Animation loop of how sea surface temperature responds to the storm.
DESCRIPTION: CONTACT:
Comparison of Sea Surface Temperature (SST) before and after hurricane Ivan between a GoM-HYCOM simulation and infrared satellite measurements. The two cold spots are regions where the supply of heat from the ocean to the storm is reduced, which acts to reduce storm intensity. They form where two cyclonic, cold-core eddies (blue spots, top panel) exist when the storm hits. The upper ocean warm layer is very thin over these features, allowing the storm to efficiently mix deeper cold water up to the surface.
George Halliwell — ghalliwell@rsmas.miami.edu
Villy Kourafalou — vkourafalou@rsmas.miami.edu
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