Explanation:
The northeastern states receive heavy rainfall due to the orographic effect of the Himalayas, forcing the moisture-laden monsoon winds to rise and condense.
Explanation:
A negative NAO phase is characterized by weaker than normal Azores High and Icelandic Low, leading to weaker westerly winds, colder and drier winters in northern Europe, and milder and wetter winters in southern Europe.
Explanation:
During October, the skies become clear but the land remains moist. High temperatures and humidity create an oppressive 'October Heat' during the retreating monsoon.
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