Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 117
... spectrum at any time will have maximum values for frequencies around k . U „ . The spread around these maximal values must depend on the duration during which the advected pressure fluctuations retain their individual identity . On this ...
... spectrum at any time will have maximum values for frequencies around k . U „ . The spread around these maximal values must depend on the duration during which the advected pressure fluctuations retain their individual identity . On this ...
Page 129
... spectrum has not been found generally acceptable . Though their use in preference to non - dimensional constants does not necessarily reduce the practical usefulness of an empirical relation as such , provided the units are well defined ...
... spectrum has not been found generally acceptable . Though their use in preference to non - dimensional constants does not necessarily reduce the practical usefulness of an empirical relation as such , provided the units are well defined ...
Page 158
... spectrum is not isotropic in the measured range , if the downstream fluctuations along the wind direction have more power than the vertical or transverse fluctuations , the dissipation is overestimated by the application of ( 1.84 ) ...
... spectrum is not isotropic in the measured range , if the downstream fluctuations along the wind direction have more power than the vertical or transverse fluctuations , the dissipation is overestimated by the application of ( 1.84 ) ...
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