Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 102
... expression ( 4.1 ) indicates that maximal contribution of any particular Fourier com- ponent to this slope is ac дх | A | k = ( AA * ) * k . max ( 4.14 ) From ( 4.3 ) it can be seen further that in a statistically stationary wave field ...
... expression ( 4.1 ) indicates that maximal contribution of any particular Fourier com- ponent to this slope is ac дх | A | k = ( AA * ) * k . max ( 4.14 ) From ( 4.3 ) it can be seen further that in a statistically stationary wave field ...
Page 113
... expression for the work of the viscous stress in the air : ∞ -2 Pava ( du dua ди 2 ди · + . + მ 2 . Əz Əz dz ~ -2ρa1aw2AA * / 81⁄2 . The viscous attenuation W , ( k ) of wave energy in both media is made up by the sum of the last two ...
... expression for the work of the viscous stress in the air : ∞ -2 Pava ( du dua ди 2 ди · + . + მ 2 . Əz Əz dz ~ -2ρa1aw2AA * / 81⁄2 . The viscous attenuation W , ( k ) of wave energy in both media is made up by the sum of the last two ...
Page 121
... expression is integrated vertically and averaged horizontally , we get an expression for the wave - induced vertical momentum flux W , ∞ [ < n'w ' ) dz = - ( u'w ' ) z = -u'w'z = TPa ( 4.53 ) The relations ( 4.51 ) and ( 4.52 ) show ...
... expression is integrated vertically and averaged horizontally , we get an expression for the wave - induced vertical momentum flux W , ∞ [ < n'w ' ) dz = - ( u'w ' ) z = -u'w'z = TPa ( 4.53 ) The relations ( 4.51 ) and ( 4.52 ) show ...
Contents
INTRODUCTION | 1 |
THE STATE OF MATTER NEAR THE INTERFACE | 42 |
SURFACE WAVES | 98 |
Copyright | |
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advection air-sea amplitude angle approximately atmosphere baroclinic barotropic Brunt-Väisälä frequency bubbles cause changes circulation cloud components constant convection convergence Coriolis force Coriolis parameter cyclonic decrease density anomaly direction dissipation drag coefficient eddy effect Ekman layer equation expression flow fluctuations fluid flux frequency friction function geostrophic gravity waves group velocity height horizontal hurricane increase inertial infrared instability integral interactions interface inversion ITCZ latitude layer depth mean meridional mixed layer moisture molecular momentum motion observations ocean oscillations parameter perturbations phase phase velocity planetary boundary layer potential temperature pressure gradient processes propagation radiance radiation ratio region relatively represents resulting Reynolds number Reynolds stress Rossby waves scale sea surface sea-surface temperature shear specified spectrum storm surface temperature term thermocline transport tropical turbulent upwelling variable variations vector vertical viscosity vorticity wave number wavelength wind stress wind velocity zero zonal дх