A zoology of boundary layers.

David Gérard-Varet; Emmanuel Grenier

RACSAM (2002)

  • Volume: 96, Issue: 3, page 401-410
  • ISSN: 1578-7303

Abstract

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In meteorology and magnetohydrodynamics many different boundary layers appear. Some of them are already mathematically well known, like Ekman or Hartmann layers. Others remain unstudied, and can be much more complex. The aim of this paper is to give a simple and unified presentation of the main boundary layers, and to propose a simple method to derive their sizes and equations.

How to cite

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Gérard-Varet, David, and Grenier, Emmanuel. "A zoology of boundary layers.." RACSAM 96.3 (2002): 401-410. <http://eudml.org/doc/40945>.

@article{Gérard2002,
abstract = {In meteorology and magnetohydrodynamics many different boundary layers appear. Some of them are already mathematically well known, like Ekman or Hartmann layers. Others remain unstudied, and can be much more complex. The aim of this paper is to give a simple and unified presentation of the main boundary layers, and to propose a simple method to derive their sizes and equations.},
author = {Gérard-Varet, David, Grenier, Emmanuel},
journal = {RACSAM},
keywords = {Meteorología; Magnetohidrodinámica; Rotación terrestre; Fluidos incompresibles; Capa límite; Ecuaciones diferenciales en derivadas parciales},
language = {eng},
number = {3},
pages = {401-410},
title = {A zoology of boundary layers.},
url = {http://eudml.org/doc/40945},
volume = {96},
year = {2002},
}

TY - JOUR
AU - Gérard-Varet, David
AU - Grenier, Emmanuel
TI - A zoology of boundary layers.
JO - RACSAM
PY - 2002
VL - 96
IS - 3
SP - 401
EP - 410
AB - In meteorology and magnetohydrodynamics many different boundary layers appear. Some of them are already mathematically well known, like Ekman or Hartmann layers. Others remain unstudied, and can be much more complex. The aim of this paper is to give a simple and unified presentation of the main boundary layers, and to propose a simple method to derive their sizes and equations.
LA - eng
KW - Meteorología; Magnetohidrodinámica; Rotación terrestre; Fluidos incompresibles; Capa límite; Ecuaciones diferenciales en derivadas parciales
UR - http://eudml.org/doc/40945
ER -

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