Tropical Cyclone Development and Dissipation
A tropical cyclone is an intense low-pressure system formed over warm oceans, characterized by strong winds and heavy rainfall.
Stages of Development:
- Formative Stage (Tropical Disturbance)
- Cluster of thunderstorms with weak circulation.
- Sea surface temperature $> 26.5^\circ C$.
- Sufficient Coriolis force (at least $5^\circ$ from equator).
- Intensification Stage (Tropical Depression)
- Closed isobars develop.
- Wind speed: $37 - 62 \text{ km/h}$.
- Central pressure decreases.
- Mature Stage (Tropical Cyclone)
- Well-developed eye at center.
- Eyewall with strongest winds.
- Wind speed $> 119 \text{ km/h}$.
Stages of Dissipation:
- Landfall: Moisture supply cuts off; weakening begins.
- Weakening Stage: Wind speeds decrease; structure disorganizes.
- Dissipation Stage: System becomes a remnant low-pressure area.
Necessary Conditions:
- Warm ocean water $\ge 26.5^\circ C$.
- Low vertical wind shear.
- High humidity.
- Pre-existing disturbance.
Energy Source:
Energy is derived from latent heat of condensation released by rising moist air.