An El Niño-Southern Oscillation (ENSO) episode typically develops in the tropical Pacific during boreal spring/summer, reaches peak intensity during late autumn or winter, and dissipates in the following spring, lasting for a typical duration of several months (approximately 9 to 18 months).
Correct Option: Option 3 (Several months).
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Southern Oscillation Index (SOI): A standardized meteorological index that quantifies the atmospheric phase of ENSO.
It measures the normalized sea level atmospheric pressure difference between Tahiti (in the central Pacific) and Darwin, Australia (in the western Pacific):
Sustained negative SOI values indicate El Niño events.
Sustained positive SOI values indicate La Niña events.
Correct Option: Option 2 (By monitoring changes in atmospheric pressure).
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The Indian Ocean Dipole (IOD) (or Indian Niño) is an ocean-atmosphere coupled climate phenomenon across the equatorial Indian Ocean.
It is defined by the anomalous difference in Sea Surface Temperature (SST) between the western tropical Indian Ocean (Arabian Sea) and the eastern tropical Indian Ocean (south of Indonesia), measured as the Dipole Mode Index (DMI).
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