Abstract
GEOPHYSICAL RESEARCH LETTERS,
VOL. 34,
L23613,
6 PP., 2007
doi:10.1029/2007GL031937
Barotropic Rossby wave radiation from a model Gulf Stream
Climate Research Division, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California, USA
Climate Research Division, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California, USA
School of Ocean and Earth Science Technology, University of Hawaii at Manoa, Honolulu, Hawaii, USA
Climate Research Division, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California, USA
Climate Research Division, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California, USA
Climate Research Division, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California, USA
Climate Research Division, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California, USA
Applied Physics Laboratory, University of Washington, Seattle, Washington, USA
Applied Physics Laboratory, University of Washington, Seattle, Washington, USA
Institute of Marine and Coastal Sciences, Rutgers University, New Brunswick, New Jersey, USA
Institute of Marine and Coastal Sciences, Rutgers University, New Brunswick, New Jersey, USA
Institute of Marine and Coastal Sciences, Rutgers University, New Brunswick, New Jersey, USA
The barotropic Rossby wave field in the North Atlantic Ocean is studied in an eddy-resolving ocean model simulation. The meandering model Gulf Stream radiates barotropic Rossby waves southward through preferred corridors defined by topographic features. The smoother region between the Bermuda Rise and the mid-Atlantic Ridge is a particularly striking corridor of barotropic wave radiation in the 20–50 day period band. Barotropic Rossby waves are also preferentially excited at higher frequencies over the Bermuda Rise, suggesting resonant excitation of topographic Rossby normal modes. The prevalence of these radiated waves suggests that they may be an important energy sink for the equilibrium state of the Gulf Stream.
Received 27 August 2007; accepted 29 October 2007; published 12 December 2007.
Citation: (2007), Barotropic Rossby wave radiation from a model Gulf Stream, Geophys. Res. Lett., 34, L23613, doi:10.1029/2007GL031937.
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