An Introduction to Atmospheric Gravity Waves, Volume 102Gravity waves exist in all types of geophysical fluids, such as lakes, oceans, and atmospheres. They play an important role in redistributing energy at disturbances, such as mountains or seamounts and they are routinely studied in meteorology and oceanography, particularly simulation models, atmospheric weather models, turbulence, air pollution, and climate research. An Introduction to Atmospheric Gravity Waves provides readers with a working background of the fundamental physics and mathematics of gravity waves, and introduces a wide variety of applications and numerous recent advances. Nappo provides a concise volume on gravity waves with a lucid discussion of current observational techniques and instrumentation. Foreword is written by Prof. George Chimonas, a renowned expert on the interactions of gravity waves with turbulence. CD containing real data, computer codes for data analysis and linear gravity wave models included with the text |
Contents
FOREWORD | xv |
PREFACE | xvii |
I | 1 |
SOME WAVE MECHANICS | 6 |
FRAMES OF REFERENCE | 9 |
WAVE PHASE AND WAVE SPEED | 10 |
GROUP VELOCITY | 14 |
WAVE DISPERSION | 17 |
THE STABIL1TY OF SHEAR FLOWS | 136 |
WAVEMODULATED RICHARDSON NUMBER | 141 |
WAVETURBULENCE COUPLING | 144 |
JEFFERYS ROLLWAVE INSTABILITY MECHANISM | 149 |
WAVE SATURATION AND WAVE BREAKING | 156 |
SATURATION PARAMETERIZATION SCHEMES | 162 |
ANALOG PARAMETERIZATION SCHEMES | 169 |
SATURATION LIMITS AND OTHER PROBLEMS | 177 |
THE BOUSSINESQ APPROXIMATION | 22 |
THE TAYLORGOLDSTEIN EQUATION | 26 |
A SIMPLE SOLUTION | 31 |
CONSTANT BACKGROUND WIND SPEED | 37 |
THE WKB METHOD | 39 |
ENERGETICS | 40 |
II | 47 |
UNIFORM FLOW OVER A SURFACE CORRUGATION | 51 |
PHASE SPEED AND GROUP VELOCITY OVER A SURFACE CORRUGATION | 56 |
ENERGY FLUX OVER A SURFACE CORRUGATION | 58 |
THE TWODIMENSIONAL RIDGE | 59 |
THE THREEDIMENSIONAL MOUNTAIN | 66 |
GRAV1TY WAVE DRAG | 71 |
MATHEMATICAL DERIVATION | 72 |
THE VARIATION OF WAVE STRESS WITH HEIGHT | 74 |
WAVE STRESS OVER A SURFACE CORRUGATION | 76 |
WAVE STRESS OVER AN ISOLATED RIDGE | 77 |
SECONDARY EFFECTS OF TERRAININDUCED WAVE DRAG | 80 |
WAVE REFLECTION AT AN ELEVATED LAYER | 86 |
WAVE TRAPPING ENERGY FLUX AND WAVE RESONANCE | 91 |
REFLECTION AT THE GROUND SURFACE | 94 |
WAVE DUCTS | 98 |
THE WIND DUCT | 101 |
WIND SPIRALS AND DUCTS | 107 |
III | 111 |
WAVE ACTION | 112 |
IV | 125 |
SHEAR INSTABILITY AND UNSTABLE MODES | 129 |
KELVINHELMHOLTZ INSTABILITY | 130 |
SINGLESTATION OBSERVATIONS | 182 |
FREEBALLOON SOUNDINGS | 183 |
3 REMOTE SENSORS | 185 |
MULTIPLE STATION OBSERVATIONS | 192 |
PRESSURE PERTURBATION MEASUREMENTS | 194 |
BALLOONS AIRCRAFT AIRGLOW AND SATELLITES | 203 |
AIRCRAFT | 204 |
AIRGLOW | 205 |
SATELLITES | 206 |
DATA ANALYS1S | 210 |
PRESSUREWIND CORRELATION | 211 |
LAG ANALYSIS | 214 |
BEAMSTEERING | 217 |
WAVELET ANALYSIS | 221 |
NUMERICAL MODELS | 227 |
TERRAINGENERATED GRAVITY WAVE | 229 |
DUCTED GRAVITY WAVES | 233 |
V | 237 |
THE SCALE HEIGHT OF THE ISOTHERMAL ATMOSPHERE | 238 |
BOUSSINESQ RELATIONS | 239 |
A6 THE GEOSTROPHIC WIND | 240 |
VI | 245 |
B2 FORTRAN CODES | 246 |
RIDGE_CFOR AND RIDGEJXFOR | 247 |
WIND JUCT_SCANFOR AND WIND_DUCT_MODESFOR | 248 |
SYNTHETIC WAVE DATA | 249 |
251 | |
263 | |