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After they have formed, such storms tend to intensify when passing over warmer water and weaken over colder water.
The rate of condensation heating that results from the intense rainfall associated with tropical cyclones is about 10 to the eleventh power kW. In one day, therefore, a storm produces 24 x 10 to the eleventh power kW h, an amount of energy that lies within the range of the yearly consumption of power by many industrialized nations.
Structure of the Storm
The mature tropical cyclone is characterized by a circular pattern of stormclouds and torrential rains, whipped by winds that may reach velocities of 160 to 300 km/h (100 to 180 miles per hour) within a radius of 10 to 100 km (6 to 60 mi) from the storm center...
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