Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 74
... direction ( 4 , « ) per unit travel distance dr into another particular direction ( p ' , x ' ) can be specified by a scattering function { S ( r ) , ... } . The polarization of radiation is generally affected by scattering and a ...
... direction ( 4 , « ) per unit travel distance dr into another particular direction ( p ' , x ' ) can be specified by a scattering function { S ( r ) , ... } . The polarization of radiation is generally affected by scattering and a ...
Page 75
... directions ( p , a ) and ( p ' , a ' ) . The expression ( 3.13 ) shows Rayleigh scattering to be twice as large along or against the direction of the ray than in the normal direction . Emission and absorption All radiation is emitted ...
... directions ( p , a ) and ( p ' , a ' ) . The expression ( 3.13 ) shows Rayleigh scattering to be twice as large along or against the direction of the ray than in the normal direction . Emission and absorption All radiation is emitted ...
Page 118
Eric Bradshaw Kraus. to grow while the longer waves in the direction of Up continue to develop slowly . As a result , the angle between the propagation of the waves that are highest locally and the local wind direction becomes smaller ...
Eric Bradshaw Kraus. to grow while the longer waves in the direction of Up continue to develop slowly . As a result , the angle between the propagation of the waves that are highest locally and the local wind direction becomes smaller ...
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