Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 27
... function ( 1.56 ) . For stationary processes , the two functions are related by the Fourier transform 00 ∞ G ( w ) = √ R ( d ) e - iw8 d8 = 2 [ R ( d ) cos ( wd ) dd . ( 1.64 ) The second equality is explained by the fact that the ...
... function ( 1.56 ) . For stationary processes , the two functions are related by the Fourier transform 00 ∞ G ( w ) = √ R ( d ) e - iw8 d8 = 2 [ R ( d ) cos ( wd ) dd . ( 1.64 ) The second equality is explained by the fact that the ...
Page 28
... function . Because the cross - correlation is not necessarily even , this generally yields a complex number JR , ( d ) e -iwd d8 = C'ƒg ( w ) —¿Qƒ , ( w ) . ( 1.67 ) The real part C ,, ( w ) is called the co - spectral density function ...
... function . Because the cross - correlation is not necessarily even , this generally yields a complex number JR , ( d ) e -iwd d8 = C'ƒg ( w ) —¿Qƒ , ( w ) . ( 1.67 ) The real part C ,, ( w ) is called the co - spectral density function ...
Page 145
... function of the stress , the height above the interface , and the wave spectrum . When a sea is fully developed , these quantities cannot be independent of each other . It is then possible to express them all as a function of the stress ...
... function of the stress , the height above the interface , and the wave spectrum . When a sea is fully developed , these quantities cannot be independent of each other . It is then possible to express them all as a function of the stress ...
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