## A Diagnostic Model of the Tropical Cyclone in Isentropic Coordinates |

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1600 iterations advection anticyclonic available energy available potential energy baroclinicity boundary layer budget for Experiment cent centered differencing cm sec constant continuity equation convection conversion to kinetic Coriolis parameter decreases dissipation effect efficiency factor energy budget equal Experiment 16 finite difference friction heating function horizontal and vertical horizontal mixing hurricane Hurricane Hilda hydrostatic equation increase infrared inner region internal mixing isentropic coordinates Isentropic cross section isentropic surface izontal kinetic energy latent heat release m/sec mass and momentum maximum wind non-linear instability numerical models oscillations parameters pressure gradient force Radial profiles radial wind profiles radius of maximum rainbands Riehl scale section for slowly sensible heating shown in Figure slowly varying specific kinetic energy tangential and radial tangential wind thermal forcing total heating tropical cyclone troposphere truncation error upper levels upstream differencing values variable grid vertical advection vertical motion Vertical profiles vertical shear warm core watts wind cross section