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🔆 Indian Ocean Dipole (IOD) & Indian Monsoon 🌧️

📍 What is IOD?
The Indian Ocean Dipole (IOD) is a climate phenomenon caused by temperature differences between the eastern (Bay of Bengal) and western (Arabian Sea) regions of the Indian Ocean. It greatly impacts the Indian monsoon and rainfall distribution.

🔹 Positive IOD:
Warmer West, Cooler East - Warmer sea temperatures in the west and cooler in the east create favorable conditions for rainfall.
Enhanced Monsoon - Strengthens monsoon circulation, increasing rainfall in central India.
Increased Rainfall - Observed above-average rainfall in central India during positive IOD years.

🔻 Negative IOD:
Cooler West, Warmer East - Temperature reversal leads to a weaker monsoon.
Weaker Monsoon - Disrupts monsoon circulation, causing a delayed or weak monsoon.
Drought Risk - Potential drought conditions, particularly in central and eastern India, with below-average rainfall.

#Geography

🔆 Indian Ocean Dipole (IOD) & Indian Monsoon 🌧️

📍 What is IOD?
The Indian Ocean Dipole (IOD) is a climate phenomenon caused by temperature differences between the eastern (Bay of Bengal) and western (Arabian Sea) regions of the Indian Ocean. It greatly impacts the Indian monsoon and rainfall distribution.

🔹 Positive IOD:
Warmer West, Cooler East - Warmer sea temperatures in the west and cooler in the east create favorable conditions for rainfall.
Enhanced Monsoon - Strengthens monsoon circulation, increasing rainfall in central India.
Increased Rainfall - Observed above-average rainfall in central India during positive IOD years.

🔻 Negative IOD:
Cooler West, Warmer East - Temperature reversal leads to a weaker monsoon.
Weaker Monsoon - Disrupts monsoon circulation, causing a delayed or weak monsoon.
Drought Risk - Potential drought conditions, particularly in central and eastern India, with below-average rainfall.

#Geography


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