In this section we present detailed TSPA analysis examples for real data.
All time units are days.
Sections 6.1 and 6.2 describe the second order TSPA
()
analysis for the normalized magnitudes of V 1794 Cyg during
subsets SET=42 and 114 from
Jetsu
et al. (1999b, Paper II).
The next Sect. 6.3 clarifies our methodology in Paper I,
where the second order TSPA analysis is performed for
all subsets of normalized magnitudes of V 1794 Cyg.
In Sect. 6.4 we apply the fifth order TSPA (
)
to the
V light curve of the cepheid variable BL Her
(Moffett & Barnes 1984).
One sample of the V magnitudes of the nonvariable
primary comparison star SAO50205 from Paper II are analysed with
the first order TSPA (
)
in Sect. 6.5.
The magnitudes of V 1794 Cyg within each passband ()
have been
normalized with
In SET=42, the deepest
(Eq. 6) minimum
between
and
is at
(Fig. 1a:
).
The best window period
P0=0.9997 detected
with
(Eq. 15) connects
P1 to
and
,
while
and
.
The
yi curves resemble sinusoids with P1, P2 and P3(
:
"mirror image''), and those
with P4 and P5 double sinusoids (Figs. 1b-f).
The
minima provide more accurate
P1, ..., P5 (Figs. 1g-k),
and the RSch trial values
.
The RSch bootstrap with
gives the final P1, ..., P5.
Of these,
has the smallest
,
that for
being comparable (Figs. 1l-p).
The critical levels for rejecting H0 with m=55 are not significant,
not even for P1 (Fig. 1l:
).
Three alternatives could explain this:
(1) The errors
are not correct, and
is unreliable.
(2) The errors are correct, but the model is not,
e.g. the order
may be too low,
or perhaps the light curve evolves during
.
(3) A few erroneous observations can contaminate the
determined by four normalized magnitudes
at each ti (i.e. one in each UBVR passband).
Hence we can not use
to reject H0 for these data.
Paper I (AV changes in Sect. 3.2.) gives a counterexample,
where TSPA modelling can apply this criterion.
The lines connecting each
to the closest point of the model
determine the phase
residuals
(Figs. 1l-p).
The linear correlation coefficient
between
and
is smallest for P1,
but of the same order as that for P5 (Figs. 1q and u).
The highly improbable
for P2, P3 and P4 reveal
that these periods are indeed spurious. In conclusion,
the best period is P1 with the smallest
and lowest
.
The double sinusoid with P5 imitates the solution with P1.
The
RSch bootstrap not only provides the P error estimate,
but also those of M (mean), A (total amplitude),
tmin,1 and
tmin,2
(epochs of primary and secondary minima).
Figure 2 summarizes the earlier P1 bootstrap of Fig. 1l.
The
FS(u) (Eq. 12)
for the
residuals
does not cause
HG rejection
with
(Fig. 2b, Eq. 14), i.e.
this "empirical distribution'' of
(Eq. 11)
is Gaussian.
The M and P distributions are also Gaussian (Figs. 2c-f).
The model gives these theoretical
M and P estimates directly,
but those of A and
tmin,1 are measured
from the model for each
to avoid
the complicated theoretical solutions with
.
That these A and
tmin,1 distributions are also Gaussian,
confirms the validity of our measurement approach (Figs. 2g-j).
Note that SET=42 has no secondary minimum
tmin,2with
,
and that the primary minimum phase is
(Fig. 2i).
In conclusion, the
,
,
,
and
bootstrap statistics for SET=42 are reliable.
The model parameter error estimates in this paper utilize
bootstrap samples during the RSch.
This ensures reliable statistics,
because these estimates usually stabilize already at
.
For example, increasing the number of samples from
to 200
in the RSch of Figs. 2c and e
gave the following error estimates for the mean (
)
and the period (
)
S | 25 | 50 | 75 | 100 | 150 | 200 |
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0.0058 | 0.0054 | 0.0050 | 0.0052 | 0.0051 | 0.0052 |
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0.0042 | 0.0041 | 0.0040 | 0.0040 | 0.0042 | 0.0042 |
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|
Among detected P1, ..., P5 |
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Smallest ![]() |
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Smallest
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The TSPA for SET=42 posed no serious problems (Sect. 6.1),
but "pathological'' cases are not rare for real data,
and analysing the normalized UBV magnitudes of
SET=114 serves as such a "good'' counterexample.
The "real''
periodicity is not the best one detected by
PSch (Fig. 3a), and TSPA reveals
that
has the smallest
(Figs. 3l-p).
The P1, ..., P5 and
connections are obvious
(Eq. 16).
All five periods reach extreme critical levels
(
),
although the residuals appear extraordinary large.
These
are extreme,
because the data accuracy is equal or below the UBVlight curve amplitudes
,
and
during SET=114
(Paper I, Table 1).
But lowering the modelling order, e.g.
=constant,
would confuse the time series analysis,
it being crucial that the same model
is used for all subsets to obtain M, A, P,
tmin,1 and
tmin,2.
As expected, the
periodicity
during SET=114 (Fig. 3m) is
less accurate than that of
during SET=42
with high
(Paper I, Table 1).
Nevertheless, the 3.34 signal detection in
SET=114 confirms that we are not modelling "noise''.
The low UBV amplitudes in SET=114 also
explain the absence of correlations in Figs. 3q-u.
The
RSch bootstrap reveals other
"unpleasant'' results for SET=114 (Fig. 4):
The P distribution is not Gaussian (Figs. 4e and f),
and a secondary minimum (
tmin,2) is present,
but only in
samples (Figs. 4k and l).
The next Sect. 6.3 clarifies how
this type of apparently confusing results were interpreted
in Paper I.
For
and
in Paper I,
three rules were found sufficient for the TSPA modelling of any particular
SET of normalized magnitudes of V 1794 Cyg:
For example,
HG is rejected for P in SET=114 (Fig. 4f),
and
RI excludes the
P,
tmin,1 and
tmin,2 estimates.
RIII alone would exclude
tmin,2 with
(Figs. 4k and l).
The mean (my) and
the standard deviation (sy) of the data
in subsets with
(i.e. all normalized subsets)
are connected to the mean (M) and
the total amplitude (A) of the TSPA model.
The linear approximations
and
are very accurate.
Note that the criteria
RI,
RII and
RIII are therefore
not used to reject the M or A estimates.
Furthermore, my and sy are independent of P,
but
tmin,1 and
tmin,2 are not.
Thus the TSPA (or any other) M and A modelling
could be substituted with the above
my and sy relations
in subsets with an adequate phase coverage.
These my and sy can be used for the same purposes
(e.g. Donahue et al. 1997) that we use M and A in Paper I.
Our
RII states the experimental result that the
RI rejections occur mostly with
.
This is understandable for
free model parameters
when one night covers only about
Pphot/10 for V 1794 Cyg.
Table 3 in Paper I summarizes the TSPA of all normalized
subsets of V 1794 Cyg, and the
RI,
RII or
RIII rejections.
Our Table 1 confirms that the
periodicity is real,
which would appear far from trivial,
were there several subsets similar to SET=114.
We summarize the TSPA combined with the best window period P0determined separately for each SET of Paper I.
The first line shows that
is among the five best periods in 84/93
cases for TSPA between
and
(nine
values in Table 3 of Paper I were
detected with
and
).
The spurious
period is detected nearly as often
(83/93), but the detection rates for the other spurious periods are lower,
especially for
.
The next lines in Table 1 rate each period,
if detected.
The 2nd and 3rd lines confirm that
is undoubtedly the best period
with the
(best model) and
(not spurious) criteria.
The 4th line lists
HR rejections with
,
i.e.
when a high
between
and
implies spurious periodicity.
This occurs more frequently for periods other than
.
Only
,
,
or their
multiples reach extreme critical levels
(e.g. Figs. 1r-t:
).
In conclusion, our Table 1 illustrates the probability
for obtaining a spurious (i.e. false) period for some arbitrary object.
The above V 1794 Cyg light curve analysis was
performed with a second order TSPA.
Here we study the V light curve of the cepheid variable BL Her
from Moffett & Barnes (1984).
The complicated shape of this light curve required a higher order model.
Several details of this shape are undoubtedly real,
because the total amplitude of the brightness variations (
)
is nearly 100 times larger than the internal accuracy of these data.
Our fifth order TSPA (
)
between
and
gave the best period of
(Fig. 5),
and confirmed the 1.307443 estimate in Moffett & Barnes (1984).
This periodicity certainly reached the best
among all period candidates (Figs. 5l-p),
but the
internal error in Vyields
.
Considering that the external error of the transformation into the standard Johnson system was "nearly as good'' as the internal error
(Moffett & Barnes 1984),
the above
should be divided by an unknown factor larger than two.
Three of the other period candidates are nearly multiples of P1, i.e.
,
and
.
The P5 periodicity is also not induced by the
window period, but it may be connected to the
277d
gap within the data and/or the
446d time span of the whole data.
Since these spurious periodicities are not connected to P0,
the phase residual correlations are not significant (Figs. 5q-u).
The RSch bootstrap with P1 confirmed that the
modelling statistics are reliable,
because the
,
,
,
,
and
distributions
are all Gaussian (Fig. 6).
Note also that the secondary minimum
tmin,2
is present in
bootstrap samples (Figs. 6kl).
The nonvariable star SAO50205 (B8II) has been used
as the primary comparison star in the differential photometry of V 1794 Cyg.
The long-term constant brightness of this object was verified in Paper II,
where it was also noted that no periodicity
was detected in the short-term brightness.
The V magnitudes of SAO50205 measured with the Automatic Photoelectric
Telecope (APT) during four subsets SET=111-114 are studied here.
If the selected model
for these
values were
their mean of 7.350,
the
external error of these APT data
would give
having
(Eq. (10):
and
).
In other words, a constant brightness model would suffice.
But to illustrate a case of "pure noise'',
the analysis of these data with the first order TSPA (
)
between
and
is presented in Fig. 7.
The PSch periodogram
is nearly featureless,
except for the weak minima close to the frequencies of 1 and 2
(Fig. 7a).
Such integer values usually indicate spurious periodicity.
The five best period candidates were divided into two groups when
inferring their origin.
The periods of P1 and P4 belong to the first group.
They are window periods inducing long gaps in the phase distribution
of the data (Figs. 7b and e).
Both periodicities are connected to the best window period
and the whole
time span of the data.
The combinations are
and
.
The measurements follow a weak slope spanning about 0.5 in phase.
The gaps in the phases of the data allow a reasonable fit of
the
model to these slopes.
The second group containing P2, P3 and P5 is a more complicated case.
These three periods are connected to
,
which would have been the best period, if the TSPA had been performed
from
to
.
The
periodogram has one weaker minimum
at
(Fig. 7a).
The model with P'' would reach
,
which is comparable to
with P2, P3 and P5.
Combining P'' to the window period
yields
,
and
.
The low total amplitude of the corresponding models prevented us from
utilizing the phase correlations in indentifying spurious periodicities
(Figs. 7r, s and u).
This problem was solved by performing the same TSPA to the 19 other
available subsets of V photometry of SAO50205.
These additional data revealed no signatures of
.
Hence P'' represents an artifact only present in SET=111-114,
where it induces the "detection'' of the P2, P3 and P5
periodicities.
Since this TSPA tested
independent frequencies,
the "best'' period of
with
does not reach the significance level of the constant brightness
model with
,
which was discussed before performing the TSPA analysis.
Although the accuracy of the data (
)
was comparable to
the total amplitude of the model (
),
there was no need to reject the Gaussian hypothesis (
HG)
for any of the model parameter estimates in
the RSch bootstrap with P2 (Fig. 8).
The above analysis of the V magnitudes of SAO50205
illustrates the difficulties encountered in
confirming the case of "pure noise'' for real data with the
-criterion (Eq. 10).
In conclusion, one must know the accuracy of the data
and infer the contribution of the window period(s).
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