As the winds converge toward the central core, they spiral upwards, sending warm moist air upwards. As this air rises, it cools and releases its latent heat into the atmosphere to add further energy to the storm.
Winds in a cyclone blow counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere. In a cyclone, air near the ground is pushed toward the low-pressure center of the cyclone, and then rises upward, expanding and cooling as it moves.
As the winds converge toward the central core, they spiral upwards, sending warm moist air upwards. As this air rises, it cools and releases its latent heat into the atmosphere to add further energy to the storm.
Answers & Comments
Answer:
Tropical Cyclone Structure
As the winds converge toward the central core, they spiral upwards, sending warm moist air upwards. As this air rises, it cools and releases its latent heat into the atmosphere to add further energy to the storm.
Explanation:
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Winds in a cyclone blow counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere. In a cyclone, air near the ground is pushed toward the low-pressure center of the cyclone, and then rises upward, expanding and cooling as it moves.
Answer:
Tropical Cyclone Structure
As the winds converge toward the central core, they spiral upwards, sending warm moist air upwards. As this air rises, it cools and releases its latent heat into the atmosphere to add further energy to the storm.