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Astron. Astrophys. 355, 743-750 (2000) 3. Fitting the GOLF dataThe GOLF series used covers the 805 days between April 11, 1996 and June 25, 1998, with more than 99% continuity. The GOLF raw data have been converted to velocities using the calibration techniques described by García (private communication) prior to carrying out an FFT transform on the entire series, with a sampling time of 80 seconds. Only the GOLF detector PM2 has been used in this analysis. The classical fitting technique in this domain consists of fitting
a simple Fourier power spectrum, often using codes derived from those
offered by Appourchaux et al. (1998). For such a spectrum,
The entire analysis was limited to the spectral range 2000
A critical point is the choice of the spectral window used for
fitting the p-modes profiles, i.e. how much of the spectrum we fit at
a time. Some workers choose to fit the entire p-mode spectrum,
arguing that this is the only way to correctly take account of the
effect of the far wings from distant modes (Roca Cortes et al. 1998).
This can be done only if the model profile assumed for the modes is
valid everywhere in the window or if the residual errors are
negligible compared with errors due to the stochastic noise. It also
assumes that the overlapping far wings are additive on a scale of
spectral power, which is not evident. As the Nigam formula used in
this paper is obtained by a Taylor expansion around the eigenfrequency
of the mode (Nigam & Kosovichev 1998), we adopted the approach of
fitting only those close multiplets that have an evident overlap, i.e.
fitting was carried out over limited spectral ranges with the
neighbouring Here, the splitting is defined as the mean for each multiplet of
the separation between the modes
The uncertainty quoted here for each parameter determined is the statistical error obtained from the fitting program, using appropriately the covariance matrix of the fit. We performed Monte Carlo simulations (based on a method developed by Fierry Fraillon et al. 1997) which confirm the reality of these uncertainties. ![]() ![]() ![]() ![]() © European Southern Observatory (ESO) 2000 Online publication: March 9, 2000 ![]() |