Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 67
... increases with the wind speed much faster than linearly . The air driven across the face of the sea in a ... increase in temperature . Whether bubbles are larger when big waves break is not known at present . 2.5 . Sea ice ...
... increases with the wind speed much faster than linearly . The air driven across the face of the sea in a ... increase in temperature . Whether bubbles are larger when big waves break is not known at present . 2.5 . Sea ice ...
Page 78
... increases with the sun's zenith distance from 16 per cent when the height of the sun is 60 ° to about 37 per cent ... increase the light scattered down vertically . All these effects are illustrated in Fig . 3.1 . When the sea is ...
... increases with the sun's zenith distance from 16 per cent when the height of the sun is 60 ° to about 37 per cent ... increase the light scattered down vertically . All these effects are illustrated in Fig . 3.1 . When the sea is ...
Page 87
... increase of r , as one looks out more horizontally , was illustrated by Fig . 3.1 . On the other hand , ɛ decreases ... increases . Near the horizon , however , the opposite holds . The sky radiance reflected into the line of sight ...
... increase of r , as one looks out more horizontally , was illustrated by Fig . 3.1 . On the other hand , ɛ decreases ... increases . Near the horizon , however , the opposite holds . The sky radiance reflected into the line of sight ...
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