Explanation:
The MJO is a 30-60 day oscillation of convection that moves eastward from the Indian Ocean to the Pacific. It can enhance or suppress monsoon rainfall depending on its phase.
Explanation:
The Indian monsoon is influenced by multiple factors, including El Niño-Southern Oscillation (ENSO), the land-sea temperature contrast (which creates a thermal low over Asia), and the movement of the Intertropical Convergence Zone (ITCZ).
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