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Mesoscale eddy–internal wave coupling. Part II : energetics and results from PolyMode

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dc.contributor.author Polzin, Kurt L.
dc.date.accessioned 2010-10-19T15:46:07Z
dc.date.available 2010-10-19T15:46:07Z
dc.date.issued 2010-04
dc.identifier.citation Journal of Physical Oceanography 40 (2010): 789-801 en_US
dc.identifier.uri http://hdl.handle.net/1912/3955
dc.description Author Posting. © American Meteorological Society, 2010. 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 40 (2010): 789-801, doi:10.1175/2009JPO4039.1. en_US
dc.description.abstract The issue of internal wave–mesoscale eddy interactions is revisited. Previous observational work identified the mesoscale eddy field as a possible source of internal wave energy. Characterization of the coupling as a viscous process provides a smaller horizontal transfer coefficient than previously obtained, with vh 50 m2 s−1 in contrast to νh 200–400 m2 s−1, and a vertical transfer coefficient bounded away from zero, with νυ + (f2/N2)Kh 2.5 ± 0.3 × 10−3 m2 s−1 in contrast to νυ + (f2/N2)Kh = 0 ± 2 × 10−2 m2 s−1. Current meter data from the Local Dynamics Experiment of the PolyMode field program indicate mesoscale eddy–internal wave coupling through horizontal interactions (i) is a significant sink of eddy energy and (ii) plays an O(1) role in the energy budget of the internal wave field. en_US
dc.format.mimetype application/pdf
dc.language.iso en_US en_US
dc.publisher American Meteorological Society en_US
dc.relation.uri http://dx.doi.org/10.1175/2009JPO4039.1
dc.subject Eddies en_US
dc.subject Internal waves en_US
dc.subject Mesoscale processes en_US
dc.title Mesoscale eddy–internal wave coupling. Part II : energetics and results from PolyMode en_US
dc.type Article en_US
dc.identifier.doi 10.1175/2009JPO4039.1


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