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...
Published in: | Journal of Physical Oceanography |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Meteorological Society
2017
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Subjects: | |
Online Access: | https://hdl.handle.net/1956/16275 https://doi.org/10.1175/jpo-d-12-094.1 |