Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 23
... eddy transports parametrically as functions of the averaged or bulk variables which are measured routinely . This has been done in the past by the introduction of empirically estimated coefficients of eddy transport defined by av v'w ...
... eddy transports parametrically as functions of the averaged or bulk variables which are measured routinely . This has been done in the past by the introduction of empirically estimated coefficients of eddy transport defined by av v'w ...
Page 146
... eddy viscosity cannot depend directly on the density stratification ; above the highest critical level , they cannot be affected directly by wave growth . This permits us to treat the effect of the two mechanisms on the energy balance ...
... eddy viscosity cannot depend directly on the density stratification ; above the highest critical level , they cannot be affected directly by wave growth . This permits us to treat the effect of the two mechanisms on the energy balance ...
Page 183
... eddy viscosity de- creases rapidly with height - in qualitative agreement with the laminar model . Bobyleva , Zilitinkevich , and Leichmann ( 1965 ) assumed that the = C1 , Kн / bz = C2 , Kobz = C3 ratios K / bz were all different ...
... eddy viscosity de- creases rapidly with height - in qualitative agreement with the laminar model . Bobyleva , Zilitinkevich , and Leichmann ( 1965 ) assumed that the = C1 , Kн / bz = C2 , Kobz = C3 ratios K / bz were all different ...
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