Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 209
... hurricane crosses a coastline . With hurricane winds it is not possible to neglect the squares and products of the horizontal velocity components even in the boundary layer . For steady axially - symmetric storms , the integrated ...
... hurricane crosses a coastline . With hurricane winds it is not possible to neglect the squares and products of the horizontal velocity components even in the boundary layer . For steady axially - symmetric storms , the integrated ...
Page 210
... hurricane area . His findings suggest that a tropical cyclone consumes more water vapour and latent heat than can be obtained from the pre - existing undisturbed tropical atmosphere . The hurricane must collect vapour from the ocean to ...
... hurricane area . His findings suggest that a tropical cyclone consumes more water vapour and latent heat than can be obtained from the pre - existing undisturbed tropical atmosphere . The hurricane must collect vapour from the ocean to ...
Page 265
... hurricane : Part I. J. atmos . Sci . 24 ( 2 ) , 197–207 . OOYAMA , K. ( 1969 ) Numerical simulation of the life cycle of tropical cyclones . J. atmos . Sci . 26 ( 1 ) , 3–40 . OSTLUND , H. G. ( 1967 ) Hurricane tritium I : preliminary ...
... hurricane : Part I. J. atmos . Sci . 24 ( 2 ) , 197–207 . OOYAMA , K. ( 1969 ) Numerical simulation of the life cycle of tropical cyclones . J. atmos . Sci . 26 ( 1 ) , 3–40 . OSTLUND , H. G. ( 1967 ) Hurricane tritium I : preliminary ...
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