The search for periodicities in all the time series was performed by calculating
the Scargle normalized periodograms
(Scargle 1982).This
technique (see Horne & Baliunas 1986) has several advantages over the conventional fast
Fourier transformation method and provides, through FAP, a simple estimate of
the significance of the height of a peak in the power spectrum. However, the FAP
value is easy to calculate only for that time series for which the successive data
are independent. In our case, the all analysed time series were prepared from
the daily values of the different solar indices which are not independent but
correlated with a characteristic correlation time of a week (Oliver & Ballester 1995).
Therefore, for all our FAP calculations used to estimate the statistical
significance of a peak z, in the Scargle power spectrum, we applied the formula
,
where N
is the number of independent frequencies, k is the normalization factor
due to data correlation and zm = z/k the normalized power
(Bai & Cliver 1990; Bai 1992b).
To determine the normalization factor k for the given time series we
followed the procedure described by Bai & Cliver (1990). The key step of this
procedure is the choice of a spectral window as well as the number of
independent frequencies. Since we would like to analyse naturally limited time series
connected with two different phases of the solar cycle over the largest possible
range of periods, we took the interval 43 to 1447 nHz (8-270 days)
as the spectral window for all the investigated time series. The shortest period, 8 days,
is connected with a possible range of correlations of the analysed data
(see Tables 2 and 3 where the autocorrelation coeficients with the lag = 1 day
and lag = 7 days are given). The longest periods, 270 days,
results from the actual length of the minimum time series equal to 540 days.
The number of totally independent frequencies inside the chosen window is
given by the value of the independent Fourier spacing,
,
where T is the time span of the data
(Scargle 1982). In the case of our time series,
days
and
nHz for the minimum,
while for the rising phase
days and
nHz. However,
de Jager (1987) has shown by Monte-Carlo
simulations that the Fourier powers taken at intervals of one-third of the independent
Fourier spacing are still statistically independent. Thus, we accepted the numbers
198 and 259 as the numbers of independent frequencies in the chosen window
for the minimum and the rising phase time series, respectively.
To illustrate the method used for determination of the normalization
factor k, we will process one of our time series step by step; as an example
we take the ISN time series in the minimum phase. First, we calculate
the Scargle power normalized by the variance of the data,
(Horne & Baliunas 1986) for
all 198 independent frequencies which allows us to construct the graph presented
in Fig. 2a. This shows the cumulative number of frequencies for
which the Scargle power exceeds a certain value z.
Then we fit all values of power z < 5 to the equation
,
which gives the value of the normalization factor k equal 2.59, since when
the formula for FAP reduces to
.
Finally, we
normalize the power spectrum once more by dividing the Scargle power by 2.59 to
obtain the normalized periodogram for which FAP values are easily calculated.
Therefore, if we substitute z = 30.54, k =2.59, and N = 198 in the FAP
formula we get the normalized power
and
FAP = 0.0015 for the highest peak in the ISN minimum time series
periodogram. Figure 2b presents this normalized
periodogram of the minimum ISN series together with FAP significance
levels obtained from FAP formula with N = 198 and k = 2.59.
The highest | Auto | k | NP | FAP | % | The highest | Auto | k | NP | FAP | % | ||||||
peak at | correlation | [%] | of | peak at | correlation | [%] | of | ||||||||||
Freq. | Per. | lag | var. | Freq. | Per. | lag | var. | ||||||||||
[nHz] | [day] | 1 | 7 | exp. | [nHz] | [day] | 1 | 7 | exp. | ||||||||
1 | 2 | 3 | 4 | 5 | 6 | 7 | 1 | 2 | 3 | 4 | 5 | 6 | 7 | ||||
ISN | MMF | ||||||||||||||||
0 | 84a | 138 | .839 | .126 | 2.59 | 11.8 | 0.15 | 17.4 | 0 | 858a | 13.5 | .523 | -.187 | 1.56 | 19.0 | 0.00 | 12.6 |
-1 | 419a | 27.6 | .476 | -.079 | 1.54 | 19.0 | 0.00 | 23.8 | |||||||||
-2 | 400a | 28.9 | .390 | -.095 | 1.65 | 13.7 | 0.02 | 30.0 | |||||||||
SVC 405 | RRE 405 | ||||||||||||||||
0 | 418a | 27.7 | .801 | .007 | 2.50 | 19.8 | 0.00 | 21.0 | 0 | 416a | 27.8 | .714 | .014 | 2.25 | 23.4 | 0.00 | 22.6 |
SVC 810 | RRE 810 | ||||||||||||||||
0 | 423a | 27.4 | .905 | .177 | 1.56 | 49.9 | 0.00 | 35.9 | 0 | 418a | 27.7 | .801 | .218 | 1.46 | 42.9 | 0.00 | 26.4 |
-1 | 396a | 29.2 | .895 | .285 | 1.71 | 18.7 | 0.00 | 45.2 | -1 | 152a | 76.2 | .765 | .346 | 1.70 | 27.7 | 0.00 | 40.6 |
-2 | 150b | 77.2 | .883 | .321 | 1.89 | 15.6 | 0.00 | 52.1 | -2 | 381a | 30.4 | .707 | .216 | 2.06 | 15.3 | 0.00 | 48.8 |
-3 | 76b | 152 | .874 | .228 | 2.01 | 14.1 | 0.01 | 57.7 | -3 | 268b | 43.2 | .667 | .242 | 2.07 | 11.8 | 0.14 | 54.2 |
-4 | 529b | 21.9 | .852 | .105 | 2.10 | 11.2 | 0.28 | 61.9 | |||||||||
-5 | 238b | 48.6 | .836 | .164 | 2.11 | 11.5 | 0.20 | 66.0 | |||||||||
SVC 1215 | RRE 1215 | ||||||||||||||||
0 | 424a | 27.3 | .912 | .219 | 1.60 | 34.6 | 0.00 | 26.7 | 0 | 157a | 73.7 | .757 | .271 | 1.72 | 18.8 | 0.00 | 13.7 |
-1 | 80b | 145 | .905 | .297 | 1.72 | 14.8 | 0.01 | 34.5 | -1 | 420a | 27.6 | .718 | .160 | 1.91 | 18.7 | 0.00 | 26.7 |
-2 | 151b | 76.6 | .893 | .207 | 1.79 | 15.0 | 0.01 | 41.8 | -2 | 383b | 30.2 | .683 | .221 | 1.93 | 12.2 | 0.10 | 34.3 |
-3 | 528b | 21.9 | .886 | .112 | 1.90 | 12.1 | 0.11 | 47.5 | -3 | 267b | 43.4 | .649 | .233 | 1.89 | 11.8 | 0.14 | 40.6 |
-4 | 113b | 102 | .873 | .176 | 1.94 | 11.5 | 0.20 | 52.9 | |||||||||
-5 | 498b | 23.2 | .855 | .084 | 1.95 | 11.8 | 0.15 | 57.8 | |||||||||
-6 | 242b | 47.8 | .839 | .129 | 2.18 | 11.8 | 0.15 | 62.5 | |||||||||
SVC 1620 | RRE 1620 | ||||||||||||||||
0 | 425a | 27.2 | .898 | .111 | 2.15 | 23.1 | 0.00 | 25.0 | 0 | 155b | 74.7 | .687 | .197 | 2.00 | 11.7 | 0.16 | 10.6 |
-1 | 420b | 27.6 | .653 | .123 | 2.07 | 11.2 | 0.28 | 19.3 | |||||||||
-2 | 382b | 30.3 | .627 | .159 | 2.12 | 10.8 | 0.40 | 27.2 | |||||||||
SVC 2800 | RRE 2800 | ||||||||||||||||
0 | 85b | 136 | .931 | .134 | 2.38 | 13.0 | 0.05 | 17.4 | 0 | 383b | 30.2 | .647 | .044 | 2.32 | 7.8 | 7.78 | 7.6 |
-1 | 424a | 27.3 | .921 | .020 | 2.57 | 13.5 | 0.03 | 28.0 | |||||||||
SVC 4995 | RRE 4995 | ||||||||||||||||
0 | 90a | 129 | .862 | .286 | 2.00 | 18.3 | 0.00 | 14.3 | 0 | 53a | 218 | .710 | .347 | 1.64 | 23.5 | 0.00 | 19.4 |
-1 | 124a | 93.3 | .832 | .166 | 2.20 | 13.9 | 0.02 | 24.6 | -1 | 158a | 73.2 | .625 | .224 | 1.83 | 19.5 | 0.00 | 30.3 |
SVC 8800 | RRE 8800 | ||||||||||||||||
0 | 122b | 94.9 | .635 | .355 | 1.63 | 15.8 | 0.00 | 10.3 | 0 | 156b | 74.2 | .638 | .396 | 1.52 | 16.2 | 0.00 | 10.0 |
-1 | 154b | 75.2 | .593 | .289 | 1.71 | 14.9 | 0.01 | 19.9 | -1 | 121b | 95.6 | .598 | .339 | 1.54 | 14.3 | 0.01 | 18.1 |
-2 | 83b | 139 | .558 | .285 | 1.55 | 11.8 | 0.15 | 24.3 |
The columns of the table show: 1: time series ("-1" indicates that the one sine curve with
period given a row above was removed from the original data, "-2" indicates that the two sine curves with periods given in two rows above were removed from the original data, and so on), 2: frequency and period of
the highest peak in a given time series, a small letter following a frequency value indicates to which
interval of probability ("a": <0.1%, "b": 0.1-1%, "c": 1-5% ) this period belongs to
after the randomising procedure, 3: the autocorrelation coefficients calculated
with two lags equal 1 and 7 days respectively, 4: the normalization factor k computed
according to the procedure described in Sect.3, 5: the normalized power equal to
the Scargle power divided by k, 6: the FAP value resulting from the normalized power,
7: in successive rows a percentage of the original data variance explained by the
prominent sinusoidal signals found in a given type of data.
The highest | Auto | k | NP | FAP | % | The highest | Auto | k | NP | FAP | % | ||||||
peak at | correlation | [%] | of | peak at | correlation | [%] | of | ||||||||||
Freq. | Per. | lag | var. | Freq. | Per. | lag | var. | ||||||||||
[nHz] | [day] | 1 | 7 | exp. | [nHz] | [day] | 1 | 7 | exp. | ||||||||
1 | 2 | 3 | 4 | 5 | 6 | 7 | 1 | 2 | 3 | 4 | 5 | 6 | 7 | ||||
ISN | MMF | ||||||||||||||||
0 | 442a | 26.2 | .906 | .150 | 2.19 | 19.2 | 0.00 | 44.6 | 0 | 799a | 14.5 | .650 | -.415 | 1.54 | 25.8 | 0.00 | 15.5 |
-1 | 127a | 91.1 | .897 | .179 | 2.37 | 13.9 | 0.02 | 49.7 | -1 | 844a | 13.7 | .634 | -.340 | 1.70 | 26.9 | 0.00 | 30.1 |
-2 | 876a | 13.2 | .548 | -.187 | 1.93 | 12.2 | 0.14 | 36.4 | |||||||||
SVC 405 | RRE 405 | ||||||||||||||||
0 | 418a | 27.7 | .731 | .086 | 1.90 | 24.5 | 0.00 | 21.9 | 0 | 418a | 27.7 | .641 | .064 | 2.15 | 15.2 | 0.01 | 9.8 |
-1 | 55a | 210 | .695 | .102 | 2.10 | 14.3 | 0.02 | 28.8 | -1 | 52a | 223 | .609 | .072 | 2.23 | 13.2 | 0.05 | 17.9 |
-2 | 444a | 26.1 | .663 | .017 | 2.15 | 11.1 | 0.39 | 33.9 | |||||||||
SVC 810 | RRE 810 | ||||||||||||||||
0 | 443a | 26.1 | .935 | .215 | 1.01 | 74.0 | 0.00 | 33.0 | 0 | 417a | 27.8 | .863 | .206 | 1.30 | 52.0 | 0.00 | 20.2 |
-1 | 416a | 27.8 | .924 | .300 | 1.21 | 50.4 | 0.00 | 45.4 | -1 | 450a | 25.7 | .842 | .275 | 1.58 | 27.2 | 0.00 | 30.2 |
-2 | 75a | 154 | .918 | .385 | 1.32 | 38.2 | 0.00 | 53.5 | -2 | 56a | 207 | .824 | .323 | 1.74 | 20.3 | 0.00 | 37.4 |
-3 | 456a | 25.4 | .904 | .275 | 1.51 | 20.1 | 0.00 | 58.0 | -3 | 71b | 163 | .806 | .245 | 1.91 | 13.2 | 0.05 | 42.0 |
-4 | 62a | 187 | .893 | .318 | 1.59 | 21.5 | 0.00 | 62.3 | |||||||||
-5 | 103a | 112 | .878 | .239 | 1.67 | 21.4 | 0.00 | 66.4 | |||||||||
-6 | 477a | 24.3 | .861 | .147 | 1.80 | 14.2 | 0.02 | 69.0 | |||||||||
-7 | 385a | 30.1 | .853 | .193 | 1.74 | 15.4 | 0.01 | 71.5 | |||||||||
-8 | 127b | 91.1 | .843 | .205 | 1.76 | 15.2 | 0.01 | 73.9 | |||||||||
-9 | 562b | 20.6 | .829 | .143 | 1.77 | 12.8 | 0.07 | 75.6 | |||||||||
-10 | 498b | 23.2 | .819 | .184 | 1.84 | 12.3 | 0.12 | 77.3 | |||||||||
SVC 1215 | RRE 1215 | ||||||||||||||||
0 | 444a | 26.1 | .957 | .240 | 1.14 | 68.5 | 0.00 | 36.4 | 0 | 418a | 27.7 | .872 | .253 | 1.37 | 33.4 | 0.00 | 14.4 |
-1 | 77a | 150 | .948 | .333 | 1.41 | 38.7 | 0.00 | 46.6 | -1 | 449a | 25.8 | .861 | .303 | 1.52 | 27.6 | 0.00 | 24.9 |
-2 | 416a | 27.8 | .938 | .206 | 1.61 | 35.2 | 0.00 | 55.6 | -2 | 76a | 152 | .845 | .349 | 1.74 | 24.9 | 0.00 | 34.3 |
-3 | 104a | 111 | .935 | .261 | 1.74 | 21.8 | 0.00 | 60.6 | -3 | 59a | 196 | .823 | .261 | 1.88 | 15.7 | 0.00 | 40.0 |
-4 | 457a | 25.3 | .922 | .159 | 1.93 | 14.3 | 0.02 | 64.1 | |||||||||
-5 | 64b | 181 | .912 | .188 | 1.93 | 14.7 | 0.01 | 67.4 | |||||||||
-6 | 129b | 89.7 | .900 | .109 | 2.00 | 14.3 | 0.02 | 70.3 | |||||||||
-7 | 480a | 24.1 | .893 | .035 | 1.94 | 15.2 | 0.01 | 73.0 | |||||||||
-8 | 563b | 20.6 | .888 | .077 | 1.96 | 12.7 | 0.08 | 75.0 | |||||||||
-9 | 499b | 23.2 | .882 | .118 | 2.02 | 13.2 | 0.05 | 77.0 | |||||||||
-10 | 385b | 30.1 | .874 | .158 | 2.04 | 11.9 | 0.18 | 78.7 | |||||||||
-11 | 49b | 236 | .869 | .161 | 2.03 | 10.2 | 0.31 | 80.3 | |||||||||
-12 | 361b | 32.1 | .858 | .116 | 1.92 | 12.6 | 0.09 | 81.9 | |||||||||
-13 | 148b | 78.2 | .850 | .128 | 1.84 | 12.5 | 0.10 | 83.1 | |||||||||
SVC 1620 | RRE 1620 | ||||||||||||||||
0 | 444a | 26.1 | .955 | .250 | 1.44 | 47.7 | 0.00 | 38.6 | 0 | 419a | 27.6 | .831 | .149 | 1.89 | 21.8 | 0.00 | 12.2 |
-1 | 77a | 150 | .946 | .329 | 1.68 | 33.6 | 0.00 | 48.9 | -1 | 78a | 148 | .816 | .181 | 2.03 | 22.6 | 0.00 | 23.8 |
-2 | 416a | 27.8 | .934 | .196 | 1.93 | 25.0 | 0.00 | 56.3 | -2 | 450a | 25.7 | .787 | .061 | 2.26 | 16.1 | 0.00 | 31.9 |
-3 | 128a | 90.4 | .930 | .239 | 2.03 | 17.8 | 0.00 | 61.0 | |||||||||
-4 | 105b | 110 | .920 | .064 | 2.17 | 12.3 | 0.12 | 64.2 | |||||||||
SVC 2800 | RRE 2800 | ||||||||||||||||
0 | 443a | 26.1 | .927 | .251 | 1.47 | 41.0 | 0.00 | 37.9 | 0 | 78a | 148 | .775 | .178 | 1.94 | 21.5 | 0.00 | 11.8 |
-1 | 77a | 150 | .917 | .315 | 1.65 | 34.3 | 0.00 | 47.8 | -1 | 421a | 27.5 | .744 | .066 | 2.13 | 16.7 | 0.00 | 20.7 |
-2 | 416a | 27.8 | .900 | .180 | 1.93 | 19.2 | 0.00 | 53.5 | |||||||||
-3 | 128b | 90.4 | .893 | .207 | 2.09 | 13.4 | 0.04 | 57.2 | |||||||||
-4 | 430b | 26.9 | .883 | .146 | 2.08 | 12.2 | 0.12 | 60.6 | |||||||||
-5 | 487a | 23.8 | .876 | .159 | 1.97 | 15.2 | 0.01 | 64.1 | |||||||||
-6 | 66b | 175 | .868 | .200 | 2.07 | 14.0 | 0.02 | 67.7 | |||||||||
-7 | 52a | 223 | .854 | .112 | 2.16 | 15.6 | 0.00 | 71.2 | |||||||||
SVC 4995 | RRE 4995 | ||||||||||||||||
0 | 442a | 26.2 | .891 | .182 | 1.75 | 31.6 | 0.00 | 37.5 | 0 | 79a | 147 | .755 | .009 | 2.66 | 9.1 | 2.78 | 7.1 |
-1 | 77a | 150 | .870 | .221 | 2.00 | 21.3 | 0.00 | 45.3 | |||||||||
-2 | 420b | 27.6 | .859 | .114 | 2.20 | 11.3 | 0.33 | 49.4 | |||||||||
-3 | 103b | 112 | .856 | .132 | 2.34 | 11.0 | 0.39 | 53.4 | |||||||||
SVC 8800 | RE 8800 | ||||||||||||||||
0 | 79a | 147 | .756 | .365 | 1.74 | 42.7 | 0.00 | 26.9 | 0 | 81a | 143 | .726 | .338 | 1.89 | 33.5 | 0.00 | 19.6 |
-1 | 66a | 175 | .696 | .189 | 2.20 | 25.9 | 0.00 | 40.5 | -1 | 67a | 173 | .668 | .185 | 2.28 | 20.9 | 0.00 | 31.5 |
-2 | 51a | 227 | .617 | .073 | 2.55 | 11.3 | 0.32 | 37.8 |
Since peaks in a periodogram may arise from aliasing or other phenomena not present in Gaussian noise (e.g., spectral leakage arising from the spacing of the data and from the finite length of the time series), the FAP values alone, are insufficient for establishing whether or not strong peaks in a periodogram are indeed real periodicities in the time series. Also, some small peaks present in the original periodogram can be real in the case when the normalized factor k would be too large in consequence of treating real periods as noise. We test for genuine peaks by recomputing the periodogram after randomising the data on the time grid. This procedure (Delache et al. 1985; Özgüç & Ataç 1994) maintains the noise characteristic of the time series but destroys all coherent signals, especially those with periods longer than the chosen cut interval of the data. In our time series, we cut the data with a seven day interval. It preserves to some extent the correlation characteristics of the data, so if a period results from a strong correlation inside the data, the number of cases in which it is observed should be rather large. We repeated this simulation 10000 times, every time computing the number of cases in which the recalculated power values for the periods having peaks in the original spectrum are equal to or larger than the peaks power of the real data. The results of these calculations are presented in Tables 4 and 5 as small letters situated after the frequency of the peaks found in the original periodograms. The letter "a" indicates that, for 10000 simulations, in less then 10 cases the peak value at the given frequency exceeded the corresponding peak power of the real data. Successive letters mark the intervals for which the probability (calculated from 10000 simulations) of obtaining as high a peak as in the original periodogram by chance are as follows: "b": 0.1-1%, "c": 1-5%, "d": 5-15%.
When more than one periodic signal is present in the data, multiple significant
peaks appear in the periodogram. Alternatively, a true signal at frequency
can cause peaks in the periodogram at frequencies
other than
because of the
finite length of the data and irregularities in the data spacing. A useful procedure
for determining whether any additional peaks with significant false alarm
probability are physically real is an iterative peak removal technique
(Delache & Scherrer 1983; Horne & Baliunas 1986).
The highest peak in the original data periodogram provides
the frequency
corresponding to the strongest sinusoidal
signal present in the data. Using the method of least squares the phase and
amplitude of this sinusoidal signal are fitted from the original data.
This allows subtraction of the best fitted sine curve from
the time series and then recalculation of a new
periodogram. This procedure is repeated as long as the FAP of the peaks
connected with subtracted sine curves are smaller than 0.5%, producing the
main periods in each of the analysed time series. To see the effect of removing
these peaks from the original data, we present in Fig. 3 the six consecutive
periodograms, calculated according to this procedure for the case of the minimum
SVC 810 time series. We see that the original periodogram is dominated by
a strong peak at frequency 423 nHz (
), so the structure of the periodogram
near this frequency is difficult to recognise. When the sine curve with this
period is removed from the data, the new period at
begins to be visible
(Fig. 3b). Subtracting the next sine curves from the data we come to Fig. 3f
which presents the periodogram of the last descendant time series having
period whose peak value gives FAP smaller than 0.5%.
Comparing all the periodograms seen in
this figure, we can conclude that the period values indicated by peak positions
do not change much during the removed procedure, which confirms the significance
of the periods found. The results
of the removal procedure are summarised in Table 2 for the minimum and in
Table 3 for the rising phase. Both tables show for the original time series
(marked by 0), and those with successively removed sine curves
(denoted by -1, -2, -3
)
such characteristic parameters as: frequency and period of
the highest peak, the autocorrelation coefficients, the normalization factor k,
the normalized power equal to the Scargle power divided by k, the FAP value
resulting from the normalized power.
MMF | SVC | SVC | SVC | SVC | SVC | SVC | SVC | ISN | Line | M | SVC | ISN | Time series | ||
RRE | RRE | RRE | RRE | RRE | RRE | RRE | [nHz] | [day] | RRE | Imp. | NP | FAP | |||
405 | 810 | 1215 | 1620 | 2800 | 4995 | 8800 | ![]() |
[% ] | |||||||
1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 | 11 | 12 | 13 | 14 | 15 | 16 |
858a | 851c | 846d | 845d | 854.5 | 13.5 | a | c | - | MMF/0 | ||||||
851d | 13 | + | 6 | 19.0 | 0.00 | ||||||||||
673c | 679c | 679d | 675c | 674b | 672b | 672b | 673.0 | 17.2 | - | 2b3c | b | ISN/-1 | |||
662c | 665c | 685c | 23 | 3c | 15 | 6.7 | 20.93 | ||||||||
588d | 585c | 580b | 584c | 584b | 585d | 583c | 586.0 | 19.8 | - | 2b2c | c | SVC 1215/-7 | |||
603d | 594d | 600c | 23 | c | 10 | 8.4 | 4.27 | ||||||||
534b | 529b | 528b | 526b | 526b | 525c | 529b | 528.1 | 21.9 | - | 5bc | b | SVC 1215/-3 | |||
548d | 23 | + | 19 | 12.1 | 0.11 | ||||||||||
491c | 498b | 496.8 | 23.3 | - | bc | - | SVC 1215/-5 | ||||||||
512d | 503d | 504c | 496b | 495b | 497d | 21 | 2bc | 11 | 11.8 | 0.15 | |||||
419a | 418a | 423a | 424a | 425a | 424a | 424b | 432a | 423.5 | 27.3 | a | 5ab | a | SVC 810/0 | ||
416a | 418a | 420a | 420b | 434c | 432c | 18 | 3ab2c | 58 | 49.9 | 0.00 | |||||
400a | 396a | 397b | 398c | 398c | 397.8 | 29.1 | a | ab2c | - | SVC 810/-1 | |||||
4 | - | 15 | 18.7 | 0.00 | |||||||||||
390a | 374c | 372d | 382.6 | 30.3 | - | ac | - | RRE 810/-2 | |||||||
382a | 381a | 383b | 382b | 383b | 386b | 18 | 2a4b | 28 | 15.3 | 0.00 | |||||
307c | 306c | 308d | 299.5 | 39 | - | 2c | - | SVC 810/-6 | |||||||
295d | 293c | 292b | 16 | bc | 6 | 8.2 | 5.14 | ||||||||
286d | 272c | 265d | 275c | 281d | 265d | 270.6 | 43 | + | 2c | - | RRE 810/-3 | ||||
268b | 267b | 266b | 21 | 3b | 11 | 11.8 | 0.14 | ||||||||
238b | 242b | 238d | 240.0 | 48 | - | 2b | - | SVC 1215/-6 | |||||||
4 | - | 6 | 11.8 | 0.14 | |||||||||||
197d | 195c | 197c | 195c | 198c | 217d | 194c | 199.0 | 58 | - | 4c | c | RRE 8800/-3 | |||
217d | 204d | 215c | 23 | c | 6 | 8.9 | 2.55 | ||||||||
150b | 151b | 150c | 147d | 156c | 154b | 154.4 | 75 | - | 3b2c | - | RRE 810/-1 | ||||
143d | 152a | 157a | 155b | 159b | 158a | 156b | 16 | 3a3b | 35 | 27.7 | 0.00 | ||||
125d | 121b | 124a | 122b | 126c | 126.4 | 92 | - | a2b | c | SVC 8800/0 | |||||
136c | 135c | 139d | 121b | 18 | b2c | 17 | 15.8 | 0.00 | |||||||
107c | 113b | 112.7 | 103 | - | bc | - | SVC 1215/-4 | ||||||||
118d | 116d | 118c | 11 | c | 5 | 11.5 | 0.20 | ||||||||
96c | 85b | 90a | 84a | 89.0 | 130 | c | ab | a | SVC 4995/0 | ||||||
88d | 96b | 83b | 13 | 2b | 20 | 18.3 | 0.00 | ||||||||
75b | 76b | 80b | 80b | 74d | 80c | 77.4 | 150 | - | 4bc | - | SVC 1215/-1 | ||||
69c | 82c | 67d | 13 | 2c | 15 | 14.8 | 0.01 | ||||||||
60d | 55c | 56c | 58c | 47c | 54c | 53.0 | 218 | + | 5c | - | RRE 4995/0 | ||||
52c | 52c | 50b | 53a | 13 | ab2c | 15 | 23.5 | 0.00 |
The first nine columns give frequencies of the lines found in the indicated type of data.
The small letter following the frequency denotes the interval to which belongs
the probability to obtain by chance as high a peak at this frequency as in the original
periodogram. The intervals are as follows: "a": <0.1% "b": 0.1-1%, "c": 1-5%,
"d": 5-15%. The bold letters indicate frequencies of the
large peaks having FAP values smaller than 0.5%.
Columns 10 and 11 give the mean frequency and mean period of the line. They are
calculated only from the periods marked by letters "a", "b", "c". The number
under the mean frequency is the difference between the highest and the lowest frequency
from all the periods found.
The next three Cols. 12-14 describe in a shorter way in what type of data
(magnetic, radio, spot numbers) the given line is visible. We mark this using
the letters "a", "b", "c", and two symbols "+" and "-". The symbol "-" means that
the given line is not noticed in the respective type of data.
The letters "a", "b", and "c" indicate that the line is recognised
and the periods found have the probability level described by these
letters, while the symbol "+" indicates that in the given type of data are periods
having the probability level described by the letter "d".
The second row in Col. 14 gives the importance number which indirectly measure
how large is support for this line in all the analysed time series (see text).
The last two columns in the first row, determine the time series in which the highest peak
for the given line have been observed. The second row gives the normalized power
of this peak as well as the resulting FAP value.
MMF | SVC | SVC | SVC | SVC | SVC | SVC | SVC | ISN | Line | M | SVC | ISN | Time series | ||
RRE | RRE | RRE | RRE | RRE | RRE | RRE | [nHz] | [day] | RRE | Imp. | NP | FAP | |||
405 | 810 | 1215 | 1620 | 2800 | 4995 | 8800 | ![]() |
[% ] | |||||||
1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 | 11 | 12 | 13 | 14 | 15 | 16 |
876a | 887b | 887d | 886d | 886c | 883.4 | 13.1 | a | b | c | MMF/-2 | |||||
886d | 886d | 887c | 881c | 11 | 2c | 11 | 12.2 | 0.14 | |||||||
844a | 863c | 864c | 853.2 | 13.6 | a | 2c | - | MMF/-1 | |||||||
841c | 23 | c | 8 | 26.9 | 0.00 | ||||||||||
814a | 823d | 822d | 806.5* | 14.4 | a | + | - | MMF/0 | |||||||
799a | 820d | 24 | a | + | 10 | 25.8 | 0.00 | ||||||||
756a | 762.4 | 15.2 | a | - | - | MMF/-3 | |||||||||
765c | 767c | 763c | 761c | 11 | 4c | 9 | 7.9 | 8.86 | |||||||
565b | 562b | 563b | 566c | 571b | 572b | 572d | 571c | 569.3 | 20.3 | - | 5bc | c | SVC 810/-9 | ||
566b | 572c | 574b | 574b | 579d | 576c | 575d | 17 | 3b2c | 28 | 12.8 | 0.07 | ||||
502c | 498b | 499b | 504b | 497a | 499b | 507d | 499.3 | 23.2 | - | a4bc | + | SVC 1215/-10 | |||
504c | 498d | 496c | 498c | 11 | 3c | 21 | 13.2 | 0.05 | |||||||
477a | 480a | 483b | 487a | 486b | 482.6 | 24.0 | - | 3ab | b | SVC 1215/-7 | |||||
10 | - | 21 | 15.2 | 0.01 | |||||||||||
456a | 457a | 457b | 464d | 453c | 455d | 459.5 | 25.2 | - | 2abc | + | SVC 810/-3 | ||||
467b | 466d | 467c | 14 | bc | 18 | 20.1 | 0.00 | ||||||||
444d | 444a | 443a | 444a | 444a | 443a | 442a | 439b | 442a | 444.4 | 26.0 | + | 6ab | a | SVC 810/0 | |
450a | 449a | 450a | 443b | 11 | 3ab | 56 | 74.0 | 0.00 | |||||||
429b | 429b | 432b | 430b | 431d | 431.7 | 26.8 | - | 4b | - | SVC 2800/-4 | |||||
434d | 434c | 436d | 436b | 7 | bc | 16 | 12.2 | 0.12 | |||||||
418a | 416a | 416a | 416a | 416a | 420b | 415c | 414c | 417.4 | 27.7 | - | 5abc | c | RRE 810/-1 | ||
418a | 417a | 418a | 419a | 421a | 420a | 7 | 6a | 60 | 50.4 | 0.00 | |||||
399a | 399.0 | 29.0 | a | - | - | MMF/-3 | |||||||||
399d | 400c | 398c | 2 | 2c | 7 | 10.8 | 0.54 | ||||||||
377a | 382c | 385a | 385b | 383c | 376d | 382d | 381.1 | 30.4 | a | ab2c | + | SVC 810/-7 | |||
387d | 381b | 381c | 381c | 383c | 383d | 373c | 14 | b4c | 22 | 15.4 | 0.01 | ||||
362b | 361b | 366d | 366c | 363.8 | 31.8 | - | 2bc | - | SVC 1215/-12 | ||||||
365d | 363c | 5 | c | 8 | 12.6 | 0.09 | |||||||||
285d | 284c | 284d | 284c | 283d | 292c | 285c | 287.0 | 40 | - | 3c | c | SVC 1215/-14 | |||
281d | 284d | 290b | 11 | b | 7 | 10.3 | 0.85 | ||||||||
157d | 149d | 146c | 148a | 151c | 152d | 150.0 | 77 | + | b2c | b | SVC 1215/-13 | ||||
141d | 155c | 16 | c | 6 | 12.5 | 0.10 | |||||||||
128b | 127b | 129b | 128a | 128b | 127b | 117d | 127a | 126.8 | 91 | - | a5b | a | SVC 1620/-3 | ||
120c | 12 | c | 26 | 17.8 | 0.00 | ||||||||||
103a | 104a | 105b | 102c | 103b | 103.6 | 112 | - | 2a2bc | - | SVC 1215/-3 | |||||
104c | 104c | 102d | 3 | 2c | 19 | 21.8 | 0.00 | ||||||||
85a | 98c | 88d | 88d | 93c | 91.6 | 126 | - | a2c | - | SVC 405/-3 | |||||
86c | 96b | 13 | bc | 11 | 9.6 | 1.70 | |||||||||
75a | 77a | 77a | 77a | 77a | 79a | 74b | 76.8 | 151 | - | 6a | b | SVC 8800/0 | |||
71b | 76a | 78a | 78a | 79a | 81a | 10 | 5ab | 61 | 42.7 | 0.00 | |||||
62a | 64b | 65c | 66b | 67d | 66a | 64.1 | 181 | - | 2a2bc | - | SVC 8800/-1 | ||||
59a | 65d | 64b | 67a | 8 | 2ab | 30 | 25.9 | 0.00 | |||||||
55a | 56a | 49b | 52a | 51b | 52.3 | 221 | - | 3a2b | - | RRE 810/-2 | |||||
52a | 54d | 51a | 7 | 2a | 31 | 20.3 | 0.00 |
* This is the mean value from two close magnetic lines.
![]() |
Figure 5: Same as Fig. 4. but for the rising phase ISN and SVC time series after removing from the original data all the sine curves having periods with FAP values smaller than 0.5%. |
![]() |
Figure 6: Same as Fig. 4. but for the minimum MMF and RRE time series after removing from the original data all the sine curves having periods with FAP values smaller than 0.5%. |
![]() |
Figure 7: Same as Fig. 4. but for the rising phase MMF and RRE time series after removing from the original data all the sine curves having periods with FAP values smaller than 0.5%. |
Copyright ESO 2001