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The winter rainfall in Northern India is locally known as----
A. Airawat
B. Mahawat
C. Sherawat
D. None of these

Answer
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Hint: A western aggravation is an extratropical storm beginning in the Mediterranean area that brings abrupt winter downpour toward the northwestern pieces of the Indian subcontinent. It is a non-monsoonal precipitation design driven by the Westerlies. The dampness in these tempests, as a rule, starts over the Mediterranean Sea, the Caspian Sea, and the Black Sea.

Complete answer:
The winter rainfall in Northern India is locally known as Mahawat. Extratropical storms are worldwide marvels with dampness generally conveyed in the upper climate, dissimilar to their tropical partners where the dampness is conveyed in the lower environment. The chilly climate season starts from mid-November in northern India and remains till February. December and January are the coldest months in the northern piece of India. The temperature diminishes from the south toward the north. The normal temperature of Chennai, on the precipitation happens on the Tamil Nadu coast from these breezes as here they blow from ocean to land. In the northern piece of the nation, a weak high-pressure district creates, light breezes moving outwards from this region. Affected by the alleviation, these breezes blow through the Ganga valley from the west and the northwest. Clear sky, low temperatures, and low mugginess, and weak, variable breezes typically set the climate apart.
So, the correct answer is Option B.

Note: A trademark highlight of the chilly climate season over the northern fields is the inflow of cyclonic aggravations from the west and the northwest. These low-pressure frameworks, begin over the Mediterranean Sea and western Asia and move into India, alongside the westerly stream.