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... the aridity of the Tibetan plateau and the Tarim basin of W China results from the interception of the moisture-laden northwest monsoon by the Himalayas' southern face. Consequently, the northern slopes receive relatively light snowfall and have little drainage, while the snow-covered and extensively glaciated southern slopes give rise to the Indian subcontinent's major rivers, including the Indus, Sutlej, Ganges, and Brahmaputra.
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