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Ocean wave heave time series as the sum of nonharmonic sinusoids

✍ Scribed by K.E. Steele


Publisher
Elsevier Science
Year
1999
Tongue
English
Weight
359 KB
Volume
26
Category
Article
ISSN
0029-8018

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✦ Synopsis


A discrete wave displacement time-series record is usually analyzed by a Discrete Fourier Transform (DFT), which represents the record as the sum of a finite number of harmonic sinusoids. When the dominant sinusoid of the record is not one of these harmonics, DFT "leakage" produces a distorted picture of the dominant wave, particularly for records not much longer than the largest period in the record. This paper proposes a non-Fourier method for determining the dominant wave period that is applicable even when the record is short relative to the largest period present in the record.