Bhavika ChopraAIR 25 · CSE 2025 · 90 wordsTheir whole copy
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The Bay of Bengal is warmer than the Arabian sea and hence more prone to cyclones that form near the Indian shoreline.
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Timing of cyclones: Usually end of south-west monsoon, October, April in Bay of Bengal
Reasons for decrease in frequency in SW monsoon:
- Increase in vertical shear.
- Active movement of Bay of Bengal branch of monsoon.
FORMATION OF CYCLONE
However, the Arabian sea is now witnessing more cyclones due to:
Warming due to climate change.
Higher sea surface and ocean mean temperatures in Arabian sea.
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