A Two-Level Method For The Steady-State Quasigeostrophic Equation
The quasi-geostrophic equations (QGE) are a model of large-scale ocean flows. We consider a pure stream function formulation and cite results for optimal error estimates for finding approximate solutions with the finite element method. We examine both the time dependent and steady-state versions of...
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Virginia Tech
2013
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| Online Access: | http://hdl.handle.net/10919/23090 |