Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 20
... specified or estimated in a meaningful manner , which is not always possible . = When the equation of continuity is averaged we get , with the specified notation , It дрд + pvi d x i = др + Ət д др a д ( p + p ' ) ( V2 + ví ) = + ¿ Vi + ...
... specified or estimated in a meaningful manner , which is not always possible . = When the equation of continuity is averaged we get , with the specified notation , It дрд + pvi d x i = др + Ət д др a д ( p + p ' ) ( V2 + ví ) = + ¿ Vi + ...
Page 72
... specified usually in langleys per minute ( 1 ly min - 1 = 1 cal cm - 2 min - 1 = 0.0698 W cm - 2 ) . The irradiance of a horizontal surface ( 0 = 6 ) from above is specified by the integral 2π J1 = √ I cos & do . Jo ( 3.3 ) The ...
... specified usually in langleys per minute ( 1 ly min - 1 = 1 cal cm - 2 min - 1 = 0.0698 W cm - 2 ) . The irradiance of a horizontal surface ( 0 = 6 ) from above is specified by the integral 2π J1 = √ I cos & do . Jo ( 3.3 ) The ...
Page 107
... specified by ( 4.27 ) must not be confused with the sublayer thickness for a constant velocity which was specified in ( 2.25 ) . The ratio of the two fluid masses affected by the viscous diffusion of vorticity from the interface is ...
... specified by ( 4.27 ) must not be confused with the sublayer thickness for a constant velocity which was specified in ( 2.25 ) . The ratio of the two fluid masses affected by the viscous diffusion of vorticity from the interface is ...
Contents
INTRODUCTION | 1 |
THE STATE OF MATTER NEAR THE INTERFACE | 41 |
RADIATION | 71 |
Copyright | |
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advection air-sea amplitude angle approximately atmosphere average baroclinic barotropic bubbles cause changes circulation cloud components constant convection convergence Coriolis force decrease denotes diffusion direction dissipation drag coefficient eddy effect Ekman layer equation equilibrium expression flow fluctuations fluid flux Fourier frequency friction function geostrophic gravity waves group velocity height horizontal hurricane increase inertial integral interaction interface kinetic energy larger latitude linear mean mixed layer moisture molecular momentum motion observations ocean parameter perturbations phase velocity planetary boundary layer potential temperature processes propagation radiance ratio region relatively represents resulting Reynolds number Reynolds stress Rossby waves salinity scale sea surface sea water sensible heat shear specific humidity specified spectral spectrum storm term thermocline transport tropical turbulent unstable upwelling vapour pressure variable variations vector vertical viscosity vorticity wave number wavelength wind stress wind velocity yields zero дх