Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 86
... upwelling infrared radiance : 9 Bo ΧΥ 1. = B2 ( 1 + xx ( 2 + 008 ) ) = B. ( 1+ cos 4 ) . I 2π cos β 2π z = 0 β For normal viewing of the sea surface , this becomes Bo 14- = B. ( 1 + 27 ) . I 2π β ( 3.24 ) ( 3.25 ) The value of the ...
... upwelling infrared radiance : 9 Bo ΧΥ 1. = B2 ( 1 + xx ( 2 + 008 ) ) = B. ( 1+ cos 4 ) . I 2π cos β 2π z = 0 β For normal viewing of the sea surface , this becomes Bo 14- = B. ( 1 + 27 ) . I 2π β ( 3.24 ) ( 3.25 ) The value of the ...
Page 87
... upwelling radiance which is trans- mitted to the observer . Except for B - the black - body emittance at surface temperature all these quantities vary with the viewing angles . The increase of r , as one looks out more horizontally ...
... upwelling radiance which is trans- mitted to the observer . Except for B - the black - body emittance at surface temperature all these quantities vary with the viewing angles . The increase of r , as one looks out more horizontally ...
Page 275
... Upwelling , 86 Vapour pressure , 44 , 52f . Variance , 25f . , 201f . Velocity of sound , 6 , 18 Velocity profile below the interface , 141f . Visible light and infrared radiation , 71f . absorption , 35 , 75f . , 82f . , 85f . , 89 ...
... Upwelling , 86 Vapour pressure , 44 , 52f . Variance , 25f . , 201f . Velocity of sound , 6 , 18 Velocity profile below the interface , 141f . Visible light and infrared radiation , 71f . absorption , 35 , 75f . , 82f . , 85f . , 89 ...
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