Explanation:
Ladakh, particularly the region around Leh, is the driest place in India, receiving less than 100 mm of precipitation annually due to its location in the rain shadow of the Himalayas.
Explanation:
Ozone depletion does not affect the Indian monsoon. The monsoon is influenced by El Niño, IOD, ITCZ, Jet Streams, and land-sea temperature contrast.
Explanation:
The central United States, including the Midwest and Northeast, has a humid continental climate (Dfa/Dfb) characterized by warm to hot summers, cold winters, and moderate precipitation.
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