of the analysis
are, therefore, not inconsistent with the suggestion that spots of luminous
matter should suddenly have appeared, as the consequence of an outburst
in the star\'s photosphere, in the outer layers of the atmosphere at latitudes
41 ° and 60° respectively, and should have been subjected to changes in position
and brightness, which were both systematic in character (1000 days\'curve)
and correlated with each other.

If this explanation holds good, it can easily be shown that the axis of
rotation of the star lies in a plane, which is perpendicular to the line of sight.
It is interesting to notice that the axis of our sun happens to be parahel to
this plane.

Finally the attention of the reader is drawn to a paper by Henroteau
(p. 131), the tendency of which lends an emphasis to our suggestion of a quali-
tative analogy between
R V Tauri and the sun. The conditions, of course,
are not comparable in a quantitative sense.

The conditions of the problem before us, as the analysis will have
sufficed to show, are of so comphcated a character that no apology will be
necessary for an explanation which is obviously exceedingly tentative.

The present research has led to our classing R V Tauri amongst the
semi-regular variable stars, of which
Mir a is the proto-type. While most of
these are more regular, some of them (e. g. IF
Cygni) are decidedly less regular
in aspect than
R V Tauri. It is very probable that an apphcation of the method
we have used would yield some important results m the case of all the
Mira

-ocr page 157-

variables. The few results already obtained along different hnes by A. Thom,
(The Journal of the British Astronomical Association XXVI p. 162) seem
to confirm this suggestion.

Grateful acknowledgement is due to Professor A. A. Nijland for
his valuable criticisms and advice, so freely given during the prepar-
ation of this work; and to the Reverend
A. Blakiston for the labour
and time he has devoted to the revision and correction of the manu-
script and proof-sheets.

-ocr page 158-
-ocr page 159-

PLATE L

-ocr page 160-

PLATE IL

—I—

0500

6500

9000

the original curve.

9500nbsp;0000

.......... the corrected curve.

-ocr page 161-

• CL

• d

^RV

XORTH.

Slars surrounding R V Tcmri. Scale 1 c.M. 1(1\'.

The princiiDal star is BD 25° 731.

A photographie chart of the same field has been pubhshed by W. Ceras]lt;i in:
„Cartes photographiques d\'étoiles variables découvertes à l\'observatoire de Moscouquot;
Serie. Pl. III.

-ocr page 162-

. - • _ _, ■nbsp;^, •,,.....,\'.v ; • ■ :

\' ; -.v ..-.

-quot;■/a, ■ ■ gt;
\' .
\'■\'.\'\'À

v\'-ri;

-ocr page 163-
-ocr page 164-
-ocr page 165-