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Qiao Fangli,Zhang Qinghua. 1994. A model of the formation and development of ocean shear wave. Acta Oceanologica Sinica, (3):345－359
A model of the formation and development of ocean shear wave
A model of the formation and development of ocean shear wave
Received:August 27, 1993  Revised:November 10, 1993
DOI：
Key words:Shear wave  pseudospectral method  large eddy simulation
中文关键词:  Shear wave  pseudospectral method  large eddy simulation
基金项目:
Author NameAffiliation
Qiao Fangli First Institute of Oceanography, state oceanic Administration, P. O. Box 98, Qingdao 266003, China 
Zhang Qinghua First Institute of Oceanography, state oceanic Administration, P. O. Box 98, Qingdao 266003, China 
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Abstract:
      From quasi-geostrophic vorticity equation,we simulate the formation of ocean shear wave in western boundary strong current area with the pseudospectral method,and idealize the initial velocity into hyperbolic tangent velocity profile,with the unsteady little perturbation developed by means of getting energy from mean motion.The change of isovorticity shows two vortexes merging or splitting between them.The evolving process of material lines reflects cold water's invading and warm water's turning,which is agreeable to satellite photograph.Vonlinear effect makes a new energy distribution in all kinds of motion scale.One important phenomenon is that Reynolds stress will change its sign when the perturbation amplitude is large enough.
中文摘要:
      From quasi-geostrophic vorticity equation,we simulate the formation of ocean shear wave in western boundary strong current area with the pseudospectral method,and idealize the initial velocity into hyperbolic tangent velocity profile,with the unsteady little perturbation developed by means of getting energy from mean motion.The change of isovorticity shows two vortexes merging or splitting between them.The evolving process of material lines reflects cold water's invading and warm water's turning,which is agreeable to satellite photograph.Vonlinear effect makes a new energy distribution in all kinds of motion scale.One important phenomenon is that Reynolds stress will change its sign when the perturbation amplitude is large enough.
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