The Ceaseless Wind: An Introduction to the Theory of Atmospheric MotionCourier Corporation, 01.06.2002 - 617 Seiten Internationally acclaimed text provides integrative presentation of concepts of atmospheric dynamics: atmospheric structure, equations of motion in inertial coordinates, meteorological equations of motion, moisture processes, models of the wind, atmospheric energetics, vorticity, atmospheric wave motion, and the quasi-geostropic theory of large-scale flow. More than 400 problems. 97 illustrations. |
Inhalt
Part One Foundations of Atmospheric Dynamics | 1 |
Some Basic Physical and Mathematical Concepts | 16 |
3 | 45 |
The Vertical Structure of the Atmosphere | 60 |
4 | 69 |
Vector and Tensor Analysis and the Fundamental | 96 |
4 | 124 |
6 | 136 |
Part Three The Theory of Atmospheric Motion | 287 |
Vorticity | 332 |
Global Thermodynamics | 399 |
Atmospheric Wave Motion | 452 |
Approximate Equations of Motion for SmallScale | 488 |
The Quasigeostrophic Theory of LargeScale Flow | 512 |
Atmospheric Modeling and Metamodeling | 554 |
The First Law of Thermodynamics | 585 |
Part Two The Equations of Atmospheric Motion | 167 |
3 | 175 |
5 | 183 |
9 | 206 |
Water in the Air | 256 |
Useful Formulas Identities and Constants | 592 |
| 599 | |
| 615 | |
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Häufige Begriffe und Wortgruppen
acceleration advection approximation assume assumption atmospheric motion baroclinic basic boundary conditions cartesian Chap circulation component consider constant continuity equation coordinate system Coriolis force curve cyclone define denote density derivative determine differential divergence divergence theorem dynamics earth entropy equations of motion fluid flux friction function geostrophic wind gravity waves heating horizontal hydrostatic hydrostatic equation incompressible inertial integral isentropic coordinates isobaric isobaric coordinates kinetic energy large-scale latitude mass mathematical mbar meteorological nonlinear obtain orthogonal parcel potential temperature prediction PROBLEM quantities quasi-geostrophic rate of change result rotation scalar scale shear Show solutions streamlines surface tensor term theorem thermal thermodynamic trajectory turbulence unit vectors values vanishes vapor variables variations vertical velocity volume vortex vortex tube vorticity equation δυ θο ди др ду дх дхі

