Physics – Geophysics
Scientific paper
Jul 2006
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006jgra..11107103p&link_type=abstract
Journal of Geophysical Research, Volume 111, Issue A7, CiteID A07103
Physics
Geophysics
1
Mathematical Geophysics: Spectral Analysis (3205, 3280), Interplanetary Physics: Solar Wind Plasma, Mathematical Geophysics: Stochastic Processes (3235, 4468, 4475, 7857), Mathematical Geophysics: Time Series Analysis (1872, 4277, 4475)
Scientific paper
The bias in periodogram spectral estimators is computed as a function of the sample size N by assuming a model power spectrum that decays like f-α at high frequencies. For α = 2, it is shown that when the aliasing of the measured power spectrum is properly taken into account the bias in the ``raw'' periodogram is nearly independent of frequency for large N. For the range of values 1.7 $\lesssim$ α <2, an upper bound on the bias is provided by the case α = 2. Theoretical calculations of the maximum absolute bias as a function of N are used to determine when the periodogram is approximately unbiased and when the bias is significant enough to require the use of a modified periodogram which incorporates data tapering, also called data windowing. For solar wind velocity data acquired by the ACE spacecraft and a chosen low frequency cutoff of 10-7 Hz, the bias in periodogram spectral estimators is found to be less than 4% for sample sizes N greater than 216 = 65536. This corresponds to a 49 day record of 64 s data.
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