Quasi-geostrophic theory of oceans and atmosphere (Record no. 1627)

MARC details
000 -LEADER
fixed length control field 04588cam a22003137a 4500
020 ## - INTERNATIONAL STANDARD BOOK NUMBER
ISBN 9789400746909 (cased)
020 ## - INTERNATIONAL STANDARD BOOK NUMBER
ISBN 9400746903 (cased)
082 04 - DEWEY DECIMAL CLASSIFICATION NUMBER
Classification number 551.46
Item number CAV/QU
100 1# - MAIN ENTRY--AUTHOR NAME
Personal name Cavallini, Fabio.
245 10 - TITLE STATEMENT
Title Quasi-geostrophic theory of oceans and atmosphere
260 ## - PUBLICATION, DISTRIBUTION, ETC. (IMPRINT)
Place of publication Dordrecht ;
-- New York :
Name of publisher Springer,
Year of publication c2013.
300 ## - PHYSICAL DESCRIPTION
Number of Pages xiii, 385 p. :
Other physical details ill. ;
490 0# - SERIES STATEMENT
Series statement Atmospheric and oceanographic sciences library,
505 0# - FORMATTED CONTENTS NOTE
Formatted contents note Machine generated contents note: pt. I Fundamentals -- 1. Basic Continuum Mechanics -- 1.1. Kinematics of Continua -- 1.1.1. The Continuum Hypothesis and the Concept of Material Element -- 1.1.2. Kinematics of Material Elements -- 1.2. Dynamics of Fluids -- 1.2.1. Momentum Equation -- 1.2.2. Basic Concepts of Vorticity Dynamics -- 1.2.3.A Look at Turbulence -- 1.2.4. Appendix: Galilean Covariance of the Lagrangian Derivative -- 2. Basic Geophysical Fluid Dynamics -- 2.1. Constitutive Equations -- 2.1.1. Equations of State -- 2.1.2. Thermodynamic Equations of Dry Air and Seawater -- 2.1.3.Compressibility and Incompressibility -- 2.2. Internal Gravity Waves in Adiabatic and Frictionless Fluids -- 2.2.1. Definition of the Model -- 2.2.2. Evolution Equations for the Velocity, Pressure and Density Fields -- 2.3. Rotating Flows -- 2.3.1. Basic Parameters of the Earth and Local Cartesian Coordinate Systems -- 2.3.2. Uniformly Rotating Coordinate Frames.
505 0# - FORMATTED CONTENTS NOTE
Formatted contents note Contents note continued: 2.3.3. The Equations of Fluid Mechanics for Uniformly Rotating Systems -- 2.3.4. Covariance of the Gradient Operator in Passing from an Inertial to a Rotating Frame of Reference -- 2.3.5. Governing Equations of Long Gravity Waves -- 2.3.6. Poincare and Kelvin Waves -- 2.3.7. Vorticity and Potential Vorticity of a Uniformly Rotating Flow -- 2.3.8. Appendix: Hydraulics and Earth's Rotation -- 2.4. Large-Scale Flows -- 2.4.1. Phenomenology of Large-Scale Circulation of Geophysical Flows -- 2.4.2. Governing Equations of Large-Scale, Geophysical Flows -- pt. II Applications -- 3. Quasi-Geostrophic Single-Layer Models -- 3.1. Shallow-Water Model -- 3.1.1. The Quasi-Geostrophic, Shallow-Water Model -- 3.1.2. Developments of the Shallow-Water Equations for Modelling Wind-Driven Ocean Circulation -- 3.2. Homogeneous Model -- 3.2.1. The Ekman Layers -- 3.2.2. The Homogeneous Model of the Wind-Driven Oceanic Circulation -- 3.2.3. Classical Solutions of the Homogeneous Model.
505 0# - FORMATTED CONTENTS NOTE
Formatted contents note Contents note continued: 3.2.4. Basic Dynamics of the Atmospheric Ekman Layer -- 4. Quasi-Geostrophic Two-Layer Model -- 4.1. Basic QG Equations for the Two-Layer Model -- 4.1.1. The Quasi-Geostrophic Two-Layer Model -- 4.1.2. Frictional Interaction Between the Layers -- 4.1.3. The Vorticity Equations of the Two-Layer Model -- 4.1.4. Wave-Like Solution of the Model -- 4.1.5. Behaviour of the Interface -- 4.2. Energetics of the Two-Layer Model -- 4.2.1. Energetics Associated to the Quasi-Geostrophic Two-Layer Model -- 4.2.2. Available Potential Energy of a Two-Layer Fluid -- 4.2.3. Integrated Energetics of the Two-Layer Model (4.65)---(4.66) -- 5. Quasi-Geostrophic Models of Continuously Stratified Flows -- 5.1. QG Continuously Stratified Flows in the Ocean -- 5.1.1. The Quasi-Geostrophic Oceanic Mesoscale -- 5.1.2. Quasi-Geostrophic Dynamics at the Oceanic Basin Scale -- 5.1.3. The Effects of Bathymetry -- 5.1.4. Forced and Wave-Like Circulation.
505 0# - FORMATTED CONTENTS NOTE
Formatted contents note Contents note continued: 5.2. QG Continuously Stratified Flows in the Atmosphere -- 5.2.1. Basic Synoptic-Scale Dynamics of the Atmosphere -- 5.2.2. Thermally Forced Stationary Waves -- 5.2.3. The Effects of Topography.
520 ## - SUMMARY, ETC.
Summary, etc 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 thermodynamics that close the governing equations of the fluids. Then, the motion is reformulated in a uniformly rotating reference frame. Chapter 3 deals with the shallow-water model and the homogeneous model of wind-driven circulation. The chapter also describes a classical application of the Ekma --Page 4 of cover.
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical Term Geophysics
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical Term Fluid mechanics.
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical Term Oceanography.
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical Term Atmospheric thermodynamics.
650 #7 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical Term Atmospheric thermodynamics.
650 #7 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical Term Fluid mechanics.
650 #7 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical Term Geophysics
650 #7 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical Term Oceanography.
700 1# - ADDED ENTRY--PERSONAL NAME
Personal name Crisciani, Fulvio.
942 ## - ADDED ENTRY ELEMENTS (KOHA)
Koha item type Books
Holdings
Withdrawn status Lost status Collection code Home library Current library Shelving location Date acquired Full call number Accession Number Koha item type
    Non-fiction KUFOS Central Library KUFOS Central Library General Stacks 29/04/2016 551.46 CAV/QU 17777 Books
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