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 | 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