Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 4
... zero for ik . The com- ponents of the alternating tensor εijk are by definition equal to +1 when the indices are in the cyclical sequence 1 , 2 , 3 , or 2 , 3 , 1 , or 3 , 1 , 2 ; they are equal to -1 when they are not cyclical , and ...
... zero for ik . The com- ponents of the alternating tensor εijk are by definition equal to +1 when the indices are in the cyclical sequence 1 , 2 , 3 , or 2 , 3 , 1 , or 3 , 1 , 2 ; they are equal to -1 when they are not cyclical , and ...
Page 15
... zero and unity . │nx ( v ― Vg ) | | vg | = [ nx ( v * v * ) < 1 . It is zero when the motion is geostrophic . It does not usually exceed unity because it is very rare for the actual wind to be either opposed or to be twice as large as ...
... zero and unity . │nx ( v ― Vg ) | | vg | = [ nx ( v * v * ) < 1 . It is zero when the motion is geostrophic . It does not usually exceed unity because it is very rare for the actual wind to be either opposed or to be twice as large as ...
Page 101
... zero , and this is possible only if the summation terms are zero individually for all values of k and t . The term containing A / ǝt is in quadrature with all the other terms . It has to be zero separately and must remain zero for any ...
... zero , and this is possible only if the summation terms are zero individually for all values of k and t . The term containing A / ǝt is in quadrature with all the other terms . It has to be zero separately and must remain zero for any ...
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