Numerical simulation of tropical cyclone development with latent heat release by the resolvable scales: Propagating small scale features observed in the prehurricane phase
Stanley Lawrence Rosenthal, Environmental Research Laboratories (U.S.), Atlantic Oceanographic and Meteorological Laboratories
U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, 1980 - Nature - 43 pages
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base-state pressure beneath C150 boundary-layer air CLDEX20 cloud elements cloud formed cloud water cold advection compensating subsidence Contour interval convective clouds convective system cooling cross section downdraft drafts dry convective adjustment early convection explicit calculation eyewall function of base-state gravity wave h Exp h figs h of Exp horizontal advection Houze hurricane hydrostatic latent heat lateral mixing low troposphere low-level cold air lowest layers Ludlam maximum vertical motion moist convection moist static energy moist updraft multicell observed occur original cloud plumes precipitation evaporation processes propagating squall line RAD1US KM radially outward real atmosphere relative humidity Rosenthal 1978 saturated section of cloud section of moist section of radial section of temperature small-scale features specific heat capacity stable air stable ascent static energy cutoff static energy divided static energy fig surface pressure-gradient force synoptic scale tangential wind TEMEX20 TROPICAL CYCLONE unsaturated upward motion vortex wind component wind shear Zipser zontal