Atmosphere, Ocean and Climate Dynamics Fall 2008

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MIT OpenCourseWare http://ocw.mit.edu 12.003 Atmosphere, Ocean and Climate Dynamics Fall 2008 For information about citing these materials or our Terms of Use, visit: http://ocw.mit.edu/terms.

Contents 0.1 Preface... 10 0.1.1 Natural fluid dynamics.... 10 0.1.2 Rotating fluid dynamics.... 13 0.1.3 Holicism... 16 I The Atmosphere 19 1 Characteristics of the atmosphere 21 1.1 Geometry... 21 1.2 Chemical composition of the atmosphere.... 22 1.3 Physical properties of air... 23 1.3.1 Moist air... 25 2 The global energy balance 29 2.1 Effective planetary temperature (emission temperature)... 29 2.2 The atmospheric absorption spectrum.... 33 2.3 The greenhouse effect.... 34 2.3.1 A simple greenhouse model... 36 2.3.2 A leaky greenhouse... 38 2.3.3 A more opaque greenhouse... 39 3 The vertical structure of the atmosphere 43 3.1 Vertical distribution of temperature and Greenhouse gases.. 43 3.1.1 Typical temperature profile... 43 3.1.2 Atmospheric layers... 45 3.2 The relationship between pressure and density: hydrostatic balance... 48 3.3 Vertical structure of pressure and density.... 50 3

4 CONTENTS 3.3.1 Isothermal atmosphere... 50 3.3.2 Non-isothermal atmosphere... 51 3.3.3 Density... 52 4 Convection 53 4.1 The nature of convection.... 53 4.1.1 Convection in a shallow fluid... 53 4.1.2 Instability... 54 4.2 Convection in water (an almost-incompressible fluid)... 56 4.2.1 Buoyancy... 56 4.2.2 Stability... 57 4.2.3 Energetics... 58 4.2.4 GFD Lab II: convection... 59 4.3 Dry convection in a compressible atmosphere... 63 4.3.1 The adiabatic lapse rate... 63 4.3.2 Potential temperature... 65 4.4 The atmosphere under stable conditions.... 68 4.4.1 Gravity waves... 68 4.4.2 Temperature inversions... 71 4.5 Moist convection... 72 4.5.1 Humidity... 73 4.5.2 Saturated adiabatic lapse rate... 74 4.5.3 Radiative-convective equilibrium..... 75 4.6 Convection in the atmosphere... 76 4.6.1 Convective clouds... 76 4.6.2 Occurrence and depth of convection.... 77 4.6.3 Where does convection occur?... 78 5 The Meridional Structure of the Atmosphere 81 5.1 Temperature... 81 5.1.1 Latitudinal dependence of incoming radiation... 81 5.1.2 Latitudinal dependence of outgoing radiation... 82 5.1.3 Meridional structure of temperature.... 84 5.1.4 The energy balance of the atmosphere... 87 5.2 Pressure and geopotential height..... 88 5.2.1 The height of pressure surfaces... 88 5.2.2 Geopotential surfaces... 89 5.3 Moisture... 90

CONTENTS 5 5.4 Winds... 95 5.4.1 Distribution of winds... 95 6 The equations of fluid motion 103 6.1 Differentiation following the motion... 103 6.2 Equation of motion for a nonrotating fluid... 106 6.2.1 Forces on a fluid parcel....106 6.2.2 The equation of motion...110 6.2.3 Hydrostatic balance...111 6.3 The continuity equation...111 6.3.1 Incompressible flow...112 6.3.2 Compressible flow...112 6.4 Equation of motion for a rotating fluid.... 114 6.4.1 GFD Lab III: radial inflow... 114 6.4.2 Transformation into rotating coordinates... 119 6.4.3 The rotating equation of motion...121 6.4.4 Experiments with Coriolis forces on a parabolic rotat- ing table...123 6.4.5 Geostrophic motion...129 6.4.6 The Taylor-Proudman Theorem... 132 6.4.7 The thermal wind equation...135 6.4.8 Subgeostrophic flow: the Ekman layer... 143 6.5 Putting things on the sphere...148 6.5.1 GFD Lab X: An experiment on the Earth s rotation.. 148 6.5.2 The centrifugal force, modified hydrostatic balance and geopotential surfaces on the sphere... 150 6.5.3 Components of the Coriolis force on the sphere: the Coriolis parameter...152 6.6 Geostrophic balance on the sphere...154 6.6.1 Small Rossby number flow...154 6.7 Thermal wind in pressure coordinates...... 163 6.7.1 Thermal wind expressed in terms of potential temper- ature....164 7 The general circulation of the atmosphere 169 7.1 The tropical Hadley circulation.... 169 7.2 The midlatitude circulation...173 7.2.1 Energy stored in the thermal wind... 174

6 CONTENTS 7.2.2 Available potential energy...175 7.2.3 Baroclinic instability...178 7.2.4 GFD Lab XI: baroclinic instability of the thermal wind 180 7.3 The big picture of the atmospheric heat (and momentum) budget.... 182 7.3.1 Energy requirements, as deduced from observations.. 182 7.3.2 Incorporating eddy transfer in to our general circula- tion theory...185 II The Ocean 189 8 The ocean and its circulation 191 8.1 Physical characteristics of the ocean...192 8.1.1 Properties of seawater; equation of state... 193 8.1.2 Temperature and salinity structure... 196 8.1.3 The mixed layer and thermocline.... 201 8.2 The observed circulation.... 204 8.3 Inferences from geostrophic and hydrostatic balance.... 207 8.3.1 Ocean surface structure and geostrophic flow... 208 8.3.2 Deep geostrophic flow...211 9 The wind-driven circulation 213 9.1 The wind stress and Ekman layers... 213 9.1.1 Balance of forces in the Ekman layer... 215 9.1.2 Wind-driven Ekman pumping... 216 9.2 Response of the interior ocean to Ekman pumping... 220 9.2.1 Interior balances.... 220 9.2.2 Taylor-Proudman on the sphere... 221 9.2.3 GFD Lab XIII: Wind-driven ocean gyres... 225 9.2.4 The wind-driven gyres and western boundary currents 226 9.3 The depth-integrated circulation.... 228 9.3.1 Mass transport of gyres: western boundary current speeds...231 9.4 Effects of inhomogeneity.... 231 9.4.1 Taylor-Proudman in a layered ocean... 233 9.5 Ocean eddies.... 236 9.5.1 Observations of ocean eddies...236

CONTENTS 7 9.5.2 Baroclinic instability in the ocean.... 238 10 The thermohaline circulation of the ocean 243 10.1 Sources of deep water...243 10.2 Time scales and intensity of thermohaline circulation... 249 10.3 Abyssal circulation schematic deduced from Taylor-Proudman 250 10.4 Observations of the abyssal circulation... 252 10.5 GFD Lab XIV: The thermohaline circulation.... 257 10.6 Why western boundary currents?... 258 10.6.1 GFD Lab XV: Source sink flow in a rotating basin... 260 11 The ocean s role in climate 263 11.1 Ocean Heat storage...263 11.2 Ocean heat transport...264 11.2.1 Mechanisms of ocean heat transport... 266