The East Greenland Coastal Current : its structure, variability, and large-scale impact

Thesis (Ph. D.)--Joint Program in Oceanography/Applied Ocean Science and Engineering (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 2008.

Bibliographic Details
Main Author: Sutherland, David A. (David Alan)
Other Authors: Robert S. Pickart.
Format: Thesis
Language:eng
Published: Massachusetts Institute of Technology 2008
Subjects:
Online Access:http://hdl.handle.net/1721.1/43156
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author Sutherland, David A. (David Alan)
author2 Robert S. Pickart.
author_facet Robert S. Pickart.
Sutherland, David A. (David Alan)
author_sort Sutherland, David A. (David Alan)
collection MIT
description Thesis (Ph. D.)--Joint Program in Oceanography/Applied Ocean Science and Engineering (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 2008.
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spelling mit-1721.1/431562022-01-14T19:08:21Z The East Greenland Coastal Current : its structure, variability, and large-scale impact EGCC : its structure, variability, and large-scale impact Sutherland, David A. (David Alan) Robert S. Pickart. Woods Hole Oceanographic Institution. Joint Program in Oceanography/Applied Ocean Science and Engineering Woods Hole Oceanographic Institution Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Earth, Atmospheric, and Planetary Sciences. /Woods Hole Oceanographic Institution. Joint Program in Oceanography/Applied Ocean Science and Engineering. Woods Hole Oceanographic Institution. Ocean currents Oceanography Thesis (Ph. D.)--Joint Program in Oceanography/Applied Ocean Science and Engineering (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 2008. Includes bibliographical references (p. 155-161). The subtidal circulation of the southeast Greenland shelf is described using a set of high resolution hydrographic and velocity transects occupied in summer 2004. The main feature present is the East Greenland Coastal Current (EGCC), a low-salinity, high velocity jet with a wedge-shaped hydrographic structure characteristic of other surface buoyancy-driven currents. The EGCC was observed along the entire Greenland shelf south of Denmark Strait, while the transect north of the strait showed only a weak shelf flow. This observation, combined with evidence from chemical tracer measurements that imply the EGCC contains a significant Pacific Water signal, suggests that the EGCC is an inner branch of the polar-origin East Greenland Current (EGC). A set of idealized laboratory experiments on the interaction of a buoyant current with a submarine canyon also supported this hypothesis, showing that for the observed range of oceanic parameters, a buoyant current such as the EGC could exhibit both flow across the canyon mouth or into the canyon itself, setting the stage for EGCC formation. Repeat sections occupied at Cape Farewell between 1997 and 2004 show that the along shelf wind stress can also have a strong influence on the structure and strength of the EGCC and EGC on timescales of 2-3 days. Accounting for the wind-induced effects, the volume transport of the combined EGC/EGCC system is found to be roughly constant (-2 Sv) over the study domain, from 68*N to Cape Farewell near 60°N. The corresponding freshwater transport increases by roughly 60% over this distance (59 to 96 mSv, referenced to a salinity of 34.8). This trend is explained by constructing a simple freshwater budget of the EGCC/EGC system that accounts for melt water runoff, melting sea-ice and icebergs, and net precipitation minus evaporation. (cont.) Variability on inter annual timescales is examined by calculating the Pacific Water content in the EGC/EGCC from 1984-2004 in the vicinity of Denmark Strait. The PW content is found to correlate significantly with the Arctic Oscillation index, lagged by 9 years, suggesting that the Arctic Ocean circulation patterns bring varying amounts of Pacific Water to the North Atlantic via the EGC/EGCC. by David A. Sutherland. Ph.D. 2008-11-07T19:09:54Z 2008-11-07T19:09:54Z 2008 2008 Thesis http://hdl.handle.net/1721.1/43156 248618134 eng M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission. http://dspace.mit.edu/handle/1721.1/7582 161 p. application/pdf n-gl--- Massachusetts Institute of Technology
spellingShingle Earth, Atmospheric, and Planetary Sciences.
/Woods Hole Oceanographic Institution. Joint Program in Oceanography/Applied Ocean Science and Engineering.
Woods Hole Oceanographic Institution.
Ocean currents
Oceanography
Sutherland, David A. (David Alan)
The East Greenland Coastal Current : its structure, variability, and large-scale impact
title The East Greenland Coastal Current : its structure, variability, and large-scale impact
title_full The East Greenland Coastal Current : its structure, variability, and large-scale impact
title_fullStr The East Greenland Coastal Current : its structure, variability, and large-scale impact
title_full_unstemmed The East Greenland Coastal Current : its structure, variability, and large-scale impact
title_short The East Greenland Coastal Current : its structure, variability, and large-scale impact
title_sort east greenland coastal current its structure variability and large scale impact
topic Earth, Atmospheric, and Planetary Sciences.
/Woods Hole Oceanographic Institution. Joint Program in Oceanography/Applied Ocean Science and Engineering.
Woods Hole Oceanographic Institution.
Ocean currents
Oceanography
url http://hdl.handle.net/1721.1/43156
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