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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
📍 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
Forwarded from UPSC Mapping Prelims Mains
🔆 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
📍 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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