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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...

Description complète

Détails bibliographiques
Auteur principal: Cavallini, Fabio
Autres auteurs: Crisciani, Fulvio
Format: Printed Book
Publié: Dordrecht ; New York : Springer, c2013.
Collection:Atmospheric and oceanographic sciences library,
Sujets:

Kerala University of Fisheries

Informations d'exemplaires de Kerala University of Fisheries
Cote: 551.46 CAV/QU
Exemplaire NFIC Statut en temps réel indisponible