Explanation:
The Indian summer monsoon is strongly influenced by the northward shift of the Intertropical Convergence Zone (ITCZ) over the Indian subcontinent, drawing in moisture-laden winds from the Indian Ocean.
Explanation:
A negative AO phase is characterized by higher than normal pressure over the Arctic and lower than normal pressure over the mid-latitudes. This allows cold Arctic air to spill southward, leading to colder winters in the mid-latitudes.
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