This paper will investigate the ability of COAMPSTM to resolve frontal passages across the west coast of the United States. Specifically, the timing and pre and postfrontal low-level wind flows will be evaluated against available observational data and/or model analyses. The emphasis will be on fronts associated with winter storms since frontal structure, including temperature gradient and directional and/or speed shear are generally most clearly defined during these events. The other area of investigation will include COAMPSTM performance in forecasting the timing, areal coverage, and intensity of pre and postfrontal precipitation. The wealth of observational data collected through CALJET and/or PACJET experiments will aid the evaluation of COAMPSTM performance.
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