A note on the hydrostatic equation in the NHEML two-dimensional hurricane model
Michael S. Moss, Stanley Lawrence Rosenthal, Environmental Research Laboratories (U.S.). Weather Modification Program Office
Weather Modification Program Office, Environmental Research Laboratories, 1975 - Hurricanes - 15 pages
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7T cr V,T,q actual and computed assumption of constant atmos atmosphere with constant circulation model CM rH CN CN compute the geopotential computed heights computed individual sums computed thicknesses computed via equations constant lapse rate CpT)dodr dependent variables dry adiabatic Experimental Meteorology Laboratory geopotential height given atmospheric levels H 4J Hurricane and Experimental HYDROSTATIC EQUATION hydrostatic formulation idealized atmosphere known heights lapse rate atmosphere layers Vertical structure lowest applicable level lowest model layer Matsuno model parameters model structure modified and ordinary modified UCLA hydrostatic NHEML two-dimensional hurricane number of levels obtain the geopotential ordinary UCLA 1974 Percent heights error phere planetary boundary layer potential temperature remaining levels rH CM rH rH CN rH rH rH sigma surfaces total energy truncation error two-dimensional hurricane model U.C.L.A. Hydrostatics UCLA general circulation UCLA Staff Members various constant lapse versus the number Vertical structure essentially