Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 73
... angle cannot exceed a limiting value arc sin ( 1.34 ) -1≈ 49 ° . Light that reaches the interface from the water at a larger angle of incidence cannot pass into the air but is totally reflected , and rays that enter the water from ...
... angle cannot exceed a limiting value arc sin ( 1.34 ) -1≈ 49 ° . Light that reaches the interface from the water at a larger angle of incidence cannot pass into the air but is totally reflected , and rays that enter the water from ...
Page 87
... angle in the form & I = rI + εBo , · ( 3.26 ) where represents here the angle between the horizon and the line of sight , I is the radiance of the surface viewed at the angle 4 , I。 the radiance of the sky in the direction of specular ...
... angle in the form & I = rI + εBo , · ( 3.26 ) where represents here the angle between the horizon and the line of sight , I is the radiance of the surface viewed at the angle 4 , I。 the radiance of the sky in the direction of specular ...
Page 237
... angle with the northward direction . The outer edge of the wave pattern is determined by § a2x / ẞt = -1 in the west and by east ( after Longuet - Higgins 1965 ) . = in the breakdown of the geostrophically balanced surface trough ...
... angle with the northward direction . The outer edge of the wave pattern is determined by § a2x / ẞt = -1 in the west and by east ( after Longuet - Higgins 1965 ) . = in the breakdown of the geostrophically balanced surface trough ...
Contents
INTRODUCTION | 1 |
THE STATE OF MATTER NEAR THE INTERFACE | 42 |
SURFACE WAVES | 98 |
Copyright | |
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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