THE SCIENTIFIC PAPERS: METEOROLOGY, OCEANOGRAPHY & TURBULENT FLOW

By EMMA LEE

CONTENTS PART I FUNDAMENTALS BASIC CONTINUUM MECHANICS KINEMATICS OF CONTINUA THE CONTINUUM HYPOTHESIS AND THE CONCEPT OF MATERIAL ELEMENT KINEMATICS OF MATERIAL ELEMENTS DYNAMICS OF FLUIDS MOMENTUM EQUATION BASIC CONCEPTS OF VORTICITY DYNAMICS A LOOK AT TURBULENCE APPENDIX: GALILEAN COVARIANCE OF THE LAGRANGIAN DERIVATIVE BASIC GEOPHYSICAL FLUID DYNAMICS CONSTITUTIVE EQUATIONS EQUATIONS OF STATE THERMODYNAMIC EQUATIONS OF DRY AIR AND SEAWATER COMPRESSIBILITY AND INCOMPRESSIBILITY INTERNAL GRAVITY WAVES IN ADIABATIC AND FRICTIONLESS FLUIDS DE?NITION OF THE MODEL EVOLUTION EQUATIONS FOR THE VELOCITY, PRESSURE AND DENSITY FIELDS ROTATING FLOWS BASIC PARAMETERS OF THE EARTH AND LOCAL CARTESIAN COORDINATE SYSTEMS UNIFORMLY ROTATING COORDINATE FRAMES THE EQUATIONS OF FLUID MECHANICS FOR UNIFORMLY ROTATING SYSTEMS COVARIANCE OF THE GRADIENT OPERATOR IN PASSING FROM AN INERTIAL TO A ROTATING FRAME OF REFERENCE GOVERNING EQUATIONS OF LONG GRAVITY WAVES POINCAR´E AND KELVIN WAVES VORTICITY AND POTENTIAL VORTICITY OF A UNIFORMLY ROTATING FLOW APPENDIX: HYDRAULICS AND EARTH’S ROTATION LARGE-SCALE FLOWS PHENOMENOLOGY OF LARGE-SCALE CIRCULATION OF GEOPHYSICAL FLOWS GOVERNING EQUATIONS OF LARGE-SCALE, GEOPHYSICAL FLOWS PART II APPLICATIONS QUASI-GEOSTROPHIC SINGLE-LAYER MODELS SHALLOW-WATER MODEL THE QUASI-GEOSTROPHIC, SHALLOW-WATER MODEL DEVELOPMENTS OF THE SHALLOW-WATER EQUATIONS FOR MODELLING WIND-DRIVEN OCEAN CIRCULATION HOMOGENEOUS MODEL THE EKMAN LAYERS THE HOMOGENEOUS MODEL OF THE WIND-DRIVEN OCEANIC CIRCULATION CLASSICAL SOLUTIONS OF THE HOMOGENEOUS MODEL BASIC DYNAMICS OF THE ATMOSPHERIC EKMAN LAYER QUASI-GEOSTROPHIC TWO-LAYER MODEL BASIC QG EQUATIONS FOR THE TWO-LAYER MODEL THE QUASI-GEOSTROPHIC TWO-LAYER MODEL FRICTIONAL INTERACTION BETWEEN THE LAYERS THE VORTICITY EQUATIONS OF THE TWO-LAYER MODEL WAVE-LIKE SOLUTION OF THE MODEL BEHAVIOUR OF THE INTERFACE ENERGETICS OF THE TWO-LAYER MODEL ENERGETICS ASSOCIATED TO THE QUASI-GEOSTROPHIC TWO-LAYER MODEL AVAILABLE POTENTIAL ENERGY OF A TWO-LAYER FLUID INTEGRATED ENERGETICS OF THE TWO-LAYER MODEL (4 65)–(4 66) QUASI-GEOSTROPHIC MODELS OF CONTINUOUSLY STRATI?ED FLOWS QG CONTINUOUSLY STRATI?ED FLOWS IN THE OCEAN THE QUASI-GEOSTROPHIC OCEANIC MESOSCALE QUASI-GEOSTROPHIC DYNAMICS AT THE OCEANIC BASIN SCALE THE EFFECTS OF BATHYMETRY FORCED AND WAVE-LIKE CIRCULATION QG CONTINUOUSLY STRATI?ED FLOWS IN THE ATMOSPHERE BASIC SYNOPTIC-SCALE DYNAMICS OF THE ATMOSPHERE THERMALLY FORCED STATIONARY WAVES THE EFFECTS OF TOPOGRAPHY