Laboratory Experiments on the Interaction of a Buoyant Coastal Current with a Canyon: Application to the East Greenland Current

This paper presents a set of laboratory experiments focused on how a buoyant coastal current flowing over a sloping bottom interacts with a canyon and what controls the separation, if any, of the current from the upstream canyon bend. The results show that the separation of a buoyant coastal current...

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Published in:Journal of Physical Oceanography
Main Authors: Sutherland, David A., Cenedese, Claudia
Other Authors: Joint Program in Oceanography/Applied Ocean Science and Engineering, Woods Hole Oceanographic Institution
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2008
Subjects:
Online Access:http://hdl.handle.net/1721.1/65141
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spelling ftmit:oai:dspace.mit.edu:1721.1/65141 2023-06-11T04:09:42+02:00 Laboratory Experiments on the Interaction of a Buoyant Coastal Current with a Canyon: Application to the East Greenland Current Sutherland, David A. Cenedese, Claudia Joint Program in Oceanography/Applied Ocean Science and Engineering Woods Hole Oceanographic Institution Sutherland, David A. 2008-12 application/pdf http://hdl.handle.net/1721.1/65141 en_US eng American Meteorological Society http://dx.doi.org/10.1175/2008jpo4028.1 Journal of Physical Oceanography 0022-3670 1520-0485 http://hdl.handle.net/1721.1/65141 Sutherland, David A., and Claudia Cenedese. “Laboratory Experiments on the Interaction of a Buoyant Coastal Current with a Canyon: Application to the East Greenland Current.” Journal of Physical Oceanography 39.5 (2009) : 1258-1271. © 2011 American Meteorological Society. Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. American Meteorological Society Article http://purl.org/eprint/type/JournalArticle 2008 ftmit https://doi.org/10.1175/2008jpo4028.1 2023-05-29T08:19:09Z This paper presents a set of laboratory experiments focused on how a buoyant coastal current flowing over a sloping bottom interacts with a canyon and what controls the separation, if any, of the current from the upstream canyon bend. The results show that the separation of a buoyant coastal current depends on the current width W relative to the radius of curvature of the bathymetry ρc. The flow moved across the mouth of the canyon (i.e., separated) for W/ρc > 1, in agreement with previous results. The present study extends previous work by examining both slope-controlled and surface-trapped currents, and using a geometry specific to investigating buoyant current–canyon interaction. The authors find that, although bottom friction is important in setting the position of the buoyant front, the separation process driven by the inertia of the flow could overcome even the strongest bathymetric influence. Application of the laboratory results to the East Greenland Current (EGC), an Arctic-origin buoyant current that is observed to flow in two branches south of Denmark Strait, suggests that the path of the EGC is influenced by the large canyons cutting across the shelf, as the range of W/ρc in the ocean spans those observed in the laboratory. What causes the formation of a two-branched EGC structure downstream of the Kangerdlugssuaq Canyon (68°N, 32°W) is still unclear, but potential mechanisms are discussed. National Science Foundation (U.S.) (NSF Grant OCE-0450658) Woods Hole Oceanographic Institution National Science Foundation (U.S.) (NSF OCE-0350891) Article in Journal/Newspaper Arctic Denmark Strait East Greenland east greenland current Greenland DSpace@MIT (Massachusetts Institute of Technology) Arctic Greenland Journal of Physical Oceanography 39 5 1258 1271
institution Open Polar
collection DSpace@MIT (Massachusetts Institute of Technology)
op_collection_id ftmit
language English
description This paper presents a set of laboratory experiments focused on how a buoyant coastal current flowing over a sloping bottom interacts with a canyon and what controls the separation, if any, of the current from the upstream canyon bend. The results show that the separation of a buoyant coastal current depends on the current width W relative to the radius of curvature of the bathymetry ρc. The flow moved across the mouth of the canyon (i.e., separated) for W/ρc > 1, in agreement with previous results. The present study extends previous work by examining both slope-controlled and surface-trapped currents, and using a geometry specific to investigating buoyant current–canyon interaction. The authors find that, although bottom friction is important in setting the position of the buoyant front, the separation process driven by the inertia of the flow could overcome even the strongest bathymetric influence. Application of the laboratory results to the East Greenland Current (EGC), an Arctic-origin buoyant current that is observed to flow in two branches south of Denmark Strait, suggests that the path of the EGC is influenced by the large canyons cutting across the shelf, as the range of W/ρc in the ocean spans those observed in the laboratory. What causes the formation of a two-branched EGC structure downstream of the Kangerdlugssuaq Canyon (68°N, 32°W) is still unclear, but potential mechanisms are discussed. National Science Foundation (U.S.) (NSF Grant OCE-0450658) Woods Hole Oceanographic Institution National Science Foundation (U.S.) (NSF OCE-0350891)
author2 Joint Program in Oceanography/Applied Ocean Science and Engineering
Woods Hole Oceanographic Institution
Sutherland, David A.
format Article in Journal/Newspaper
author Sutherland, David A.
Cenedese, Claudia
spellingShingle Sutherland, David A.
Cenedese, Claudia
Laboratory Experiments on the Interaction of a Buoyant Coastal Current with a Canyon: Application to the East Greenland Current
author_facet Sutherland, David A.
Cenedese, Claudia
author_sort Sutherland, David A.
title Laboratory Experiments on the Interaction of a Buoyant Coastal Current with a Canyon: Application to the East Greenland Current
title_short Laboratory Experiments on the Interaction of a Buoyant Coastal Current with a Canyon: Application to the East Greenland Current
title_full Laboratory Experiments on the Interaction of a Buoyant Coastal Current with a Canyon: Application to the East Greenland Current
title_fullStr Laboratory Experiments on the Interaction of a Buoyant Coastal Current with a Canyon: Application to the East Greenland Current
title_full_unstemmed Laboratory Experiments on the Interaction of a Buoyant Coastal Current with a Canyon: Application to the East Greenland Current
title_sort laboratory experiments on the interaction of a buoyant coastal current with a canyon: application to the east greenland current
publisher American Meteorological Society
publishDate 2008
url http://hdl.handle.net/1721.1/65141
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
Denmark Strait
East Greenland
east greenland current
Greenland
genre_facet Arctic
Denmark Strait
East Greenland
east greenland current
Greenland
op_source American Meteorological Society
op_relation http://dx.doi.org/10.1175/2008jpo4028.1
Journal of Physical Oceanography
0022-3670
1520-0485
http://hdl.handle.net/1721.1/65141
Sutherland, David A., and Claudia Cenedese. “Laboratory Experiments on the Interaction of a Buoyant Coastal Current with a Canyon: Application to the East Greenland Current.” Journal of Physical Oceanography 39.5 (2009) : 1258-1271. © 2011 American Meteorological Society.
op_rights Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.
op_doi https://doi.org/10.1175/2008jpo4028.1
container_title Journal of Physical Oceanography
container_volume 39
container_issue 5
container_start_page 1258
op_container_end_page 1271
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