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As water vapor evaporates from the warm ocean surface, it is forced upward in the convective clouds that surround the eyewall and rainband regions of a storm. As the water vapor cools and condenses from a gas back to a liquid state, it releases latent heat. The release of latent heat warms the surrounding air, making it lighter and thus promoting more vigorous cloud development.
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QuickTime plug-in
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No cost
Please give credit to NASA GSFC Scientific Visualization Studio.
DLESE Catalog ID:
NASA-SVS-001605
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Related resources:
This resource has a thumbnail image at
'Two hurricances approaching the coast of the United States, with the second hurricance slowed due to cooler waters caused by the track of the first.'
Resource contact / Creator / Publisher:
Author:
Susan Byrne NASA GSFC Scientific Visualization Studio
Principal Investigator:
Robert Adler NASA/GSFC |