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a Resulting circulation patterns for Model I
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60 hours 72 hours advection amplitudes anti-cyclonic flow approximately barotropic boundary conditions Circulation developed cm/sec Coriolis parameter curves cyclonic flow decrease density anomaly depth diffusion of momentum downwelling effects Ekman Ekman layer elapsed energy rate far-field finite-difference fluid frictional gradually gravity waves half-strength homogeneous model homogeneous ocean hurricane Hilda hurricane structure Ichiye inertial oscillations inflow angle initial isopycnal surfaces kinetic energy Leipper magnitude maximum wind motion near-field nonlinear numerical numerical stability O'Brien and Reid oceanic spin-up particle velocities permanent thermocline plane primitive equations r(km radius of maximum sea surface temperature selected radii spatially integrated spin-down process stationary hurricane storm stratified models stratified ocean's response stratified region tangential component Temporal variation thermal mixing thermocline transient transitory wind turbulent two-layer upwelling values variables vertical advection vertical convective circulation vertical gradients vertical structure volume transports wind field wind intensity wind stress components wind stress field wind system