Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 4
... , k . The usual vector operation symbols will be used only to represent operations within the horizontal plane . For example , V.v = dx dy du dv + av du ▽ XV = - nz . дх ду In a fluid one has to distinguish between local changes.
... , k . The usual vector operation symbols will be used only to represent operations within the horizontal plane . For example , V.v = dx dy du dv + av du ▽ XV = - nz . дх ду In a fluid one has to distinguish between local changes.
Page 9
... дх Əx2 ( 1.15 ) The velocity vector and the momentum flux tensor must both be continuous across the interface of two ... дх , дх J2vi дх ( 1.17 ) A slightly different form of ( 1.17 ) makes use of the vector identity avi Vj axi = a ...
... дх Əx2 ( 1.15 ) The velocity vector and the momentum flux tensor must both be continuous across the interface of two ... дх , дх J2vi дх ( 1.17 ) A slightly different form of ( 1.17 ) makes use of the vector identity avi Vj axi = a ...
Page 22
... dx dx av av av · + дх , дх дх ; ) 0 . The mean velocities are , of course , affected indirectly through the formation of eddies that can be dissipated . If all eddy transports except those along the vertical are neglected , we can write ...
... dx dx av av av · + дх , дх дх ; ) 0 . The mean velocities are , of course , affected indirectly through the formation of eddies that can be dissipated . If all eddy transports except those along the vertical are neglected , we can write ...
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