Ekman layers of rotating fluids, the case of well prepared initial data

E. Grenier; N. Masmoudi

doi:10.1080/03605309708821290

Ekman layers of rotating fluids, the case of well prepared initial data

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Abstract

In this paper we study the convergence of weak solutions of the Navier Stokes equations with a large Coriolis term as the Rossby and Ekman numbers go to zero, and in particular the so called Ekman boundary layers, and justify some classical expansions in geophysical fluid dynamics (see [14], chapter 4).

Original language	English (US)
Pages (from-to)	213-218
Number of pages	6
Journal	Communications in Partial Differential Equations
Volume	22
Issue number	5-6
DOIs	https://doi.org/10.1080/03605309708821290
State	Published - 1997

ASJC Scopus subject areas

Analysis
Applied Mathematics

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10.1080/03605309708821290

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title = "Ekman layers of rotating fluids, the case of well prepared initial data",

abstract = "In this paper we study the convergence of weak solutions of the Navier Stokes equations with a large Coriolis term as the Rossby and Ekman numbers go to zero, and in particular the so called Ekman boundary layers, and justify some classical expansions in geophysical fluid dynamics (see [14], chapter 4).",

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AU - Grenier, E.

AU - Masmoudi, N.

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AB - In this paper we study the convergence of weak solutions of the Navier Stokes equations with a large Coriolis term as the Rossby and Ekman numbers go to zero, and in particular the so called Ekman boundary layers, and justify some classical expansions in geophysical fluid dynamics (see [14], chapter 4).

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JO - Communications in Partial Differential Equations

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Ekman layers of rotating fluids, the case of well prepared initial data

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