Atmospheric DynamicsCambridge University Press, 2004年12月16日 - 224 頁 In his book, John Green presents a unique personal insight into the fundamentals of fluid mechanics and atmospheric dynamics. Generations of students have benefited from his lectures, and this book, many years in the making, is the result of his wide teaching and research experience. The theory of fluid flow has developed to such an extent that very complex mathematics and models are currently used to describe it, but many of the fundamental results follow from relatively simple considerations: these classic principles are derived here in a novel, distinctive, and at times even idiosyncratic, way. The book is an introduction to fluid mechanics in the atmosphere for students and researchers that are already familiar with the subject, but who wish to extend their knowledge and philosophy beyond the currently popular development of conventional undergraduate instruction. |
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第 1 到 5 筆結果,共 87 筆
第 iv 頁
... . Fluid mechanics . I. Title . II . Series . QC860.G66 1999 551.5 15 - dc21 97-43007 CIP ISBN 0 521 24975 9 hardback ISBN 0 521 61696 4 paperback Contents Introduction 1 Chapter | Description of atmospheric motion systems.
... . Fluid mechanics . I. Title . II . Series . QC860.G66 1999 551.5 15 - dc21 97-43007 CIP ISBN 0 521 24975 9 hardback ISBN 0 521 61696 4 paperback Contents Introduction 1 Chapter | Description of atmospheric motion systems.
第 v 頁
... motion systems 3 1.1 1.2 1.3 1.4 1.5 1.6 1.7 Introduction 3 Spectrum of motion 4 How isolated phenomena appear in wavenumber - space 7 Repeated phenomena 9 Contribution of phenomena to the global kinetic energy spectrum 10 What do we ...
... motion systems 3 1.1 1.2 1.3 1.4 1.5 1.6 1.7 Introduction 3 Spectrum of motion 4 How isolated phenomena appear in wavenumber - space 7 Repeated phenomena 9 Contribution of phenomena to the global kinetic energy spectrum 10 What do we ...
第 vi 頁
... Motion independent of longitude 29 Continuity of mass 31 Continuity of energy 32 3.6 Dry adiabatic 33 3.7 Wet adiabatic 34 3.8 3.9 3.10 3.11 3.12 3.13 3.14 3.15 Thermodynamic processes 35 Energetics 36 Completeness 37 Vorticity 38 The ...
... Motion independent of longitude 29 Continuity of mass 31 Continuity of energy 32 3.6 Dry adiabatic 33 3.7 Wet adiabatic 34 3.8 3.9 3.10 3.11 3.12 3.13 3.14 3.15 Thermodynamic processes 35 Energetics 36 Completeness 37 Vorticity 38 The ...
第 vii 頁
... motion 104 8.1 8.2 8.3 8.4 8.5 8.6 8.7 8.8 8.9 8.10 Definition of mesoscale 104 Above the logarithmic layer 105 The ... motion 111 Continually balanced motion 113 Evolution of the mean flow 114 More general forcing 115 Chapter 9 Motion ...
... motion 104 8.1 8.2 8.3 8.4 8.5 8.6 8.7 8.8 8.9 8.10 Definition of mesoscale 104 Above the logarithmic layer 105 The ... motion 111 Continually balanced motion 113 Evolution of the mean flow 114 More general forcing 115 Chapter 9 Motion ...
第 viii 頁
... Motion in a barotropic atmosphere 144 The barotropic quasi - geostrophic vorticity equation 144 Stationary waves 145 Lids lead to resonance 145 Surface friction 146 Friction at an upper lid 147 Very deep atmosphere 147 Upward ...
... Motion in a barotropic atmosphere 144 The barotropic quasi - geostrophic vorticity equation 144 Stationary waves 145 Lids lead to resonance 145 Surface friction 146 Friction at an upper lid 147 Very deep atmosphere 147 Upward ...
內容
Introduction | 1 |
Notation | 18 |
Fundamental equations | 26 |
Nearly horizontal atmosphere | 44 |
Gravity waves | 63 |
Shearing instability | 76 |
Vertical convection | 93 |
Mesoscale motion | 104 |
Motion of large scale | 117 |
The forecast problem | 134 |
Modelling | 159 |
Models | 172 |
Transport and mixing | 186 |
General circulation | 196 |
9 | 207 |
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常見字詞
acceleration adiabatic advection albedo amplifying amplitude anticyclone atmosphere baroclinic waves becomes boundary condition circulation constant convection coordinate Coriolis cumulonimbus cumulus decrease defined density dissipation eddy example exp ikx exponentially Figure finite flow fluid flux friction geostrophic gives gradient gravity waves ground group velocity heat height horizontal hydrostatic initial integral interface isentropic isentropic surfaces kinetic energy latitude layer linear mean molecular diffusion momentum equation motion non-linear notice numerical parameter parcel particle phase speed physical potential energy potential temperature potential vorticity pressure field processes propagation quasi-geostrophic relative represent Rossby waves scale shearing instability short waves shows simple sinh solution stationary steering level stratification stream function suppose surface term thermal thermal wind thermodynamic timescale tion transfer troposphere U₁ upper vanishes variables variation vertical velocity viscosity visualise vortex vorticity equation water vapour wavelength wavenumber wind zonal дх