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Kyle Chudler, Weixin Xu, and Steven A. Rutledge

location and amount of precipitation generated by the model disagreed with observations. Only by including both a typical monsoonal wind profile (westerlies in the low levels, easterlies aloft) and ocean surface fluxes did the model simulations fall in accord with observations. In other model simulations, Xie et al. (2006) found that even the relatively small and narrow mountain ranges of Myanmar cause enough impedance of the monsoon flow to create the convergence necessary to generate convection and

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