This book deals with the main principles of large-scale atmospheric
dynamics on the basis of adiabatic motion constants. It can be
considered as an introduction to the theory of quasi
two-dimensional fluid motion concentrating primarily on nearly
horizontal fluid parcel displacements in a stably stratified
compressible fluid. A thorough mathematical treatment of the
governing equations is coupled with a clear interpretation of the
phenomena studied and accompanied by examples of real
meteorological data analysis. Topics include a complete set of
compressible fluid dynamic equations along with a survey on fluid
dynamical conservation laws used in meteorology and atmospheric
physics; the derivation of two-dimensional atmospheric models;
large-scale flows; isentropic analysis of large-scale atmospheric
processes; and the principles of kinetic energy sinks and their
relation to the energy balance in the atmosphere.
General
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