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Scott A. Braun, Paul A. Newman, and Gerald M. Heymsfield

associated with the strong environmental shear impinged on the entire western flank of the storm, with the driest air wrapping around the southern side of the circulation. It is not yet possible to determine the impact of the SAL and upper-level dry air from these observations. However, ensemble simulations with the Weather Research and Forecasting Model with coupled aerosol–cloud–radiation physics are being used to quantify the role of the SAL and dry air in this case. Fig . 10. Equivalent potential

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