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13B. The longitudinal gradient of rainfall from the west coast to the center of the continent across 40° N latitude in North America is best explained by:A. The descending air from Hadley Cells being concentrated in the central United StatesB. The intertropical convergence zone being centered at 120° West LongitudeC. The rainshadow effectD. Northward shifting of the northern hemisphere Hadley Cell during this time of year E. C and D acting together
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