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

E. Grenier^*
, N. Masmoudi

^*Corresponding author for this work

École normale supérieure
CNRS
Université Paris Dauphine

Research output: Contribution to journal › Article › peer-review

91 Citations (Scopus)

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
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
Publication status	Published - 1997
Externally published	Yes

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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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Y1 - 1997

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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).

UR - https://www.scopus.com/pages/publications/0001052077

U2 - 10.1080/03605309708821290

DO - 10.1080/03605309708821290

M3 - Article

AN - SCOPUS:0001052077

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VL - 22

SP - 213

EP - 218

JO - Communications in Partial Differential Equations

JF - Communications in Partial Differential Equations

IS - 5-6

ER -

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

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