Explanation:
The Thar Desert receives low rainfall due to its location in the rain shadow of the Aravalli Range, the influence of the subtropical high-pressure belt, and its distance from the sea.
Explanation:
The MJO is characterized by an eastward-moving pattern of enhanced and suppressed convection (thunderstorms) across the Indian and Pacific Oceans, influencing rainfall and wind patterns.
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.
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