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Articles | Volume 11, issue 2
Articles | Volume 11, issue 2
https://doi.org/10.5194/os-11-287-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/os-11-287-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Articles | Volume 11, issue 2
Research article
 | 
27 Mar 2015
Research article |  | 27 Mar 2015

Tidal forcing, energetics, and mixing near the Yermak Plateau

I. Fer, M. Müller, and A. K. Peterson

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Cited articles

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Chapman, D. C.: Enhanced subinertial diurnal tides over isolated topographic features, Deep-Sea Res., 36, 815–824, 1989.
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Over the Yermak Plateau northwest of Svalbard there is substantial energy conversion from barotropic to internal tides. Internal tides are trapped along the topography. An approximate local conversion-to-dissipation balance is found over shallows and also in the deep part of the sloping flanks. Dissipation of tidal energy can be a significant contributor to turbulent mixing and cooling of the Atlantic layer in the Arctic Ocean.
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