Aimed at graduate students and researchers in mathematics, engineering, oceanography, meteorology and mechanics, this text provides a detailed introduction to the physical theory of rotating fluids, a significant part of geophysical fluid dynamics. The Navier-Stokes equations are examined in both incompressible and rapidly rotating forms. Series: Oxford Lecture Series in Mathematics & Its Applications. Num Pages: 264 pages, black & white illustrations. BIC Classification: PB; PHDF; PHVG; RBKC. Category: (P) Professional & Vocational; (UP) Postgraduate, Research & Scholarly; (UU) Undergraduate. Dimension: 246 x 166 x 21. Weight in Grams: 518. . 2006. Illustrated. hardcover. . . . . Books ship from the US and Ireland.

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Bibliographic Details

Title: Mathematical Geophysics: An introduction to rotating fluids and the Navier-Stokes equations: 32 (Oxford Lecture Series in Mathematics and Its Applications)
Publisher: OUP Oxford
Publication Date: 2006
Language: English
ISBN 10: 019857133X
ISBN 13: 9780198571339
Binding: Hardcover
Condition: New

About this title

Synopsis

Aimed at graduate students, researchers and academics in mathematics, engineering, oceanography, meteorology, and mechanics, this text provides a detailed introduction to the physical theory of rotating fluids, a significant part of geophysical fluid dynamics. The text is divided into four parts, with the first part providing the physical background of the geophysical models to be analyzed. Part two is devoted to a self contained proof of the existence of weak (or strong) solutions to the imcompressible Navier-Stokes equations. Part three deals with the rapidly rotating Navier-Stokes equations, first in the whole space, where dispersion effects are considered. The case where the domain has periodic boundary conditions is then analyzed, and finally rotating Navier-Stokes equations between two plates are studied, both in the case of periodic horizontal coordinated and those in R2. In Part IV, the stability of Ekman boundary layers and boundary layer effects in magnetohydrodynamics and quasigeostrophic equations are discussed. The boundary layers which appear near vertical walls are presented and formally linked with the classical Prandlt equations. Finally spherical layers are introduced, whose study is completely open.

About the Author

Jean-Yves Chemin is a Professor at the University of Paris VI Benoit Desjardins is based at the Centre of Atomic Studies centre de Bruyers le Chatel Isabelle Gallagher is a Professor at the Institut de Math�matiques de Jussieu
Emmanuel Greiner is based at the �cole Normale Superiore de Lyon

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