Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
From inside the book
Results 1-3 of 38
Page 71
... wavelength interval 2d2 / 2 . The monochromatic radiance is the fundamental variable in any discussion of radiation ... wavelengths , or at least over a 6 RADIATION General aspects of environmental electromagnetic radiation.
... wavelength interval 2d2 / 2 . The monochromatic radiance is the fundamental variable in any discussion of radiation ... wavelengths , or at least over a 6 RADIATION General aspects of environmental electromagnetic radiation.
Page 73
... wavelength . The refractive index of water increases from 1.332 for light with a wavelength of 0.656 μm at the red end of the spectrum of 1.344 for a wavelength of 0.404 μm at the violet end . Though the difference is less than 1 per ...
... wavelength . The refractive index of water increases from 1.332 for light with a wavelength of 0.656 μm at the red end of the spectrum of 1.344 for a wavelength of 0.404 μm at the violet end . Though the difference is less than 1 per ...
Page 77
... wavelength of light that higher- order terms in the expansion ( 3.12 ) are quite negligible , and Rayleigh scattering , inversely proportional to the fourth power of the wavelength , is produced . The sun radiates most intensely at a ...
... wavelength of light that higher- order terms in the expansion ( 3.12 ) are quite negligible , and Rayleigh scattering , inversely proportional to the fourth power of the wavelength , is produced . The sun radiates most intensely at a ...
Contents
INTRODUCTION | 1 |
THE STATE OF MATTER NEAR THE INTERFACE | 41 |
RADIATION | 71 |
Copyright | |
6 other sections not shown
Other editions - View all
Common terms and phrases
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