Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 197
... Mixed layers continue to deepen , unless this deepening is counteracted by ... layer . The effect of a stress without any external heat input can be ... mixed layer density Ps Po + yh . Introduction into eqn ( 6.31 ) yields = dh ...
... Mixed layers continue to deepen , unless this deepening is counteracted by ... layer . The effect of a stress without any external heat input can be ... mixed layer density Ps Po + yh . Introduction into eqn ( 6.31 ) yields = dh ...
Page 198
... layer depth . In reality , this depth is time - dependent , and it must be a func- tion of the heat flow as well as other variables . An attempt to combine the two ... mixed - layer wind 198 THE PLANETARY BOUNDARY LAYER § 6.4.
... layer depth . In reality , this depth is time - dependent , and it must be a func- tion of the heat flow as well as other variables . An attempt to combine the two ... mixed - layer wind 198 THE PLANETARY BOUNDARY LAYER § 6.4.
Page 199
... mixed layer to become deeper because of the enhanced generation of turbulent energy . This causes additional entrainment of potentially warm air with a geostrophic value of the momentum from above . However , the air - sea exchange is ...
... mixed layer to become deeper because of the enhanced generation of turbulent energy . This causes additional entrainment of potentially warm air with a geostrophic value of the momentum from above . However , the air - sea exchange is ...
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