Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 18
... fluid element would oscillate about its equilibrium level in an ideal , inviscid fluid with a linear density decrease ( ap / dz < 0 ) . The first term in the curly brackets of eqn ( 1.46 ) results from the compressibility which is ...
... fluid element would oscillate about its equilibrium level in an ideal , inviscid fluid with a linear density decrease ( ap / dz < 0 ) . The first term in the curly brackets of eqn ( 1.46 ) results from the compressibility which is ...
Page 169
... fluid system ; if the suffix w is used to denote properties of the lower fluid , the boundary conditions for eqn ( 6.13 ) have the form ( u + iv ) B → 0 , - ( u + iv ) B— ( u + iv ) = ( u + iv ) , − ( u + iv ) I pvə ( u + iv ) B / dz ...
... fluid system ; if the suffix w is used to denote properties of the lower fluid , the boundary conditions for eqn ( 6.13 ) have the form ( u + iv ) B → 0 , - ( u + iv ) B— ( u + iv ) = ( u + iv ) , − ( u + iv ) I pvə ( u + iv ) B / dz ...
Page 261
... Fluid Mech . 15 , 560–76 . ( 1965 ) Large eddies in the atmospheric boundary layer and their possible role in the formation of cloud rows . J. atmos . Sci . 22 , 176–84 . ( 1969 ) The generation of Langmuir circulations by the eddy ...
... Fluid Mech . 15 , 560–76 . ( 1965 ) Large eddies in the atmospheric boundary layer and their possible role in the formation of cloud rows . J. atmos . Sci . 22 , 176–84 . ( 1969 ) The generation of Langmuir circulations by the eddy ...
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