Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 4
... components when any one of these three directional subscripts appears twice in any term . The same is implied also when a term is squared ( v1 = v1vi Vivi v1 + v2 + v3 ) . Two or more subscripts after any symbol denote a tensor . In ...
... components when any one of these three directional subscripts appears twice in any term . The same is implied also when a term is squared ( v1 = v1vi Vivi v1 + v2 + v3 ) . Two or more subscripts after any symbol denote a tensor . In ...
Page 111
... components . In particular , the pressure can contribute to wave development only if p ( ) has a part which varies ... component . The induction coefficients m and n may depend on the wave number but not on the amplitude . An ...
... components . In particular , the pressure can contribute to wave development only if p ( ) has a part which varies ... component . The induction coefficients m and n may depend on the wave number but not on the amplitude . An ...
Page 112
... components with a short wavelength . Energy dissipation Energy dissipation near the sea surface occurs mainly in white - caps and breaking seas . In linear surface gravity waves viscosity acts very slowly . It is discussed here mainly ...
... components with a short wavelength . Energy dissipation Energy dissipation near the sea surface occurs mainly in white - caps and breaking seas . In linear surface gravity waves viscosity acts very slowly . It is discussed here mainly ...
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