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The traditional periodogram method of spectral estimation using FFT
is not appropriate for the present analysis because with a 110 year data set,
we could only estimate the spectra at 0.009 cpy, 0.018 cpy,
etc..., i.e. we would not have sufficient frequency resolution at low
frequencies. Further, since windowing of the data would not be possible
for these low frequencies, the standard deviation of the estimate of the
spectra would be as large as the estimate itself [15].
At the higher frequencies, where windowing of the data is possible
(due to which the confidence level in the estimates is higher), and where the
frequency resolution is sufficent, we have verified that the ME spectral
estimates agree with the traditional periodogram spectral estimates.
A disadvantage of the ME method, however, is the problem of spurious
peaks when a large number of poles is used. Consequently,
we prefer to use a smaller number of poles and obtain slightly smoothed
spectra in the present case. There is little drawback in doing this,
since we estimate the spectra in all cases using the same number of
poles. In the next section where we comment on possible important
low-frequency processes, we filter the data before subjecting it to a ME
spectral analysis, so that a spectral estimate with just a few poles will
capture the underlying peaks.
Next: Comparison of the variabilities
Up: Nonhydrostatic Effects in Long
Previous: The Instantaneous Fields
Balasubramany (Balu) Nadiga
1/8/1998