Sea ice breakup and marine melt of a retreating tidewater outlet glacier in northeast Greenland (81°N)
Abstract Rising temperatures in the Arctic cause accelerated mass loss from the Greenland Ice Sheet and reduced sea ice cover. Tidewater outlet glaciers represent direct connections between glaciers and the ocean where melt rates at the ice-ocean interface are influenced by ocean temperature and cir...
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Online Access: | https://doi.org/10.1038/s41598-017-05089-3 https://doaj.org/article/47590520a4bb40d7a576d60fe250c65a |
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ftdoajarticles:oai:doaj.org/article:47590520a4bb40d7a576d60fe250c65a 2023-05-15T14:57:55+02:00 Sea ice breakup and marine melt of a retreating tidewater outlet glacier in northeast Greenland (81°N) Jørgen Bendtsen John Mortensen Kunuk Lennert Jens K. Ehn Wieter Boone Virginie Galindo Yu-bin Hu Igor A. Dmitrenko Sergei A. Kirillov Kristian K. Kjeldsen Yngve Kristoffersen David G. Barber Søren Rysgaard 2017-07-01T00:00:00Z https://doi.org/10.1038/s41598-017-05089-3 https://doaj.org/article/47590520a4bb40d7a576d60fe250c65a EN eng Nature Portfolio https://doi.org/10.1038/s41598-017-05089-3 https://doaj.org/toc/2045-2322 doi:10.1038/s41598-017-05089-3 2045-2322 https://doaj.org/article/47590520a4bb40d7a576d60fe250c65a Scientific Reports, Vol 7, Iss 1, Pp 1-11 (2017) Medicine R Science Q article 2017 ftdoajarticles https://doi.org/10.1038/s41598-017-05089-3 2022-12-31T05:24:13Z Abstract Rising temperatures in the Arctic cause accelerated mass loss from the Greenland Ice Sheet and reduced sea ice cover. Tidewater outlet glaciers represent direct connections between glaciers and the ocean where melt rates at the ice-ocean interface are influenced by ocean temperature and circulation. However, few measurements exist near outlet glaciers from the northern coast towards the Arctic Ocean that has remained nearly permanently ice covered. Here we present hydrographic measurements along the terminus of a major retreating tidewater outlet glacier from Flade Isblink Ice Cap. We show that the region is characterized by a relatively large change of the seasonal freshwater content, corresponding to ~2 m of freshwater, and that solar heating during the short open water period results in surface layer temperatures above 1 °C. Observations of temperature and salinity supported that the outlet glacier is a floating ice shelf with near-glacial subsurface temperatures at the freezing point. Melting from the surface layer significantly influenced the ice foot morphology of the glacier terminus. Hence, melting of the tidewater outlet glacier was found to be critically dependent on the retreat of sea ice adjacent to the terminus and the duration of open water. Article in Journal/Newspaper Arctic Arctic Ocean glacier Greenland Ice cap Ice Sheet Ice Shelf Sea ice Tidewater Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Flade Isblink ENVELOPE(-15.000,-15.000,81.583,81.583) Greenland Scientific Reports 7 1 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Medicine R Science Q |
spellingShingle |
Medicine R Science Q Jørgen Bendtsen John Mortensen Kunuk Lennert Jens K. Ehn Wieter Boone Virginie Galindo Yu-bin Hu Igor A. Dmitrenko Sergei A. Kirillov Kristian K. Kjeldsen Yngve Kristoffersen David G. Barber Søren Rysgaard Sea ice breakup and marine melt of a retreating tidewater outlet glacier in northeast Greenland (81°N) |
topic_facet |
Medicine R Science Q |
description |
Abstract Rising temperatures in the Arctic cause accelerated mass loss from the Greenland Ice Sheet and reduced sea ice cover. Tidewater outlet glaciers represent direct connections between glaciers and the ocean where melt rates at the ice-ocean interface are influenced by ocean temperature and circulation. However, few measurements exist near outlet glaciers from the northern coast towards the Arctic Ocean that has remained nearly permanently ice covered. Here we present hydrographic measurements along the terminus of a major retreating tidewater outlet glacier from Flade Isblink Ice Cap. We show that the region is characterized by a relatively large change of the seasonal freshwater content, corresponding to ~2 m of freshwater, and that solar heating during the short open water period results in surface layer temperatures above 1 °C. Observations of temperature and salinity supported that the outlet glacier is a floating ice shelf with near-glacial subsurface temperatures at the freezing point. Melting from the surface layer significantly influenced the ice foot morphology of the glacier terminus. Hence, melting of the tidewater outlet glacier was found to be critically dependent on the retreat of sea ice adjacent to the terminus and the duration of open water. |
format |
Article in Journal/Newspaper |
author |
Jørgen Bendtsen John Mortensen Kunuk Lennert Jens K. Ehn Wieter Boone Virginie Galindo Yu-bin Hu Igor A. Dmitrenko Sergei A. Kirillov Kristian K. Kjeldsen Yngve Kristoffersen David G. Barber Søren Rysgaard |
author_facet |
Jørgen Bendtsen John Mortensen Kunuk Lennert Jens K. Ehn Wieter Boone Virginie Galindo Yu-bin Hu Igor A. Dmitrenko Sergei A. Kirillov Kristian K. Kjeldsen Yngve Kristoffersen David G. Barber Søren Rysgaard |
author_sort |
Jørgen Bendtsen |
title |
Sea ice breakup and marine melt of a retreating tidewater outlet glacier in northeast Greenland (81°N) |
title_short |
Sea ice breakup and marine melt of a retreating tidewater outlet glacier in northeast Greenland (81°N) |
title_full |
Sea ice breakup and marine melt of a retreating tidewater outlet glacier in northeast Greenland (81°N) |
title_fullStr |
Sea ice breakup and marine melt of a retreating tidewater outlet glacier in northeast Greenland (81°N) |
title_full_unstemmed |
Sea ice breakup and marine melt of a retreating tidewater outlet glacier in northeast Greenland (81°N) |
title_sort |
sea ice breakup and marine melt of a retreating tidewater outlet glacier in northeast greenland (81°n) |
publisher |
Nature Portfolio |
publishDate |
2017 |
url |
https://doi.org/10.1038/s41598-017-05089-3 https://doaj.org/article/47590520a4bb40d7a576d60fe250c65a |
long_lat |
ENVELOPE(-15.000,-15.000,81.583,81.583) |
geographic |
Arctic Arctic Ocean Flade Isblink Greenland |
geographic_facet |
Arctic Arctic Ocean Flade Isblink Greenland |
genre |
Arctic Arctic Ocean glacier Greenland Ice cap Ice Sheet Ice Shelf Sea ice Tidewater |
genre_facet |
Arctic Arctic Ocean glacier Greenland Ice cap Ice Sheet Ice Shelf Sea ice Tidewater |
op_source |
Scientific Reports, Vol 7, Iss 1, Pp 1-11 (2017) |
op_relation |
https://doi.org/10.1038/s41598-017-05089-3 https://doaj.org/toc/2045-2322 doi:10.1038/s41598-017-05089-3 2045-2322 https://doaj.org/article/47590520a4bb40d7a576d60fe250c65a |
op_doi |
https://doi.org/10.1038/s41598-017-05089-3 |
container_title |
Scientific Reports |
container_volume |
7 |
container_issue |
1 |
_version_ |
1766330008905711616 |