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operators for the precipitation data are constructed from the CRM outputs and the radiative transfer models of NASA SDSU. The passive microwave simulator takes the background information from model forecasts including atmospheric variables and hydrometeors. A delta–Eddington two-stream radiative transfer with slant view ( Olson and Kummerow 1996 ) calculates the brightness temperatures at the given model resolution. The simulated brightness temperatures are then convolved within the FOV of the specified
operators for the precipitation data are constructed from the CRM outputs and the radiative transfer models of NASA SDSU. The passive microwave simulator takes the background information from model forecasts including atmospheric variables and hydrometeors. A delta–Eddington two-stream radiative transfer with slant view ( Olson and Kummerow 1996 ) calculates the brightness temperatures at the given model resolution. The simulated brightness temperatures are then convolved within the FOV of the specified
