State estimates and forecasts of the loop current in the Gulf of Mexico using the MITgcm and its adjoint

Author:

Gopalakrishnan Ganesh1,Cornuelle Bruce D.1,Hoteit Ibrahim2,Rudnick Daniel L.3,Owens W. Brechner4

Affiliation:

1. Climate, Atmospheric Science and Physical Oceanography; Scripps Institution of Oceanography; La Jolla, San Diego California USA

2. Department of Earth Sciences and Engineering, King Abdullah University of Science and Technology; Jeddah Kingdom of Saudi Arabia

3. Marine Physical Laboratory; Scripps Institution of Oceanography; La Jolla California USA

4. Physical Oceanography; Woods Hole Oceanographic Institution; Woods Hole Massachusetts USA

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Reference58 articles.

1. DNSC08 mean sea surface and mean dynamic topography models;Andersen;J. Geophys. Res. Oceans,2009

2. Assimilation of high-frequency radar currents in a nested model of the West Florida Shelf;Barth;J. Geophys. Res. Oceans,2008

3. The HYCOM (HYbrid Coordinate Ocean Model) data assimilative system;Chassignet;J. Mar. Syst.,2007

4. Separation of an anticyclone and subsequent developments in the loop current (1969);Cochrane;Contrib. Phys, Oceanogr. Gulf Mexico,1972

5. Ensemble optimal interpolation: Multivariate properties in the Gulf of Mexico;Counillon;Tellus A,2009a

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