Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 44
... heat with temperature . To compute this , one considers that the specific enthalpy § , of a vapour is equal to the sensible heat of the liquid before evaporation , plus the latent heat at the temperature of evaporation , plus the change ...
... heat with temperature . To compute this , one considers that the specific enthalpy § , of a vapour is equal to the sensible heat of the liquid before evaporation , plus the latent heat at the temperature of evaporation , plus the change ...
Page 149
... sensible heat and water vapour H = pcpTw ' pq'w ' ( calories per unit area per unit time ) , Q = ( 5.39 ) ( mass of ... heat of evaporation caused by the upward moisture flux is LQ where L is the latent heat per unit mass ( 2.7 ) ...
... sensible heat and water vapour H = pcpTw ' pq'w ' ( calories per unit area per unit time ) , Q = ( 5.39 ) ( mass of ... heat of evaporation caused by the upward moisture flux is LQ where L is the latent heat per unit mass ( 2.7 ) ...
Page 193
... heat below that level and an increase in layer depth due to entrain- ment . The process is analogous to the rise of ... sensible heat content of the layer . The enthalpy can be changed also by the entrainment of colder water from ...
... heat below that level and an increase in layer depth due to entrain- ment . The process is analogous to the rise of ... sensible heat content of the layer . The enthalpy can be changed also by the entrainment of colder water from ...
Contents
INTRODUCTION | 1 |
THE STATE OF MATTER NEAR THE INTERFACE | 41 |
RADIATION | 71 |
Copyright | |
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advection air-sea amplitude angle approximately atmosphere average baroclinic barotropic bubbles cause changes circulation cloud components constant convection convergence Coriolis force decrease denotes diffusion direction dissipation drag coefficient eddy effect Ekman layer equation equilibrium expression flow fluctuations fluid flux Fourier frequency friction function geostrophic gravity waves group velocity height horizontal hurricane increase inertial integral interaction interface kinetic energy larger latitude linear mean mixed layer moisture molecular momentum motion observations ocean parameter perturbations phase velocity planetary boundary layer potential temperature processes propagation radiance ratio region relatively represents resulting Reynolds number Reynolds stress Rossby waves salinity scale sea surface sea water sensible heat shear specific humidity specified spectral spectrum storm term thermocline transport tropical turbulent unstable upwelling vapour pressure variable variations vector vertical viscosity vorticity wave number wavelength wind stress wind velocity yields zero дх