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Earth Observing Laboratory
Field Data Archive

GOTEX: Gulf Of Tehuantepec Experiment, Coupled Development of Ocean Waves and Boundary Layers (aka OceanWaves)

Summary

When high pressure is over the Gulf of Mexico in the Caribbean, a circulation sets up forcing strong winds through the Chivela mountain pass, creating an off-shore jet over the Pacific Ocean. The wind can blow out for 500-600 km offshore for several days giving rise to strongly-forced fetch-limited wave conditions. In February 2004, groups from Scripps Institution of Oceanography (UCSD), UC Irvine, NASA/EG&G, NCAR and the National Autonomous University of Mexico collaborated to conduct the Gulf of Tehuantepec Experiment (GOTEX) to measure the coupled development of the atmospheric boundary layer and the surface wave field out over the Gulf of Tehuantapec, off southern Mexico's Pacific coast. The NSF/NCAR C-130Q Hercules aircraft was equipped with a suite of sensors for measuring surface waves and wave breaking, including a downward-looking scanning lidar (Airborne Terrain Mapper, or ATM), video cameras, inertial motion sensors, and radome gust probe wind measurements. (Taken from Melville, W.K. "Extreme wave events in the Gulf of Tehuantapec" Pp2 [Available online April 2010 from http://www.soest.hawaii.edu/PubServices/2005pdfs/Melville.pdf])

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Temporal coverage

Begin Date 2004-01-25 00:00:00
End Date 2004-02-29 23:59:59

Spatial coverage


Map data from IBCSO, IBCAO, and Global Topography.

Maximum (North) Latitude: 17.00, Minimum (South) Latitude: 12.00
Minimum (West) Longitude: -98.00, Maximum (East) Longitude: -92.00

NSF

This material is based upon work supported by the NSF National Center for Atmospheric Research, a major facility sponsored by the U.S. National Science Foundation and managed by the University Corporation for Atmospheric Research. Any opinions, findings and conclusions or recommendations expressed in this material do not necessarily reflect the views of the U.S. National Science Foundation.