Dissipation of turbulent kinetic energy inferred from Seagliders: an application to the eastern Nordic Seas overflows

Turbulent mixing is an important process controlling the descent rate, water mass modification, and volume transport augmentation due to entrainment in the dense overflows across the Greenland–Scotland Ridge. These overflows, along with entrained Atlantic waters, form a major portion of the North At...

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Bibliographic Details
Published in:Journal of Physical Oceanography
Main Authors: Beaird, Nicholas, Fer, Ilker, Rhines, Peter B., Eriksen, Charles
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2017
Subjects:
Online Access:https://hdl.handle.net/1956/16275
https://doi.org/10.1175/jpo-d-12-094.1