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Turbulent kinetic energy dissipation in Barrow Canyon

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dc.contributor.author Shroyer, Emily L.
dc.date.accessioned 2012-07-24T16:37:29Z
dc.date.available 2012-12-01T09:43:16Z
dc.date.issued 2012-06
dc.identifier.citation Journal of Physical Oceanography 42 (2012): 1012–1021 en_US
dc.identifier.uri http://hdl.handle.net/1912/5274
dc.description Author Posting. © American Meteorological Society, 2012. 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 42 (2012): 1012–1021, doi:10.1175/JPO-D-11-0184.1. en_US
dc.description.abstract Pacific Water flows across the shallow Chukchi Sea before reaching the Arctic Ocean, where it is a source of heat, freshwater, nutrients, and carbon. A substantial portion of Pacific Water is routed through Barrow Canyon, located in the northeast corner of the Chukchi. Barrow Canyon is a region of complex geometry and forcing where a variety of water masses have been observed to coexist. These factors contribute to a dynamic physical environment, with the potential for significant water mass transformation. The measurements of turbulent kinetic energy dissipation presented here indicate diapycnal mixing is important in the upper canyon. Elevated dissipation rates were observed near the pycnocline, effectively mixing winter and summer water masses, as well as within the bottom boundary layer. The slopes of shear/stratification layers, combined with analysis of rotary spectra, suggest that near-inertial wave activity may be important in modulating dissipation near the bottom. Because the canyon is known to be a hotspot of productivity with an active benthic community, mixing may be an important factor in maintenance of the biological environment. en_US
dc.description.sponsorship ELS was supported as a WHOI Postdoctoral Scholar through the WHOI Ocean and Climate Change Institute. 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/JPO-D-11-0184.1
dc.subject Arctic en_US
dc.subject Continental shelf/slope en_US
dc.subject Mixing en_US
dc.subject Small scale processes en_US
dc.title Turbulent kinetic energy dissipation in Barrow Canyon en_US
dc.type Article en_US
dc.description.embargo 2012-12-01 en_US
dc.identifier.doi 10.1175/JPO-D-11-0184.1


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