Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 46
... equilibrium with water vapour at the same temperature , molecules in either phase have the same tendency to pass across the interface into the other phase . This means that the chemical potentials of the two phases must be equal . It ...
... equilibrium with water vapour at the same temperature , molecules in either phase have the same tendency to pass across the interface into the other phase . This means that the chemical potentials of the two phases must be equal . It ...
Page 47
... equilibrium with the ambient partial pressure p . The quantity ph — a hypothetical ambient partial pressure which would be in equilibrium with the existing concen- tration q - is often interpreted simply as a gas pressure in the liquid ...
... equilibrium with the ambient partial pressure p . The quantity ph — a hypothetical ambient partial pressure which would be in equilibrium with the existing concen- tration q - is often interpreted simply as a gas pressure in the liquid ...
Page 61
... equilibrium with the drop , the chemical potential of the surrounding vapour must be larger than that in equilibrium with a plane water surface , and the difference must be equal to the internal pressure in the drop . If E ( r ) denotes ...
... equilibrium with the drop , the chemical potential of the surrounding vapour must be larger than that in equilibrium with a plane water surface , and the difference must be equal to the internal pressure in the drop . If E ( r ) denotes ...
Contents
INTRODUCTION | 1 |
THE STATE OF MATTER NEAR THE INTERFACE | 41 |
RADIATION | 71 |
Copyright | |
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Common terms and phrases
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