Quantifying flow regimes in a Greenland glacial fjord using iceberg drifters
Large, deep-keeled icebergs are ubiquitous in Greenland's outlet glacial fjords. Here we use the movement of these icebergs to quantify flow variability in Sermilik Fjord, southeast Greenland, from the ice mélange through the fjord to the shelf. In the ice mélange, a proglacial mixture of sea i...
Published in: | Geophysical Research Letters |
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American Geophysical Union (AGU)
2016
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Online Access: | http://hdl.handle.net/1808/22253 https://doi.org/10.1002/2014GL062256 |
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ftunivkansas:oai:kuscholarworks.ku.edu:1808/22253 2023-05-15T16:03:35+02:00 Quantifying flow regimes in a Greenland glacial fjord using iceberg drifters Sutherland, David A. Roth, George E. Hamilton, Gordon S. Mernild, Sebastian H. Stearns, Leigh A. Straneo, Fiammetta 2016-12-16T20:42:42Z http://hdl.handle.net/1808/22253 https://doi.org/10.1002/2014GL062256 unknown American Geophysical Union (AGU) Sutherland, D. A., G. E. Roth, G. S. Hamilton, S. H. Mernild, L. A. Stearns, and F. Straneo (2014), Quantifying flow regimes in a Greenland glacial fjord using iceberg drifters, Geophys. Res. Lett., 41, 8411–8420, doi:10.1002/2014GL062256. http://hdl.handle.net/1808/22253 doi:10.1002/2014GL062256 ©2014. American Geophysical Union. All Rights Reserved. openAccess Icebergs Fjord circulation Ice melange East Greenland Current Greenland ice sheet Iceberg melt Article 2016 ftunivkansas https://doi.org/10.1002/2014GL062256 2022-08-26T13:20:12Z Large, deep-keeled icebergs are ubiquitous in Greenland's outlet glacial fjords. Here we use the movement of these icebergs to quantify flow variability in Sermilik Fjord, southeast Greenland, from the ice mélange through the fjord to the shelf. In the ice mélange, a proglacial mixture of sea ice and icebergs, we find that icebergs consistently track the glacier speed, with slightly faster speeds near terminus and episodic increases due to calving events. In the fjord, icebergs accurately capture synoptic circulation driven by both along-fjord and along-shelf winds. Recirculation and in-/out-fjord variations occur throughout the fjord more frequently than previously reported, suggesting that across-fjord velocity gradients cannot be ignored. Once on the shelf, icebergs move southeastward in the East Greenland Coastal Current, providing wintertime observations of this freshwater pathway. Funded by The National Science Foundation. Grant Numbers: OCE-1130008, ARC-0909274 and The University of Oregon. Article in Journal/Newspaper East Greenland east greenland current glacier Greenland Ice Sheet Sea ice Sermilik The University of Kansas: KU ScholarWorks Greenland Geophysical Research Letters 41 23 8411 8420 |
institution |
Open Polar |
collection |
The University of Kansas: KU ScholarWorks |
op_collection_id |
ftunivkansas |
language |
unknown |
topic |
Icebergs Fjord circulation Ice melange East Greenland Current Greenland ice sheet Iceberg melt |
spellingShingle |
Icebergs Fjord circulation Ice melange East Greenland Current Greenland ice sheet Iceberg melt Sutherland, David A. Roth, George E. Hamilton, Gordon S. Mernild, Sebastian H. Stearns, Leigh A. Straneo, Fiammetta Quantifying flow regimes in a Greenland glacial fjord using iceberg drifters |
topic_facet |
Icebergs Fjord circulation Ice melange East Greenland Current Greenland ice sheet Iceberg melt |
description |
Large, deep-keeled icebergs are ubiquitous in Greenland's outlet glacial fjords. Here we use the movement of these icebergs to quantify flow variability in Sermilik Fjord, southeast Greenland, from the ice mélange through the fjord to the shelf. In the ice mélange, a proglacial mixture of sea ice and icebergs, we find that icebergs consistently track the glacier speed, with slightly faster speeds near terminus and episodic increases due to calving events. In the fjord, icebergs accurately capture synoptic circulation driven by both along-fjord and along-shelf winds. Recirculation and in-/out-fjord variations occur throughout the fjord more frequently than previously reported, suggesting that across-fjord velocity gradients cannot be ignored. Once on the shelf, icebergs move southeastward in the East Greenland Coastal Current, providing wintertime observations of this freshwater pathway. Funded by The National Science Foundation. Grant Numbers: OCE-1130008, ARC-0909274 and The University of Oregon. |
format |
Article in Journal/Newspaper |
author |
Sutherland, David A. Roth, George E. Hamilton, Gordon S. Mernild, Sebastian H. Stearns, Leigh A. Straneo, Fiammetta |
author_facet |
Sutherland, David A. Roth, George E. Hamilton, Gordon S. Mernild, Sebastian H. Stearns, Leigh A. Straneo, Fiammetta |
author_sort |
Sutherland, David A. |
title |
Quantifying flow regimes in a Greenland glacial fjord using iceberg drifters |
title_short |
Quantifying flow regimes in a Greenland glacial fjord using iceberg drifters |
title_full |
Quantifying flow regimes in a Greenland glacial fjord using iceberg drifters |
title_fullStr |
Quantifying flow regimes in a Greenland glacial fjord using iceberg drifters |
title_full_unstemmed |
Quantifying flow regimes in a Greenland glacial fjord using iceberg drifters |
title_sort |
quantifying flow regimes in a greenland glacial fjord using iceberg drifters |
publisher |
American Geophysical Union (AGU) |
publishDate |
2016 |
url |
http://hdl.handle.net/1808/22253 https://doi.org/10.1002/2014GL062256 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
East Greenland east greenland current glacier Greenland Ice Sheet Sea ice Sermilik |
genre_facet |
East Greenland east greenland current glacier Greenland Ice Sheet Sea ice Sermilik |
op_relation |
Sutherland, D. A., G. E. Roth, G. S. Hamilton, S. H. Mernild, L. A. Stearns, and F. Straneo (2014), Quantifying flow regimes in a Greenland glacial fjord using iceberg drifters, Geophys. Res. Lett., 41, 8411–8420, doi:10.1002/2014GL062256. http://hdl.handle.net/1808/22253 doi:10.1002/2014GL062256 |
op_rights |
©2014. American Geophysical Union. All Rights Reserved. openAccess |
op_doi |
https://doi.org/10.1002/2014GL062256 |
container_title |
Geophysical Research Letters |
container_volume |
41 |
container_issue |
23 |
container_start_page |
8411 |
op_container_end_page |
8420 |
_version_ |
1766399273859022848 |