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The proposed advantages of the CASA radar network include a high-resolution sampling of the lower atmosphere using small, low-cost radars and the ability of the network of Doppler radars to dynamically adapt to changing conditions. These features should improve the detection of hazardous weather events in the lower atmosphere that may be missed by the existing WSR-88D network, and will provide more complete data for the initialization of numerical models.
Unlike our previous studies that were limited to a single idealized supercell case, additional types of convective storms, including multi-cellular convective systems, are simulated within the radar network. Assimilations and forecasts are performed by incorporating the simulated radar data into the Advanced Regional Prediction System (ARPS) model using the EnSRF method.
Supplementary URL: http://weather.ou.edu/~savageau/research/