Subglacial lake drainage detected beneath the Greenland ice sheet
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...
Published in: | Nature Communications |
---|---|
Main Authors: | , , |
Format: | Text |
Language: | English |
Published: |
Nature Pub. Group
2015
|
Subjects: | |
Online Access: | http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4633647/ http://www.ncbi.nlm.nih.gov/pubmed/26450175 https://doi.org/10.1038/ncomms9408 |
id |
ftpubmed:oai:pubmedcentral.nih.gov:4633647 |
---|---|
record_format |
openpolar |
spelling |
ftpubmed:oai:pubmedcentral.nih.gov:4633647 2023-05-15T14:03:57+02:00 Subglacial lake drainage detected beneath the Greenland ice sheet Palmer, Steven McMillan, Malcolm Morlighem, Mathieu 2015-10-09 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4633647/ http://www.ncbi.nlm.nih.gov/pubmed/26450175 https://doi.org/10.1038/ncomms9408 en eng Nature Pub. Group http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4633647/ http://www.ncbi.nlm.nih.gov/pubmed/26450175 http://dx.doi.org/10.1038/ncomms9408 Copyright © 2015, Nature Publishing Group, a division of Macmillan Publishers Limited. All Rights Reserved. http://creativecommons.org/licenses/by/4.0/ 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/ CC-BY Article Text 2015 ftpubmed https://doi.org/10.1038/ncomms9408 2015-11-29T01:23:42Z 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. Text Antarc* Antarctica Greenland Ice Sheet PubMed Central (PMC) Greenland Nature Communications 6 1 |
institution |
Open Polar |
collection |
PubMed Central (PMC) |
op_collection_id |
ftpubmed |
language |
English |
topic |
Article |
spellingShingle |
Article Palmer, Steven McMillan, Malcolm Morlighem, Mathieu Subglacial lake drainage detected beneath the Greenland ice sheet |
topic_facet |
Article |
description |
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. |
format |
Text |
author |
Palmer, Steven McMillan, Malcolm Morlighem, Mathieu |
author_facet |
Palmer, Steven McMillan, Malcolm Morlighem, Mathieu |
author_sort |
Palmer, Steven |
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 Pub. Group |
publishDate |
2015 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4633647/ http://www.ncbi.nlm.nih.gov/pubmed/26450175 https://doi.org/10.1038/ncomms9408 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Antarc* Antarctica Greenland Ice Sheet |
genre_facet |
Antarc* Antarctica Greenland Ice Sheet |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4633647/ http://www.ncbi.nlm.nih.gov/pubmed/26450175 http://dx.doi.org/10.1038/ncomms9408 |
op_rights |
Copyright © 2015, Nature Publishing Group, a division of Macmillan Publishers Limited. All Rights Reserved. http://creativecommons.org/licenses/by/4.0/ 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_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1038/ncomms9408 |
container_title |
Nature Communications |
container_volume |
6 |
container_issue |
1 |
_version_ |
1766274858573889536 |