Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 85
... infrared radiation , but the presence of these aerosols in the marine atmosphere is intermittent , and their influence on the trans- mission of infrared radiation will not be considered here . In the water , infrared radiation does not ...
... infrared radiation , but the presence of these aerosols in the marine atmosphere is intermittent , and their influence on the trans- mission of infrared radiation will not be considered here . In the water , infrared radiation does not ...
Page 90
... infrared heat loss from the sea surface . A low cloud layer with a thickness of , at most 200 m , can absorb all infrared radiation . The radiation emitted downward from the cloud base in this case is equal to black - body radiation ...
... infrared heat loss from the sea surface . A low cloud layer with a thickness of , at most 200 m , can absorb all infrared radiation . The radiation emitted downward from the cloud base in this case is equal to black - body radiation ...
Page 95
... infrared radiation balance at the surface depends not only on the amount of clouds but also on their height h . Phillips , as quoted by Charney in the Handbook of meteorology , suggests that this can be allowed for in overcast ...
... infrared radiation balance at the surface depends not only on the amount of clouds but also on their height h . Phillips , as quoted by Charney in the Handbook of meteorology , suggests that this can be allowed for in overcast ...
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