Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 48
... cause an upward transport , be- cause the solubility also increases with increasing pressure or depth as indicated in eqn ( 2.13 ) . A secondary minimum of oxygen concen- tration is often found at some hundred metres of depth near the ...
... cause an upward transport , be- cause the solubility also increases with increasing pressure or depth as indicated in eqn ( 2.13 ) . A secondary minimum of oxygen concen- tration is often found at some hundred metres of depth near the ...
Page 116
... cause deformations of the interface . The amplitude of these pressure fluctuations is very small , but under certain circum- stances , they can act much longer than the pebble . They are caused by turbulent eddies which are carried ...
... cause deformations of the interface . The amplitude of these pressure fluctuations is very small , but under certain circum- stances , they can act much longer than the pebble . They are caused by turbulent eddies which are carried ...
Page 208
... cause a rise in 0. by about 10 ° C for a 60 - mb pressure drop along the trajectory . The importance of this additional energy supply to air in the hurricane , before it ascends in the warm core , was stressed particularly by Malkus and ...
... cause a rise in 0. by about 10 ° C for a 60 - mb pressure drop along the trajectory . The importance of this additional energy supply to air in the hurricane , before it ascends in the warm core , was stressed particularly by Malkus and ...
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