DocumentCode
2558378
Title
Turbines can suppress Loop Current to reduce Gulf of Mexico hurricane threat
Author
LaRosa, Richard
Author_Institution
sealevelcomtrol.com, South Hempstead, NY, USA
fYear
2010
fDate
7-7 May 2010
Firstpage
1
Lastpage
6
Abstract
When the Loop Current (LC) intrudes into the Gulf of Mexico (GoM) it collects a deep pool of warm water that can energize a hurricane which passes through it. Data is presented to support the hypothesis that the LC is driven by gravity, and that its intrusion is a way of dissipating extra hydraulic drive power caused by the higher mean sea level at Grand Cayman Island compared to Grand Bahama Island. If some of this extra drive power is converted by submerged turbines into electric power for the shore grid, and the rest is dissipated by eddies shed by mooring cables and turbine structures, there will be no warm pools to energize hurricanes. Some turbine design estimates are made and a possible configuration is shown.
Keywords
gravity; hydraulic turbines; ocean thermal energy conversion; oceanographic equipment; oceanographic regions; storms; Coriolis force; Grand Bahama Island; Grand Cayman Island; Gulf of Mexico hurricane threat; dynamic height contours; electric power; extra hydraulic drive power; floating turbines; gravity influence; hurricane supression; loop current intrusion; mean sea level; mooring cables; ocean surface currents; radar altimetry; sea surface height; shore grid; submerged turbines; turbine structures; turbulent shear; warm pools; Cables; Gravity; Hurricanes; Hydraulic drives; National electric code; Oceans; Power systems; Sea level; Sea surface; Turbines; Coriolis force; Gulf of Mexico; Loop Current intrusion; dynamic height contours; floating turbines; hurricane suppression; radar altimetry; sea surface height; turbulent shear;
fLanguage
English
Publisher
ieee
Conference_Titel
Applications and Technology Conference (LISAT), 2010 Long Island Systems
Conference_Location
Farmingdale, NY
Print_ISBN
978-1-4244-5548-5
Electronic_ISBN
978-1-4244-5550-8
Type
conf
DOI
10.1109/LISAT.2010.5478277
Filename
5478277
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