Impact Assessment of Orography on the Extreme Precipitation Event of July 2010 over Pakistan: A Numerical Study

Figure 4

(a) Vertically integrated moisture flux and winds between 1000 hPa and 500 hPa, (b) longitude-time graph of moisture flux between 32° and 35°N from 26 to 30 July, (c) time series of geopotential height at 200 hPa, and (d) location of the center of the Tibetan High during the period of 21–31 July, 2010.

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