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A three-dimensional ocean general circulation model for mesoscale eddies——Ⅱ Diagnostic analysis

A three-dimensional ocean general circulation model for mesoscale eddies——Ⅱ Diagnostic analysis

作     者:Moto Ikeda 

作者机构:Graduate School of Environmental Earth Science Hokkaido University Sapporo Japan 060. 

出 版 物:《Acta Oceanologica Sinica》 (海洋学报(英文版))

年 卷 期:1997年第16卷第1期

页      面:29-43页

核心收录:

学科分类:07[理学] 0707[理学-海洋科学] 

主  题:Diagnostic analysis A three-dimensional ocean general circulation model for mesoscale eddies 

摘      要:A three-dimensional density field associated with mesoscaie unstable waves generated by the 3-D, primitive-equation model (Wang and Ikeda, 1996) is provided to the quasi-geostrophic pressure tendency and ω-equations, and to the (ageostrophic) Q-vector equation. Diagnostic analyses, analogous to the approaches in meteorology: ω-equation and Q-vector method, are for the first time developed to examine the mesoscaie dynamical processes and mechanisms of the unstable waves propagating in the mid-latitude ocean. The weaknesses and strengths of these two diagnostic approaches are evaluated and compared to the model results. The Q-vector method is then recommended to diagnose the vertical motion associated with the mesoscaie dynamics from a hydrographic CTD (conductivity-temperature-depth) array, while the quasi-geostrophic equations produce some small-scale features (errors) in the diagnosed fields.

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