The command SINEFIT/TSA serves two purposes: a) least squares
estimation of the parameters of a detected signal and b) filtering the
data for a given frequency (so-called prewhitening). The trend
removal (zero frequency) constitutes a special case of this filtering.
For a pure sinusoid model, the
statistic used in SINEFIT/TSA is related to that used in SCARGLE/TSA (Lomb, 1976,
Scargle, 1982).
We recommend this statistic for larger data sets and for the detection of smooth, nearly sinusoidal signals, since then its test power is large and the statistical properties are known. In particular the expected value is 1. For observations correlated in groups of size ncorr, divide the value of the Scargle statistics by ncorr(Sect. 12.2.4). The slow algorithm implemented here is suitable for modest numbers of observations. For a faster, FFT based version see Press and Rybicki (1991).
SINEFIT/TSA returns also the table of the residuals X(r) (i.e. of the observations with the fitted oscillation subtracted) in a format suitable for further analysis by any method supported by the TSA package. In this way, the command can be used to perform a CLEAN-like analysis manually by removing individual oscillations one by one in the time domain (see Roberts et al., 1987, Gray & Desikhary, 1973). Since in most astronomical time series the number of different sinusoids present is quite small, we recommend this manual procedure rather than its automated implementation in frequency space by the CLEAN algorithm.
Alternatively, the command can be used to remove a trend from data.
In order to use SINEFIT/TSA for a fixed frequency, specify one
iteration only. The corresponding value of
may in principle
be recovered from the standard deviation
,
where
df=nobs-nparm and
nobs and nparm are the number of observations and the number
of Fourier coefficients (including the mean value), respectively.
However, the computation of the
periodogram with SINEFIT/TSA is very cumbersome while the results should correspond
exactly to the Scargle periodogram (Scargle, 1982, Lomb, 1976).
Among all statistics named in this chapter, AOV used by ORT/TSA
and AOV/TSA is the only one with
exactly known statistical properties even for small samples. On large
samples, AOV is not less sensitive than other statistics using phase
binning, i.e. the step function model: ,
Whittaker & Roberts
and PDM. Therefore we recommend the ORT/TSA and AOV/TSA
commands for samples of all sizes and particularly for
signals with narrow sharp features (pulses,
eclipses). If on the average ncorr consecutive observations are
correlated, divide the value of the periodogram by ncorr and
use the
F(n-1,no/ncorr-n) distribution (Sect. 12.2.4).
For smooth light curves use low order, e.g. 4 or 3, for optimal
sensitivity. For numerous observations and sharp light curves use phase
bins of width comparable to that of the narrow features (e.g. pulses,
eclipses). Note that phase coverage and consequently quality of the
statistics near 0 frequency are notoriously poor for most observations.