An Introduction to Dynamic MeteorologyAcademic Press, 17 dic 2012 - 552 pagine During the past decade, the science of dynamic meteorology has continued its rapid advance. The scope of dynamic meteorology has broadened considerably. Much of the material is based on a two-term course for seniors majoring in atmospheric sciences. This book presents a cogent explanation of the fundamentals of meteorology and explains storm dynamics for weather-oriented meteorologists. It discusses climate dynamics and the implications posed for global change. The new edition has added a companion website with MATLAB exercises and updated treatments of several key topics.
NEW IN THIS EDITION
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Sommario
1 | |
31 | |
3 Elementary Applications of the Basic Equations | 67 |
4 Circulation Vorticity and Potential Vorticity | 95 |
5 Atmospheric Oscillations | 127 |
6 Quasigeostrophic Analysis | 171 |
7 Baroclinic Development | 213 |
8 The Planetary Boundary Layer | 255 |
13 Numerical Modeling and Prediction | 453 |
Useful Constants and Parameters | 491 |
List of Symbols | 493 |
Vector Analysis | 499 |
Moisture Variables | 503 |
Standard Atmosphere Data | 507 |
Symmetric Baroclinic Oscillations | 509 |
Conditional Probability and Likelihood | 511 |
9 Mesoscale Circulations | 279 |
10 The General Circulation | 325 |
11 Tropical Dynamics | 377 |
12 Middle Atmosphere Dynamics | 413 |
513 | |
519 | |
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adiabatic advection amplitude analysis angular approximation associated assumed atmosphere average balance baroclinic boundary layer Chapter circulation compared component conserved consider constant convection coordinate Coriolis cyclonic defined density depends derivative determined difference direction discussed distribution disturbance divergence dynamics eddy energy equation equatorial example expressed field Figure flow fluid flux force function geopotential geostrophic given gives gradient gravity heat height Hemisphere horizontal increase indicated initial instability latitude layer linear lines mass maximum mean meridional modes momentum motion Note observed obtain occur oscillation parcel perturbation phase positive potential temperature potential vorticity pressure Problem processes propagation provides referred region relative represented respectively result Rossby rotation scale shear shown solution speed surface thermal tropical turbulent unit variables vector velocity vertical warm wave wind zonal