Kumud MishraAIR 69 · CSE 2024 · 227 wordsTheir whole copy
Opening · a definition
Tropical cyclones are the low pressure regions with high wind velocity being influenced by the coriolis force of the Earth. Ex. cyclone Amphan, Vayu.
Body · points and prose
The Process of formation of tropical cyclones
→ They are formed in the tropical regions of the Earth with 5 necessary conditions:
- Sea surface temperature ↑ 27°C
- Large sea surface area and presence of coriolis force.
- An already existing weak low pressure area.
- Minimum variation in vertical wind speed.
- Upper divergence above the sea level system.
Features of tropical cyclones
↳ cover large sea surface area with high wind velocity. ↳ Develop near low pressure area and frontal system is absent unlike extra tropical cyclones.
Tropical cyclone Eye (calm area)
↳ they generally develop near tropics moving from East to west in North.
Changing nature in the Indian Ocean
- Earlier Bay of Bengal used to experience 6-8 annual cyclones, whereas only 1-2 cyclones in Arabian sea.
- But due to global warming, climate change the cyclones in Arabian sea have increased. Ex. Vayu, Nisarga, Tauktae, Biparjoy.
- The warming of Arabian sea and the Indian ocean Dipole facilitates cyclones.
- The El nino modiki, MJO, Rossby waves with increased moisture have increased the intensity of cyclones.
Close · a way forward
Thus, the need of the hour is to have better Early warning systems in the Indian Ocean region.
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