Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 94
... observations from Australia and from the Indian Ocean to be proportional to the sixth power of the air temperature . Idso and Jackson obtained a remarkably good fit to the same data as well as to observations from Alaska and Arizona by ...
... observations from Australia and from the Indian Ocean to be proportional to the sixth power of the air temperature . Idso and Jackson obtained a remarkably good fit to the same data as well as to observations from Alaska and Arizona by ...
Page 130
... Observations by Burling ( 1959 ) , Kitaigoradskii and Strelakov ( 1963 ) , as well as others quoted by Phillips ... observations on ocean weather ships , it was represented by Pierson and Moskowitz ( 1964 ) in the form = = exp ( -x ...
... Observations by Burling ( 1959 ) , Kitaigoradskii and Strelakov ( 1963 ) , as well as others quoted by Phillips ... observations on ocean weather ships , it was represented by Pierson and Moskowitz ( 1964 ) in the form = = exp ( -x ...
Page 148
... observations in conditions of different stability . The data analysis by Businger et al . shows that a fourth - order function , either eqn ( 5.37 ) or the preceding equation , does fit the observations very well when the lapse rate is ...
... observations in conditions of different stability . The data analysis by Businger et al . shows that a fourth - order function , either eqn ( 5.37 ) or the preceding equation , does fit the observations very well when the lapse rate is ...
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