Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 60
... Bubbles and spray The air - sea boundary is not a simply connected surface . Bubbles in the water and droplets in the air extend the area of interaction between the two fluids . They also affect the rate and the character of that ...
... Bubbles and spray The air - sea boundary is not a simply connected surface . Bubbles in the water and droplets in the air extend the area of interaction between the two fluids . They also affect the rate and the character of that ...
Page 64
... bubbles causes the area over which bubbles actually rise to be appreciably larger than the visible white - cap area . In the latter , bubbles may be seen to rise to the surface for a minute or more , but they continue to give the water ...
... bubbles causes the area over which bubbles actually rise to be appreciably larger than the visible white - cap area . In the latter , bubbles may be seen to rise to the surface for a minute or more , but they continue to give the water ...
Page 65
... bubble . The ejection speed of these drops is strikingly fast , but decreases with increasing bubble diameter from nearly 100 m / s for a bubble diameter of about 0.007 cm to 10 m / s for bubbles with a diameter of 1 mm . These ejection ...
... bubble . The ejection speed of these drops is strikingly fast , but decreases with increasing bubble diameter from nearly 100 m / s for a bubble diameter of about 0.007 cm to 10 m / s for bubbles with a diameter of 1 mm . These ejection ...
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