Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 16
... perturbation time scale which is of the same order as the advective time scale w ~ L / U is typical for synoptic scale perturbations in the atmosphere . These perturbations are characterized by Ro < 1 and Re⇒ 1. They cannot cause large ...
... perturbation time scale which is of the same order as the advective time scale w ~ L / U is typical for synoptic scale perturbations in the atmosphere . These perturbations are characterized by Ro < 1 and Re⇒ 1. They cannot cause large ...
Page 174
... perturbations or waves have been observed in laboratory experiments near the boundary of rotating discs or near the bottom of P CI = 0.16 g C1 = 0 · 034 g Type I waves Type II waves FIG . 6.2 . Wavelength ( 21 / do 11.8 ; 211 / do 28.0 ) ...
... perturbations or waves have been observed in laboratory experiments near the boundary of rotating discs or near the bottom of P CI = 0.16 g C1 = 0 · 034 g Type I waves Type II waves FIG . 6.2 . Wavelength ( 21 / do 11.8 ; 211 / do 28.0 ) ...
Page 213
... perturbations . It will be shown in the following section ( eqns ( 7.12 ) , ( 7.13 ) ) that it may be possible to represent low - latitude atmospheric perturbations by a sum of terms which each have a wave - like nature . The preferred ...
... perturbations . It will be shown in the following section ( eqns ( 7.12 ) , ( 7.13 ) ) that it may be possible to represent low - latitude atmospheric perturbations by a sum of terms which each have a wave - like nature . The preferred ...
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