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Kyle Chudler, Weixin Xu, and Steven A. Rutledge

katabatic drainage winds from the mountain ranges enhanced offshore flow and therefore convergence with the westerlies. And in the North American Monsoon Experiment (NAME; Lang et al. 2007 ; Nesbitt et al. 2008 ), offshore movement of land-generated convection was determined to contribute a significant fraction of the offshore precipitation. Afternoon convection formed over the Sierra Madre Occidental, and then moved westward into the Gulf of California, often in the form of mesoscale convective

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