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Ding Pingxing,Kong Yazhen,Sun Fu. 1996. Bispectrum and asymmetry of wave shape. Acta Oceanologica Sinica, (3):297-305
Bispectrum and asymmetry of wave shape
Bispectrum and asymmetry of wave shape
Received:October 23, 1995  Revised:May 17, 1996
DOI:
Key words:Bispecrum  wave shape  asymmetry  nonlinear
中文关键词:  Bispecrum  wave shape  asymmetry  nonlinear
基金项目:This project was supported by the Excellent Talent Foundation across the Century of State Educational Commission.
Author NameAffiliation
Ding Pingxing State Key Laboratory Of Estuarine and Coastal Research, Institute of EStuarine and Coastal Research, East China Normal University, Shanghai 200062, China 
Kong Yazhen State Key Laboratory Of Estuarine and Coastal Research, Institute of EStuarine and Coastal Research, East China Normal University, Shanghai 200062, China 
Sun Fu Laboratory of Physical Oceanography, Ocean University of Qingdao, Qingdao 266003, China 
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Abstract:
      Based on the definition and concept introduced in this paper,the theoretical expression of surface slope bispectrum for two-dimensional random waves is derived.Furthermore,the skewness of surface elevation distribution and that of surface she distribution are respectively employed to define the up-down and front-back asymmetry of a waves hape so that the relations between bispectrum and skewness are proposed.Through these relations,the updown end front-back asymmetry of the wave shape can be quantitatively determined by means of the bispectral analyses of observed wave data.
中文摘要:
      Based on the definition and concept introduced in this paper,the theoretical expression of surface slope bispectrum for two-dimensional random waves is derived.Furthermore,the skewness of surface elevation distribution and that of surface she distribution are respectively employed to define the up-down and front-back asymmetry of a waves hape so that the relations between bispectrum and skewness are proposed.Through these relations,the updown end front-back asymmetry of the wave shape can be quantitatively determined by means of the bispectral analyses of observed wave data.
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