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Tropical storms obtain their energy from the ocean waters below. As a storm moves across the Gulf of Mexico, it may interact with an upwelling of cooler waters from the deeper ocean or, in the case of Isaac, a downwelling inside rings of warm water that separated from a warm-water current, called the Loop Current, that moves through the Gulf of Mexico to join with the Gulf Stream along the U.S. East Coast. As the storm moves forward, ocean temperatures are fueling the storm's intensity. UM Rosenstiel School of Marine and Atmospheric Science researchers, in collaboration with NOAA's Atlantic Oceanographic and Meteorological Laboratory, deployed a total of 376 airborne sensors during six NOAA hurricane hunter aircraft flights conducted before, during, and after the passage of Isaac over the eastern Gulf of Mexico. The researchers observed a predominant downwelling of water inside these warm-water rings, or eddies, from the Loop Current, which caused its intensification from a tropical storm to a category 1 hurricane just prior to landfall.
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