- A tropical cyclone is a storm system characterized by a large low-pressure center and numerous thunderstorms that produce strong winds and heavy rain. Tropical cyclones feed on heat released when moist air rises, resulting in condensation of water vapor contained in the moist air
OCEAN BASIN
SEASON
AVERAGE CYCLONES PER SEASON
(winds above 63 km/h)
PERCENTAGE OF GLOBAL TOTAL
SEVERE CYCLONES PER SEASON
(winds above 120 km/h) North Indian May to June & October to December
5.4
7%
2.5 Northwest Pacific Mainly June to December
25.7
31%
16.0 Northeast Pacific May to November
16.5
20%
8.9 North Atlantic June to November
9.7
11%
5.4 Southwest Indian December to April
10.4
12%
4.4 Southeast Indian/Aust December to April
6.9
8%
3.4 Southwest Pacific November to April
9.0
11%
4.3 - Queensland
- 10
- Typhoons, Hurricanes
- Tropical cyclones develop in the Tropical regions of the world. Heat from the sun causes warm,High air to rise into the atmosphere. As the air rises, a low pressure system forms and condensation occurs, which releases latent heat causing the air to rise further into the atmosphere. If the air pressure in the upper atmosphere is Moist , then the rising column of warm air will Spiral outwards in the upper atmosphere and air will rush from the Surface to replace it, forming a tropical cyclone.
- Is the centre of the storm and it is calm and has clear eyes
- If they arn't intense enough
Tuesday, May 10, 2011
2.5
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