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Book
Hydrodynamic limits of the Boltzmann equation
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ISBN: 3540928464 3540928472 Year: 2009 Publisher: Berlin : Springer,

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Abstract

The aim of this book is to present some mathematical results describing the transition from kinetic theory, and, more precisely, from the Boltzmann equation for perfect gases to hydrodynamics. Different fluid asymptotics will be investigated, starting always from solutions of the Boltzmann equation which are only assumed to satisfy the estimates coming from physics, namely some bounds on mass, energy and entropy.


Book
Hydrodynamic limits of the Boltzmann equation
Author:
ISBN: 9783540928478 9783540928461 Year: 2009 Publisher: Berlin ; London : Springer,

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Abstract

The aim of this book is to present some mathematical results describing the transition from kinetic theory, and, more precisely, from the Boltzmann equation for perfect gases to hydrodynamics. Different fluid asymptotics will be investigated, starting always from solutions of the Boltzmann equation which are only assumed to satisfy the estimates coming from physics, namely some bounds on mass, energy and entropy.


Digital
Hydrodynamic Limits of the Boltzmann Equation
Author:
ISBN: 9783540928478 Year: 2009 Publisher: Berlin, Heidelberg Springer-Verlag Berlin Heidelberg


Book
Mathematical study of the betaplane model : equatorial waves and convergence results
Authors: ---
ISSN: 0249633X ISBN: 9782856292280 Year: 2006 Publisher: Paris : Société Mathématique de France - SMF,


Book
Mathematical study of degenerate boundary layers : a large scale ocean circulation problem
Authors: ---
ISBN: 9781470428358 1470428350 Year: 2018 Publisher: Providence AMS

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Book
Mathematical study of degenerate boundary layers : a large scale ocean circulation problem
Authors: ---
ISBN: 1470444070 Year: 2018 Publisher: Providence, RI : American Mathematical Society,

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Abstract

This paper is concerned with a complete asymptotic analysis as E o 0 of the Munk equation partial _xpsi -E Delta ^2 psi = au in a domain Omega subset mathbf R^2, supplemented with boundary conditions for psi and partial _n psi . This equation is a simple model for the circulation of currents in closed basins, the variables x and y being respectively the longitude and the latitude. A crude analysis shows that as E o 0, the weak limit of psi satisfies the so-called Sverdrup transport equation inside the domain, namely partial _x psi ^0=au , while boundary layers appear in the vicinity of the boundary.

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