Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 4
... vector is defined by the relation = = av k Ni = Ɛijk JX j = vi მ , მო , дх , дх ik · The symbol = is used ... vector v with components u and v . Unit vectors in the x , y , z directions are denoted by i , j , k . The usual ...
... vector is defined by the relation = = av k Ni = Ɛijk JX j = vi მ , მო , дх , дх ik · The symbol = is used ... vector v with components u and v . Unit vectors in the x , y , z directions are denoted by i , j , k . The usual ...
Page 8
... vector 20 , with the momentum vector pvz . The vector 2 , is parallel to the polar axis and has a magnitude equal to the earth's angular velocity Ω = 2/24 hr 0.76 × 10-4 s - 1 . = ( 1.13 ) The last term in ( 1.12 ) represents the ...
... vector 20 , with the momentum vector pvz . The vector 2 , is parallel to the polar axis and has a magnitude equal to the earth's angular velocity Ω = 2/24 hr 0.76 × 10-4 s - 1 . = ( 1.13 ) The last term in ( 1.12 ) represents the ...
Page 37
... vector Cgi = aw ək ; = awk ; ak k ( 1.92 ) This vector can differ from the phase velocity c , both in magnitude and direction . The energy of a wave packet was shown to be advected with the group velocity . The flux of energy density ...
... vector Cgi = aw ək ; = awk ; ak k ( 1.92 ) This vector can differ from the phase velocity c , both in magnitude and direction . The energy of a wave packet was shown to be advected with the group velocity . The flux of energy density ...
Contents
INTRODUCTION | 1 |
THE STATE OF MATTER NEAR THE INTERFACE | 42 |
SURFACE WAVES | 98 |
Copyright | |
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advection air-sea amplitude angle approximately atmosphere baroclinic barotropic Brunt-Väisälä frequency bubbles cause changes circulation cloud components constant convection convergence Coriolis force Coriolis parameter cyclonic decrease density anomaly direction dissipation drag coefficient eddy effect Ekman layer equation expression flow fluctuations fluid flux frequency friction function geostrophic gravity waves group velocity height horizontal hurricane increase inertial infrared instability integral interactions interface inversion ITCZ latitude layer depth mean meridional mixed layer moisture molecular momentum motion observations ocean oscillations parameter perturbations phase phase velocity planetary boundary layer potential temperature pressure gradient processes propagation radiance radiation ratio region relatively represents resulting Reynolds number Reynolds stress Rossby waves scale sea surface sea-surface temperature shear specified spectrum storm surface temperature term thermocline transport tropical turbulent upwelling variable variations vector vertical viscosity vorticity wave number wavelength wind stress wind velocity zero zonal дх