Explanation:
Western Disturbances are most active during the winter season (December to February), bringing essential rainfall and snowfall to the northern and northwestern parts of India.
Explanation:
Lake-effect snow occurs when cold, dry air moves over a relatively warm lake, picking up moisture and heat, which leads to intense convection and heavy snowfall downwind of the lake.
Explanation:
The Atacama Desert is extremely dry due to a combination of the cold Humboldt Current off the coast (which cools the air and limits evaporation) and the rain shadow effect of the Andes Mountains.
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