Dynamics of the Atmosphere: A Course in Theoretical MeteorologyDynamics of the Atmosphere consists of two parts: the first presenting the mathematical tools needed for a thorough understanding of the topics covered in the second part of the book. The second part begins with the derivation of the equation describing the atmospheric motion on the rotating earth. Subjects tackled in subsequent chapters include kinematics of the atmosphere (including vorticity and circulation theorems), wave motion in the atmosphere, inertial and dynamic stability, and turbulent systems in the atmosphere. Finally, newer methods of weather prediction, such as the spectral technique and the stochastic dynamic method, are introduced in order to demonstrate their potential for extending the forecasting range. Complete with numerous exercise sets and solutions, this textbook has been written for advanced undergraduate and graduate students of meteorology and other related sciences. It may also be used as a reference source by professional meteorologists and researchers in atmospheric science. |
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Dynamics of the Atmosphere: A Course in Theoretical Meteorology Wilford Zdunkowski,Andreas Bott No preview available - 2003 |
Dynamics of the Atmosphere: A Course in Theoretical Meteorology Wilford Zdunkowski,Andreas Bott No preview available - 2003 |
Common terms and phrases
approximation assume atmosphere baroclinic barotropic basis vectors Cartesian coordinate system Cartesian coordinates components consider constant continuity equation contravariant coordinate system Coriolis Coriolis parameter cos² covariant defined derivative differential equation divergence dyadic equation of motion exchange coefficient expression Əqi field fixed point flow fluid flux function geopotential geostrophic wind given gradient heat equation horizontal hydrostatic equation integral kinetic energy linear measure numbers obtain orthogonal phase velocity Prandtl layer pressure prognostic equation quantities right-hand side Rossby Rossby waves rotation scalar product shown in Figure solution stability surface tensor term theorem trajectory transformation turbulent unstable V₁ vanishes variables velocity vertical vorticity equation wavenumber waves zero θα дак ди др дх ду Эф მ მ მა მდ მი