Subglacial lake drainage detected beneath the Greenland ice sheet

Article Copyright © 2015, Rights Managed by Nature Publishing Group The contribution of the Greenland ice sheet to sea-level rise has accelerated in recent decades. Subglacial lake drainage events can induce an ice sheet dynamic response—a process that has been observed in Antarctica, but not yet in...

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Published in:Nature Communications
Main Authors: Palmer, SJ, McMillan, M, Morlighem, M
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group 2015
Subjects:
Online Access:http://hdl.handle.net/10871/18452
https://doi.org/10.1038/ncomms9408
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record_format openpolar
spelling ftunivexeter:oai:ore.exeter.ac.uk:10871/18452 2024-09-09T19:11:14+00:00 Subglacial lake drainage detected beneath the Greenland ice sheet Palmer, SJ McMillan, M Morlighem, M 2015 http://hdl.handle.net/10871/18452 https://doi.org/10.1038/ncomms9408 en eng Nature Publishing Group SETSM DEMs (http://www.pgc.umn.edu/elevation/stereo) were accessed from the Polar Geospatial centre at the University of Minnesota, and Greenland Ice Sheet Mapping Project data (http://bprc.osu.edu/GDG/gimpdem.php) were accessed from Byrd Polar Research Center at The Ohio State University. Landsat images were provided by the US Geological Survey and were accessed using Earth Explorer (http://earthexplorer.usgs.gov/). ICESat data (http://dx.doi.org/10.5067/ICESAT/GLAS/DATA126) and MEaSUREs ice flow data (http://dx.doi.org/10.5067/MEASURES/CRYOSPHERE/nsidc-0478.001) were accessed via the National Snow and Ice Data Centre. Nature Communications 6, Article number: 8408 doi:10.1038/ncomms9408 doi:10.1038/ncomms9408 NE/M000869/1 http://hdl.handle.net/10871/18452 2041-1723 Nature Communications This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/ Earth sciences Geology and geophysics Article 2015 ftunivexeter https://doi.org/10.1038/ncomms940810.5067/ICESAT/GLAS/DATA126 2024-07-29T03:24:15Z Article Copyright © 2015, Rights Managed by Nature Publishing Group The contribution of the Greenland ice sheet to sea-level rise has accelerated in recent decades. Subglacial lake drainage events can induce an ice sheet dynamic response—a process that has been observed in Antarctica, but not yet in Greenland, where the presence of subglacial lakes has only recently been discovered. Here we investigate the water flow paths from a subglacial lake, which drained beneath the Greenland ice sheet in 2011. Our observations suggest that the lake was fed by surface meltwater flowing down a nearby moulin, and that the draining water reached the ice margin via a subglacial tunnel. Interferometric synthetic aperture radar-derived measurements of ice surface motion acquired in 1995 suggest that a similar event may have occurred 16 years earlier, and we propose that, as the climate warms, increasing volumes of surface meltwater routed to the bed will cause such events to become more common in the future Natural Environment Research Council (NERC) Article in Journal/Newspaper Antarc* Antarctica Greenland Ice Sheet Polar Research University of Exeter: Open Research Exeter (ORE) Greenland Nature Communications 6 1
institution Open Polar
collection University of Exeter: Open Research Exeter (ORE)
op_collection_id ftunivexeter
language English
topic Earth sciences
Geology and geophysics
spellingShingle Earth sciences
Geology and geophysics
Palmer, SJ
McMillan, M
Morlighem, M
Subglacial lake drainage detected beneath the Greenland ice sheet
topic_facet Earth sciences
Geology and geophysics
description Article Copyright © 2015, Rights Managed by Nature Publishing Group The contribution of the Greenland ice sheet to sea-level rise has accelerated in recent decades. Subglacial lake drainage events can induce an ice sheet dynamic response—a process that has been observed in Antarctica, but not yet in Greenland, where the presence of subglacial lakes has only recently been discovered. Here we investigate the water flow paths from a subglacial lake, which drained beneath the Greenland ice sheet in 2011. Our observations suggest that the lake was fed by surface meltwater flowing down a nearby moulin, and that the draining water reached the ice margin via a subglacial tunnel. Interferometric synthetic aperture radar-derived measurements of ice surface motion acquired in 1995 suggest that a similar event may have occurred 16 years earlier, and we propose that, as the climate warms, increasing volumes of surface meltwater routed to the bed will cause such events to become more common in the future Natural Environment Research Council (NERC)
format Article in Journal/Newspaper
author Palmer, SJ
McMillan, M
Morlighem, M
author_facet Palmer, SJ
McMillan, M
Morlighem, M
author_sort Palmer, SJ
title Subglacial lake drainage detected beneath the Greenland ice sheet
title_short Subglacial lake drainage detected beneath the Greenland ice sheet
title_full Subglacial lake drainage detected beneath the Greenland ice sheet
title_fullStr Subglacial lake drainage detected beneath the Greenland ice sheet
title_full_unstemmed Subglacial lake drainage detected beneath the Greenland ice sheet
title_sort subglacial lake drainage detected beneath the greenland ice sheet
publisher Nature Publishing Group
publishDate 2015
url http://hdl.handle.net/10871/18452
https://doi.org/10.1038/ncomms9408
geographic Greenland
geographic_facet Greenland
genre Antarc*
Antarctica
Greenland
Ice Sheet
Polar Research
genre_facet Antarc*
Antarctica
Greenland
Ice Sheet
Polar Research
op_relation SETSM DEMs (http://www.pgc.umn.edu/elevation/stereo) were accessed from the Polar Geospatial centre at the University of Minnesota, and Greenland Ice Sheet Mapping Project data (http://bprc.osu.edu/GDG/gimpdem.php) were accessed from Byrd Polar Research Center at The Ohio State University. Landsat images were provided by the US Geological Survey and were accessed using Earth Explorer (http://earthexplorer.usgs.gov/). ICESat data (http://dx.doi.org/10.5067/ICESAT/GLAS/DATA126) and MEaSUREs ice flow data (http://dx.doi.org/10.5067/MEASURES/CRYOSPHERE/nsidc-0478.001) were accessed via the National Snow and Ice Data Centre.
Nature Communications 6, Article number: 8408 doi:10.1038/ncomms9408
doi:10.1038/ncomms9408
NE/M000869/1
http://hdl.handle.net/10871/18452
2041-1723
Nature Communications
op_rights This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1038/ncomms940810.5067/ICESAT/GLAS/DATA126
container_title Nature Communications
container_volume 6
container_issue 1
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