Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 138
... turbulent region can be characterized by Reynolds numbers of the form Uz Re = บ ( 5.10 ) = The viscous flow merges into the turbulent regime at an average distance z 8 ... turbulent flux 138 § 5.2 TURBULENT TRANSFER NEAR THE INTERFACE.
... turbulent region can be characterized by Reynolds numbers of the form Uz Re = บ ( 5.10 ) = The viscous flow merges into the turbulent regime at an average distance z 8 ... turbulent flux 138 § 5.2 TURBULENT TRANSFER NEAR THE INTERFACE.
Page 143
... turbulent energy as discussed in § 1.6 . Some of this energy is dissipated locally , but the remainder may be converted into other forms of energy . This is specified by eqn ( 1.52 ' ) which , adapted to a quasi - stationary ...
... turbulent energy as discussed in § 1.6 . Some of this energy is dissipated locally , but the remainder may be converted into other forms of energy . This is specified by eqn ( 1.52 ' ) which , adapted to a quasi - stationary ...
Page 157
... turbulent horizontal transports . Direct measurements of the covariances w'T ' and w'q ' have been discussed in the ... turbulent energy — are really insignificant in any particular situation . Reliance on the assumptions that led ...
... turbulent horizontal transports . Direct measurements of the covariances w'T ' and w'q ' have been discussed in the ... turbulent energy — are really insignificant in any particular situation . Reliance on the assumptions that led ...
Contents
INTRODUCTION | 1 |
THE STATE OF MATTER NEAR THE INTERFACE | 42 |
SURFACE WAVES | 98 |
Copyright | |
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Common terms and phrases
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