Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 28
... integral - f ( x , t ) = ( 2π ) −2fa ( k ,, w ) e1 ( k‚æ ‚ — wt ) dl dm dn dw . ( 1.68 ) The symbol k , denotes a radius vector in a wave number space . Its components , designated here by the letters l , m , n , are a measure of the ...
... integral - f ( x , t ) = ( 2π ) −2fa ( k ,, w ) e1 ( k‚æ ‚ — wt ) dl dm dn dw . ( 1.68 ) The symbol k , denotes a radius vector in a wave number space . Its components , designated here by the letters l , m , n , are a measure of the ...
Page 72
... integral of this quantity over all directions of the hemisphere domed over the surface element is called the irradiance of that surface . The term emittance may be used in place of irradiance when we consider the radiation that leaves a ...
... integral of this quantity over all directions of the hemisphere domed over the surface element is called the irradiance of that surface . The term emittance may be used in place of irradiance when we consider the radiation that leaves a ...
Page 163
... Integral methods For particular , limited purposes , it is possible to derive the mean vertical flux of horizontal momentum into an extensive sea surface area , from the airborne horizontal flux of horizontal momentum flux through the ...
... Integral methods For particular , limited purposes , it is possible to derive the mean vertical flux of horizontal momentum into an extensive sea surface area , from the airborne horizontal flux of horizontal momentum flux through the ...
Contents
INTRODUCTION | 1 |
THE STATE OF MATTER NEAR THE INTERFACE | 42 |
SURFACE WAVES | 98 |
Copyright | |
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Common terms and phrases
advection air-sea amplitude angle approximately atmosphere baroclinic barotropic Brunt-Väisälä frequency bubbles cause changes circulation cloud components constant convection convergence Coriolis force Coriolis parameter cyclonic decrease density anomaly direction dissipation drag coefficient eddy effect Ekman layer equation expression flow fluctuations fluid flux frequency friction function geostrophic gravity waves group velocity height horizontal hurricane increase inertial infrared instability integral interactions interface inversion ITCZ latitude layer depth mean meridional mixed layer moisture molecular momentum motion observations ocean oscillations parameter perturbations phase phase velocity planetary boundary layer potential temperature pressure gradient processes propagation radiance radiation ratio region relatively represents resulting Reynolds number Reynolds stress Rossby waves scale sea surface sea-surface temperature shear specified spectrum storm surface temperature term thermocline transport tropical turbulent upwelling variable variations vector vertical viscosity vorticity wave number wavelength wind stress wind velocity zero zonal дх