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The plume of Mississippi and Atchafalaya River system (MARS) is normally confined to the continental shelf and extends westward. During March 2010, while weather in North America was dominated by unu...
The Lagrangian prediction skill (model ability to reproduce Lagrangian drifter trajectories) of the nowcast/forecast system developed for the Gulf of Mexico at the University of Colorado at Boulder is...
The spatial dependence of Lagrangian displacement and velocity statistics is studied in the context of a data assimilating numerical model of the Gulf Mexico. In the active eddy region of the Western ...
Hurricane Heat Potential of the Gulf of Mexico     Hurricane Heat Potential  Gulf of Mexico       font style='font-size:12px;'> 2009/4/3
It has been demonstrated that a large input of energy from the ocean is necessary to establish and maintain hurricane force winds over the sea. However, there has been no suitable data which could ser...
Deuterium Distribution in the Gulf of Mexico     Deuterium Distribution  Gulf of Mexico       font style='font-size:12px;'> 2009/4/2
The variations of the stable isotopes of hydrogen (protium and deuterium) were determined in the various water masses of the Gulf of Mexico. Surface waters of the central Gulf were found to have an av...
Effects of a Cold-Air Outbreak on Shelf Waters of the Gulf of Mexico     Cold-Air  Gulf of Mexico  Shelf Waters        font style='font-size:12px;'> 2009/3/26
Two surveys of the waters over an area of the continental shelf in the northwestern Gulf of Mexico were made during January 1966. The first observation period was just before a major outbreak of cold,...
Monthly mean dynamic height topographies for the upper 500 m of the Gulf of Mexico, seasonal mean topographies for the upper 1000 m and annual topographies for the deep flow are presented. The dynamic...
The curl of the annual mean wind stress is proposed as the forcing mechanism for the anticyclonic gyre observed in the Cayman Sea. A simple wind-driven model is presented to illustrate how a steady-st...
Current-meter observations obtained at two sites on the continental slope of the eastern Gulf of Mexico, at nominal positions of 29°N, 88°W (the Mobile site) and 27.5°N, 85.5°W (the Tampa site) are pr...
Anticyclonic Rings in the Gulf of Mexico     Anticyclonic Rings  Gulf of Mexico       font style='font-size:12px;'> 2009/2/8
Using the historical data set, this study describes the anticyclonic rings that separated from the Loop Current in the eastern Gulf of Mexico. Six quasi-synoptic data sets are used to describe the evo...
Heat and Freshwater Budgets of the Gulf of Mexico     Freshwater Budgets  Heat  Gulf of Mexico       font style='font-size:12px;'> 2009/2/6
Monthly mean oceanic heat storage rates (QT) for the upper 200 meters of the Gulf of Mexico are calculated directly from multi-annual vertical temperature data. The annual march of QT exhibits a minim...
The Wake of Hurricane Allen in the Western Gulf of Mexico     Hurricane Allen  Western Gulf  Mexico       font style='font-size:12px;'> 2009/1/21
In August 1980, Hurricane Allen passed over a moored array of instruments recording current, temperature and conductivity in the western Gulf of Mexico. An alongshore surge occurred during the storm p...
Observations of currents and temperature at a mooring on the 18 m isobath, 30 km south of the Florida shoreline, are discussed for the 31-day period 15 August–15 September 1978. Tidal currents, having...
Cyclonic Eddies in the Eastern Gulf of Mexico     Cyclonic Eddies  Eastern Gulf of Mexico       font style='font-size:12px;'> 2009/1/14
Cold-domed cyclonic eddies juxtaposed to the cyclonic shear side of the Gulf Loop Current are observed in simultaneously obtained hydrographic, current meter mooring, and satellite infrared data. The ...
Anticyclones originating from the Loop Current are known to propagate into the western Gulf of Mexico. Their frequency of generation, their long lifetimes, and satellite data suggest that at any one t...

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