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Qiao Fangli. 1996. Instability analysis of three-dimensional ocean shear waves. Acta Oceanologica Sinica, (1):1-8
Instability analysis of three-dimensional ocean shear waves
Instability analysis of three-dimensional ocean shear waves
Received:November 06, 1995  Revised:November 30, 1995
DOI:
Key words:Shear waves  instability analysis  continuous stratificationn
中文关键词:  Shear waves  instability analysis  continuous stratificationn
基金项目:
Author NameAffiliation
Qiao Fangli First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China 
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Abstract:
      Based on the continuously stratified quasi-geostrophic vorticity equation, the present paper analyses the instability of three-dimensional shear waves.The cause that most shear waves occur on the shelfside of strong currens near the west boundaries of the oceans is presented.The growth rate of small perturbations relies on the stratification charactern, and a maximum value of growth rate exists for certain stratification.
中文摘要:
      Based on the continuously stratified quasi-geostrophic vorticity equation, the present paper analyses the instability of three-dimensional shear waves.The cause that most shear waves occur on the shelfside of strong currens near the west boundaries of the oceans is presented.The growth rate of small perturbations relies on the stratification charactern, and a maximum value of growth rate exists for certain stratification.
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