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J. Li, S. Sorooshian, W. Higgins, X. Gao, B. Imam, and K. Hsu

b ), the model underestimates the CAPE in this region during surge periods. The modeled vector wind and potential temperature for the 29th sigma layers (∼0.9865) at 0300, 0500, 0700, and 0900 UTC 13 July 2004 ( Fig. 13 ) show colder and stronger outflow for the high-resolution run. These results support the conclusions of previous studies that the model can reproduce upslope winds very well. A comparison of the model-generated southerly winds at both resolutions at the grid point nearest ISS4

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