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Quasi-geostrophic theory of oceans and atmosphere

Large-scale winds and currents tend to balance Coriolis and pressure gradient forces. The time evolution of these winds and currents is the subject of the quasi-geostrophic theory. Chapter 1 presents concepts and equations of classical inertial fluid mechanics. Chapter 2 deals with the equations of...

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Detalles Bibliográficos
Autor principal: Cavallini, Fabio
Otros Autores: Crisciani, Fulvio
Formato: Printed Book
Publicado: Dordrecht ; New York : Springer, c2013.
Colección:Atmospheric and oceanographic sciences library,
Materias:

Kerala University of Fisheries

Detalle de Existencias desde Kerala University of Fisheries
Número de Clasificación: 551.46 CAV/QU
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