Adiabatic invariants in large-scale atmospheric dynamics

Adiabatic invariants in large-scale atmospheric dynamics

by Kurganskiæi, M. V., (Mikhail Vasil'evich)

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Preface. Introduction. Equations of Motion and Conservation Laws. Reduced Equations of Atmospheric Dynamics. Hydrodynamic Instability of Conservative Motions. Isentropic Analysis of Large-scale Processes. Dissipative Processes in the Atmosphere. Reference. Index.

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Title Statements

  • Full title :Adiabatic invariants in large-scale atmospheric dynamics / Michael V. Kurgansky and A.M. Obukhov.

Summary

Preface. Introduction. Equations of Motion and Conservation Laws. Reduced Equations of Atmospheric Dynamics. Hydrodynamic Instability of Conservative Motions. Isentropic Analysis of Large-scale Processes. Dissipative Processes in the Atmosphere. Reference. Index.

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Edition Statements

  • Publication Date:2002.

Publication Statements

  • Publisher(s):Taylor & Francis
  • Place of Publication:London
  • Language:eng
  • Publication Date:2002.

The Physical Object

  • Description:1 online resource (xi, 222 pages) : : illustrations, maps

Edition Identifiers

  • ISBN:0203216482, 9780203216484
  • oclc:ocn276791813
  • LC Classification:QC880.4.A3 K8713 2002eb
  • Dewey Decimal:551.515

Table of Contents

BOOK COVER; TITLE; COPYRIGHT; CONTENTS; FOREWORD TO THE ENGLISH EDITION; PREFACE; INTRODUCTION; CHAPTER 1 Equations of Motion and Conservation Laws; 1.1 Equations of compressible fluid dynamics; 1.2 Adiabatic approximation. Potential vorticity theorem; 1.3 Vorticity charge (potential vorticity substance); 1.4 Helicity; 1.5 Energy and entropy of the atmosphere; 1.6 Atmospheric angular momentum; CHAPTER 2 Reduced Equations of Atmospheric Dynamics; 2.1 Two-dimensional atmospheric models ('shallow-water' approximation); 2.2 Adjustment of fluid dynamic fields.

2.3 Filtered (quasi-geostrophic) equations2.4 Rossby waves; 2.5 Continuous (spontaneous) wave emission; CHAPTER 3 Hydrodynamic Instability of Conservative Motions; 3.1 Barotropic instability; 3.2 Baroclinic instability; 3.3 Linear analysis (Eady model); 3.4 Two-layer Phillips' model; 3.5 Vertical stability of atmospheric motions. Richardson's criterion; CHAPTER 4 Isentropic Analysis of Large-scale Processes; 4.1 Isentropic coordinates; 4.2 Theorem on potential vorticity; 4.3 Precise formulation of the available potential energy concept; 4.4 Diabatic transformation of potential vorticity.

4.5 General properties of air adiabatic …

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