Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 15
... zero and unity . | n × ( v — Vg ) | | vg | = │n × ( v * _v * ) | < 1 . It is zero when the motion is geostrophic . It does not usually exceed unity because it is very rare for the actual wind to be either opposed or to be twice as ...
... zero and unity . | n × ( v — Vg ) | | vg | = │n × ( v * _v * ) | < 1 . It is zero when the motion is geostrophic . It does not usually exceed unity because it is very rare for the actual wind to be either opposed or to be twice as ...
Page 20
... zero by definition : T'q ' = v ' = 0 , etc. This statement is based on the supposition that a mean exists and that it can be specified or estimated in a meaningful manner , which is not always possible . = When the equation of ...
... zero by definition : T'q ' = v ' = 0 , etc. This statement is based on the supposition that a mean exists and that it can be specified or estimated in a meaningful manner , which is not always possible . = When the equation of ...
Page 101
... zero , and this is possible only if the summation terms are zero individually for all values of k and t . The term containing ǝA / Ət is in quadrature with all the other terms . It has to be zero separately and must remain zero for any ...
... zero , and this is possible only if the summation terms are zero individually for all values of k and t . The term containing ǝA / Ət is in quadrature with all the other terms . It has to be zero separately and must remain zero for any ...
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