Partial and Spectral-Viscosity Models for Geophysical Flows

Two models based on the hydrostatic primitive equations are proposed. The first model is the primitive equations with partial viscosity only, and is oriented towards large-scale wave structures in the ocean and atmosphere. The second model is the viscous primitive equations with spectral eddy viscosity, and is oriented towards turbulent geophysical flows. For both models, the existence and uniqueness of global strong solutions are established. For the second model, the convergence of the solutions to the solutions of the classical primitive equations as eddy viscosity parameters tend to zero is also established.

作 者： Qingshan CHEN Max GUNZBURGER Xiaoming WANG   作者單位： Qingshan CHEN,Max GUNZBURGER(Department of Scientific Computing, Florida State University, Tallahassee, FL 32306, USA)

Xiaoming WANG(Department of Mathematics, Florida State University, Tallahassee, FL 32306, USA) 

刊 名： 數(shù)學(xué)年刊B輯（英文版）  ISTIC SCI 英文刊名： CHINESE ANNALS OF MATHEMATICS,SERIES B  年，卷(期)： 2010 31(5)  分類號(hào)： O1  關(guān)鍵詞： Primitive equations   Partial viscosity   Spectral-eddy viscosity  

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