Seasonally derived components of the Canada Basin halocline
Author(s)
Timmermans, Mary-Louise; Proshutinsky, Andrey; Marshall, John C; Scott, Jeremy
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The Arctic halocline stratification is an important barrier to the transport of deep ocean heat to the underside of sea ice. Surface water in the Chukchi Sea, warmed in summer by solar radiation, ventilates the Canada Basin halocline to create a warm layer below the mixed‐layer base. The year‐round persistence of this layer is shown to be consistent with the seasonal cycle of halocline ventilation. We present hydrographic observations and model results to show how Chukchi Sea density outcrops migrate seasonally as surface fluxes modify salinity and temperature. This migration is such that in winter, isopycnals bounding the warm halocline are blocked from ventilation, while the cool, relatively salty and deeper halocline layers are ventilated. In this way, the warm halocline is isolated by stratification (both vertically and laterally) each winter. Results shed light on the fate and impact to sea ice of the warm halocline under future freshening and warming of the surface Arctic Ocean.
Date issued
2017-04Department
Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary SciencesJournal
Geophysical Research Letters
Publisher
American Geophysical Union (AGU)
Citation
Timmermans, Mary-Louise, John Marshall, Andrey Proshutinsky, and Jeffery Scott. “Seasonally Derived Components of the Canada Basin Halocline.” Geophysical Research Letters 44, no. 10 (May 26, 2017): 5008–5015.
Version: Final published version
ISSN
0094-8276