The turbulent oscillator : a mechanism of low-frequency variability of the wind-driven ocean gyres
Berloff, Pavel S.
Hogg, Andrew Mc C.
Dewar, William K.
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Intrinsic low-frequency variability is studied in the idealized, quasigeostrophic, midlatitude, wind-driven ocean gyres operating at large Reynolds number. A robust decadal variability mode driven by the transient mesoscale eddies is found and analyzed. The variability is a turbulent phenomenon, which is driven by the competition between the eddy rectification process and the potential vorticity anomalies induced by changes of the intergyre transport
Author Posting. © American Meteorological Society, 2007. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography. 37 (2007): 2363-2386, doi:10.1175/jpo3118.1.
Suggested CitationArticle: Berloff, Pavel S., Hogg, Andrew Mc C., Dewar, William K., "The turbulent oscillator : a mechanism of low-frequency variability of the wind-driven ocean gyres", Journal of Physical Oceanography 37 (2007): 2363-2386, DOI:10.1175/jpo3118.1, https://hdl.handle.net/1912/4155
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