Leh in Ladakh is the driest place in India, receiving less than 100 mm of annual precipitation due to its location in the rain shadow of the Himalayas.
Explanation:
The Indian Ocean Dipole involves changes in sea surface temperatures and wind patterns across the Indian Ocean, leading to reversals in surface winds and currents during positive and negative phases.
Explanation:
The polar jet stream forms due to the strong temperature contrast between polar air and tropical air, creating a steep pressure gradient and strong winds, which are then deflected by the Coriolis force.
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