The whole light curve, constructed from the AAVSO one-day means (about 6070)
of observations, is displayed
on a condensed time scale in Fig. 2.
The respective parts, plotted on an expanded time scale, can be seen in
Fig. 3 and Fig. 4. The seasonal gaps are usually short
and the dense coverage allows to follow the course of the brightness
variations almost day by day. One can immediately resolve that the amplitude
significantly varies on the time scale of years. There are definitely groups
of large variations with an amplitude about 2 mag. These changes
have a repeating character and occur on a typical time scale of hundreds of
days. On the other hand, extended intervals (years) of a flat light curve
with just minor fluctuations can be seen in other years.
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Figure 3: The same AAVSO light curve as in Fig. 2 but plotted with high temporal resolution (the first half) |
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Figure 4: The same AAVSO light curve as in Fig. 2 but plotted with high temporal resolution (the second half) |
The AAVSO data set begins with an epoch of large-amplitude variations
(from 10 mag to 13 mag
). The extrema of brightness
are sharp, especially the maxima have a character of distinct peaks
("outbursts"). Both gradual and abrupt transitions between extrema can be
resolved. Notice that after 3.8 years this season abruptly ends
around JD = 2438970 with a transition into an intermediate level of
brightness (about 11 mag
); a brief dip may have occurred here.
This transition can be established with an accuracy of several days.
V Sge spends the next 3.3 years in this intermediate level. Just minor
variations can be seen till JD = 2440190 when a rapid decline of
brightness introduced another series of large-scale variations. In this
season which lasted for 8 years (till JD = 2443000) the brightness varied
from about 10.5-11 mag to 12.5 mag
(several brief
excursions up to about 10 mag
). Most extrema of brightness are
flatter and more rounded now. The light curve is gaining a character of
alternating high and low states in this season (hereafter HS and LS). Part of
this segment was already plotted with smaller time resolution in
Fig. 5 of
Paper I, but owing to weaker coverage the AFOEV data were averaged over
several days. Despite the heavier smoothing, which left only the long-term
changes in the AFOEV data, the mean course of the HS/LS variations is in
agreement with the AAVSO observations.
Another extended interval of an almost flat light curve, lasting for about
8 years, spans . The interval is interrupted
near JD = 2444400 by one event, having the character of an isolated
outburst. Its analysis was given in Paper I. The duration of this outburst is
much shorter than the surrounding interval of the flat light curve.
The next season of large-scale variations, which was introduced by a
well defined rapid decline into a low state, set in near JD = 2445900.
Most variations with an amplitude larger than about 1 mag can
be described as alternating HSs and LSs again. However, they occur on a
shorter time scale (up to 100 days) than in the previous season of the HS/LS
transitions. Besides the episodes of well defined HSs and LSs one can resolve
short-term variations in the high state; they take place on the time scale
of days and have an amplitude of several tenths of mag
. The
alternating HSs and LSs vanished around JD = 2447300 and the brightness
remained near the level of HS. Although some fluctuations of brightness are
present after this date (till about 2447500) they do not resemble the
episodes of LSs anymore. Brightness of V Sge showed no episodes of low state
till JD = 2448300 (for about 3 years).
Although some data are missing near JD = 2448300 it is evident that an episode of LS occurred here and introduced a new extended series of alternating HSs and LSs. These states are very pronounced now and repeat on the time scale of 200-300 days. Most transitions between the states are relatively abrupt (i.e. much shorter than the duration of the state) and can be easily resolved. The high states usually display some structure. Brightness of a HS immediately after recovery from a LS is often higher than that before the decline into LS. Also some shallow minimum near the middle of a HS can be resolved. Detail of the brightness fluctuations in HS is shown in Fig. 8 in Paper I, again averaged over several nights.
In summary, this examination of the AAVSO light curve revealed that the seasons of the suppressed brightness variations (hereafter called flat segments) interchange with intervals of pronounced changes (hereafter active segments). The borderlines of the segments are usually well defined and the light curve can be divided into seven seasons. They are marked in Fig. 2 and abbreviated as S1-S7. Changes of brightness in the active segments often have a character of the HS/LS transitions. The flat segments display just minor fluctuations of brightness and although some rare larger excursions (a few days) from the main level may be present, they can better be compared to the brief dips, documented by [33, Robertson et al. (1997)]. Our data do not allow to carry out a reasonable assessment of such short rare events.
One more segment, formed from the AFOEV data and representing the
light curve in the years 1934-1944, is included. Its large part is displayed
in Fig. 2 in Paper I and can be characterized as a long-lasting epoch of low
brightness (near 12 mag) with occasional relatively narrow
outbursts (see Paper I for details). In the following analysis we will treat
it as segment S0. We note that there are just very few scattered data within
the years 1944-1961 and do not enable any reasonable analysis in this time
period.
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Figure 5:
a) Two-sided moving averages of the brightness for the
AAVSO data. b) Standard deviations ![]() |
Moving averages is one method which enables us to suppress the high
frequency variations and obtain thus a better insight into the long-term
trends. We will present the results of this method first because it allows to
analyse variations through the whole data set without further presumptions.
Two-sided moving averages of the AAVSO data were calculated for several
values of Q. The parameter Q refers to the interval of days, within which
the data were averaged. We also introduce the standard deviation of every calculated mean point. This quantity gives information about the
current amplitude of the variations.
We calculated the moving averages for several
values of Q.
Figure 5 displays the results for Q=400 days. This filter
half-width washed out the variations inside the active segments and
emphasized the general levels of brightness. 200 to 570 observations are
inherent in each mean. It can be resolved in Fig. 5a that the
lowest mean brightness occurs in S1 but increases towards the transition from
S1 to S2 (from active to flat segment) near JD = 2439000. Also initially
large rapidly decreases towards S2. The average level of
brightness in S3 (active segment with HSs and LSs) is clearly lower than in
the neighbouring flat segments S2 and S4.
slightly grows
through segment S3 but then rapidly falls as the border with S4 approaches.
The active segment S5 is clearly defined by a large bump in (Fig. 5b). However, the light curve in Fig. 5a shows that
the mean brightness level through this segment stayed almost unchanged with
respect to adjoining S4 and S6.
HSs and LSs in S7 are very pronounced and have a long cycle-length. They therefore tend to be more sensitive to the seasonal gaps. The course of the moving averages for this segment may be then distorted to some extent. Nevertheless, the mean light curve shows that the highest brightness did occur in this segment.
In summary, the moving averages reveal the long-term changes of the
mean level of brightness of V Sge. Mainly the respective seasons of
the large-amplitude variations (manifested by enhanced and
corresponding to the active segments) tend to brighten with time; this is
clear especially for the sequence S1-S3-S5. The course of
confirms the obvious fact that amplitude of the brightness changes varies
in agreement with the division into segments. We note that the transitions
between the neighbouring segments are
inevitably rounded in Fig. 5a,b
due to the large value of Q used.
![]() |
Figure 6: The statistical distributions of brightness constructed from the one-day means of observations in the respective segments. The intervals in JD and parameters of the segments are given in Table 1 |
The histograms of the one-day means, constructed for the brightness in
segments S0-S7, are displayed in Fig. 6. The width of each bin is
0.25 mag in all cases. Parameters of the distributions can be
found in Table 1. The distribution of the whole AAVSO data
set (S1-S7) is clearly unimodal without any other features and is roughly
symmetrical. We preferred not to include segment S0 in this histogram since
it represents a season separated from the rest of the data by a gap of about
17 years.
Large changes of the distribution from segment to segment can be seen
when the respective histograms are constructed for S1 to S7. They confirm
the division presented above. Notice three similar segments S2, S4, S6 which
are clearly unimodal, relatively narrow, roughly symmetrical and all have
almost identical mean levels (near 11.3 mag). On the other hand,
very broad distributions are observed in active S1, S3, S5, S7. The histogram
for S1 is flat and has an asymmetrically placed peak near 11.9 mag
. The distributions of S3 and S7 are bimodal. The histogram for S5 is
slightly more narrow than S3 and S7 and its bimodality is at most marginal.
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The divergent distributions, apparent in the histograms for the individual segments, suggest changes on a very long time scale (years to decades) in the activity of V Sge. The net parameters of each segment (mean brightness, skewness, excess), listed in Table 1 and plotted versus JD in Fig. 7, allow for a better insight into these trends.
The evolution of the net parameters of the active segments S0, S1, S3, S5, S7 deserves special attention. The most striking variation is a gradual change of asymmetry of the histograms (skewness) in the sequence S0-S1-S3-S5-S7 (Fig. 7a). This change through the four latter segments can be considered linear; the fit is denoted by dashed line in Fig. 7a. We admit that the limits of segment S0 are not so clearly defined as the rest of the segments. Nevertheless, skewness of S0 follows the trend of the later active segments.
A gradual increase of the mean brightness in the sequence S1-S3-S5-S7,
apparent in Fig. 7c, amounts about 0.4 mag. The
points are connected by a line for clarity. Mean levels of HSs and LSs
are included; they allow to resolve their contribution to the resulting
trend. It turns out that the mean levels of HSs in active segments are always
brighter than the levels of the adjacent flat segments S2, S4, S6.
Brightening of the active segments is in accordance with the moving averages
(compare Fig. 5a and Fig. 7c). Two levels of LS in S7
are displayed, with the last episode and without it (see below).
![]() |
Figure: 7 Net parameters of the respective segments from Table 1 plotted versus Julian Date. Each point is centered on the middle of the appropriate segment. See Sect. 3.3.1 for details |
Comparison of Fig. 7 with Figs. 2, 3 and 4 allows to relate evolution of the net parameters with the changes of the character of the light curve in the respective active segments. The large negative skewness and low mean brightness of S0 are caused by the relatively narrow outbursts from the quiescence level (Fig. 2 in Paper I). The type of variations in segment S1 is intermediate between the separated outbursts in S0 and HS/LS transitions in S3, S5, S7. The well defined transitions between HS and LS, analysed in Sect. 3.4, began in S3. With increasing mean brightness in the next active segments V Sge spends more time in HS than in LS, causing thus an increase of skewness.
The alternating high and low states are a characteristic photometric
activity of several kinds of interacting binaries: cataclysmic variables
(CVs) of the VY Scl type (e.g. [36, Shafter et al. 1985),] polars (e.g.
[14, Hudec & Meinunger 1977),] X-ray binaries (e.g.
[15, Hudec & Wenzel 1986).] However,
due to its short duration, only rarely is the course of the transition
between the states covered by the observations. V Sge displayed the typical
HS/LS transitions in active segments S3, S5, S7 (see Sect. 3.1). Dense
coverage of the AAVSO data allowed to resolve the course of these transitions
in 36 cases. The typical appearance of the HS/LS variations in V Sge can be
described as follows. The onset of the episode of LS begins with a rapid
fall of brightness from HS by about 1 mag. The phase of LS is
not quite flat in some cases; it displays a very slow brightening (e.g. LSs
centered on JD = 2449300 and 2449520). The final return to HS is
approximately as rapid as the decline. Brightness after return to HS is
sometimes (mainly in S7) slightly higher than immediately before onset
of LS. Interchanging HSs and LSs in segment S5 occurred on a short time scale
(Sect. 3.5) and the stable level of LSs was not always fully
developed.
![]() |
Figure 8: a) Duration of the respective HS/LS transitions in three active segments (S3, S5, S7) of typical HS/LS behaviour of V Sge, plotted versus Julian Date. Logarithmic scale is used for the y-axis. b) Rate of the brightness change during the transitions. Those transitions which belong to the same episode of the low state (fall and rise of brightness) are connected by lines. See Sect. 3.4 for details |
The declining and rising parts of the light curve of the well covered transitions were approximated by straight lines. Linear least squares fits were used inside the intervals, adjusted interactively, for determination of the parameters of the transitions. The results for S3, S5 and S7 are summarized in Table 2.
Not all transitions have equal amplitude; many states, especially
HSs, display their own structure (fluctuations on the time scale of days or
trends-often brightening through LS and decline through HS). The transition
therefore does not always begin and finish in the mean level of the state. In
order to describe the transitions in S3, S5, S7 fully, both duration and the
rate of change are needed (Fig. 8ab). The
lower limit of the duration is comparable for all three segments (typically
several days, the shortest transition only 4 days). The respective segments
largely differ mainly in the range over which the durations are scattered.
Transitions in S3 are generally slow with a large scatter (7 to 80 days),
which also is reflected in their low rate of change. On the contrary, S5
represents a relatively tight group of very rapid transitions (4 to 11 days).
The rate of change for the respective transitions in S5 varies by one to
four, which is larger than the ratio of the durations and confirms scatter of
the amplitudes. Parameters of the transitions in S7 are intermediate to S3
and S5.
Statistical distribution of durations of all measured transitions (Fig. 9) shows a clustering between 4 and 20 days and a weak tail towards prolonged transitions (up to 80 days).
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We further analysed a possibility of gradual variations of the brightness levels of the respective HSs and LSs through the whole active segment. We mainly checked the working hypothesis that the brightness difference between HS and LS is largest near the middle of the segment and decreases towards its borders (possible gradual development and vanishing of the instability). The mean brightness of each state with the removed transitions was calculated, received a unit weight and was centered on the middle of the appropriate state. Inspection of the data confirmed that the level of the given state was achieved also in several cases of weaker coverage. The means were fitted by linear and quadratic polynomials. Upward curvature of the quadratic fit of HSs and downward curvature for LSs would be expected if our working hypothesis were true.
The linear fits both to HSs and LSs satisfy the course well in segment
S3; the quadratic terms are very small. However, the brightness difference
between HS and LS linearly increases through S3.
Notice that this behaviour
is also apparent in the evolution of
in Fig. 5b.
Linear fits are justified also in S5. They reveal small decrease of
brightness of both HSs and LSs through this segment while the brightness
difference between HS and LS stays almost constant. Brightness of HSs
increases linearly through S7. At the same time, levels of the respective
LSs in S7 display more complicated changes with a prominent increase of
brightness during the last two episodes. It supports the interpretation of
the medium state after JD = 2449940 as an episode of an exceptionally
shallow LS.
We can conclude that with the exception of LSs in S7 the changes of the levels of the respective states are small and their courses can be considered linear. It strengthens the above given arguments that the transitions between the adjoining segments are rapid and that the characteristics of HSs and LSs are usually kept for the whole duration of the given segment.
Already visual inspection revealed that most HS/LS transitions occur
in at least a semi-regular manner. A search for periodicities was therefore
undertaken using the PDM program and the autocorrelation method.
The
PDM program ("phase dispersion minimization"), based on the method of
[40, Stellingwerf (1978)]
and written by Dr. J. Horn at the Ondrejov
Observatory, is suitable for nonsinusoidal time variations covered by
irregularly spaced observations. Significance of a given period is evaluated
by the parameter , lying in the range
0-1. Insignificant periods
have
while highly significant periods are expected to have
or lower. Horn's program enables not only an automatic
searching for the best period inside a given interval but also an interactive
examination of the resulting data foldings. It allows to assess whether the
course of the particular folded light curve is reasonable.
The autocorrelation method, described by
[29, Percy et al. (1981),] allows to
search for characteristic time scales or quasiperiods which extend just
for several cycles. This method makes use of the brightness difference
mag versus the time difference
t of each observation,
divided into equal bins. (Quasi)periodic behaviour then gives rise to the
minima in the resulting
mag versus
t curve.
Segment S7 was analysed first because it contains the most pronounced
HS/LS transitions. We restricted ourselves to
and excluded the last LS which brightness is roughly intermediate to HS and
LS. The period search revealed two possible periods: 286 days (
)and 238 days (
). Notice that the latter value is very close
to the period of 240 days, found by
[33, Robertson et al. (1997)] in their CCD
data. However, it gives too many points in antiphase. Our data folded with
P=286 days can be seen in Fig. 10.
implies that
the HS/LS transitions cannot be considered strictly periodic; 286 days is
just a typical time scale. The autocorrelation diagram displays a prominent
deep minimum at 270 days (Fig. 11) which is in good agreement with
the result of the PDM method. We therefore can conclude that the quasiperiod
near 280 days has its meaning and is not just accidental because the folded
light curve bears much of the course of the original data.
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Figure 10: The data inside the epoch of the HS/LS transitions (segment S7; JD = 2448314-2449930) folded with the period of 286 days. The peak at JD = 2449080, which occurred after recovery from LS, was taken as the initial moment of the folding. See Sect. 3.5 for details |
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Figure 11: Autocorrelation diagram for the segments S3, S5, S7. Notice the deep minimum at 270 days for the segment S7 which is in good agreement with the period of 286 days, found by the PDM program (Fig. 10). See Sect. 3.5 for details |
The PDM program did not reveal any period with in S3. The
autocorrelation diagram displays a minimum at 260 days but it is not as deep
as in S7 (Fig. 11).
Inspection of segment S5 revealed that the cycle-length is shorter
than in S3 and S7. However, no periods with were found. Even
the autocorrelation diagram does not display any prominent feature. Part
of this segment was also covered by the photographic data, analysed by
[23, Marsakova (1998).] The dominant period of 61 days, found by Marsakova, may
represent a characteristic time scale of the HS/LS transitions, persisting
just for several consecutive transitions; it only confirms a shorter cycle of
the transitions in this segment.
In summary, only typical cycle-lengths, not strict periods, can be traced in the active segments. We can state that while the HSs and LSs in segments S3 and S7 tend to occur on the time scale of about 270 days, a significantly shorter time scale (<100 days) prevails in S5.
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