Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 23
... transports parametrically as functions of the averaged or bulk variables which are measured routinely . This has been done in the past by the introduction of empirically estimated coefficients of eddy transport defined by ат _KH z av v ...
... transports parametrically as functions of the averaged or bulk variables which are measured routinely . This has been done in the past by the introduction of empirically estimated coefficients of eddy transport defined by ат _KH z av v ...
Page 49
... transport coefficients Molecular transports can become important particularly in the immediate vicinity of the air - sea interface . Values for the transport coefficients at standard sea - level pressure are listed in Table 2.3 . The ...
... transport coefficients Molecular transports can become important particularly in the immediate vicinity of the air - sea interface . Values for the transport coefficients at standard sea - level pressure are listed in Table 2.3 . The ...
Page 199
... transport of energy mass and particular substances . The divergence of this integrated mass transport in the oceanic bound- ary layer can create localized upwelling which has often large climatic and ecological effects . In the ...
... transport of energy mass and particular substances . The divergence of this integrated mass transport in the oceanic bound- ary layer can create localized upwelling which has often large climatic and ecological effects . In the ...
Contents
INTRODUCTION | 1 |
THE STATE OF MATTER NEAR THE INTERFACE | 41 |
RADIATION | 71 |
Copyright | |
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Common terms and phrases
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