Characteristics of meltwater export from Jakobshavn Isbræ and Ilulissat Icefjord
Jakobshavn Isbræ, which terminates in Ilulissat Icefjord, has undergone rapid retreat and is currently the largest contributor to ice-sheet mass loss among Greenland's marine terminating glaciers. Accelerating mass loss is increasing fresh water discharge to the ocean, which can feed back on ic...
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Cambridge University Press
2017
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ftdoajarticles:oai:doaj.org/article:236d3413e1724d7fb0cb67f3de2d7aca 2023-05-15T13:29:32+02:00 Characteristics of meltwater export from Jakobshavn Isbræ and Ilulissat Icefjord Nicholas Beaird Fiammetta Straneo William Jenkins 2017-04-01T00:00:00Z https://doi.org/10.1017/aog.2017.19 https://doaj.org/article/236d3413e1724d7fb0cb67f3de2d7aca EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0260305517000192/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2017.19 0260-3055 1727-5644 https://doaj.org/article/236d3413e1724d7fb0cb67f3de2d7aca Annals of Glaciology, Vol 58, Pp 107-117 (2017) glacier discharge icebergs ice/ocean interactions meltwater chemistry polar and subpolar oceans Meteorology. Climatology QC851-999 article 2017 ftdoajarticles https://doi.org/10.1017/aog.2017.19 2023-03-12T01:31:57Z Jakobshavn Isbræ, which terminates in Ilulissat Icefjord, has undergone rapid retreat and is currently the largest contributor to ice-sheet mass loss among Greenland's marine terminating glaciers. Accelerating mass loss is increasing fresh water discharge to the ocean, which can feed back on ice melt, impact marine ecosystems and potentially modify regional and larger scale ocean circulation. Here we present hydrographic observations, including inert geochemical tracers, that allow the first quantitative description of the glacially-modified waters exported from the Jakobshavn/Icefjord system. Observations within the fjord suggest a deep-reaching overturning cell driven by glacial buoyancy forcing. Modified waters containing submarine meltwater (up to 2.5 ± 0.12%), subglacial discharge (up to 6 ± 0.37%) and large portions of entrained ocean waters are seen to exit the fjord and flow north. The exported meltwaters form a buoyant coastal gravity current reaching to 100 m depth and extending 10 km offshore. Article in Journal/Newspaper Annals of Glaciology Ice Sheet Ilulissat Jakobshavn Jakobshavn isbræ Directory of Open Access Journals: DOAJ Articles Ilulissat ENVELOPE(-51.099,-51.099,69.220,69.220) Jakobshavn Isbræ ENVELOPE(-49.917,-49.917,69.167,69.167) Annals of Glaciology 58 74 107 117 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
glacier discharge icebergs ice/ocean interactions meltwater chemistry polar and subpolar oceans Meteorology. Climatology QC851-999 |
spellingShingle |
glacier discharge icebergs ice/ocean interactions meltwater chemistry polar and subpolar oceans Meteorology. Climatology QC851-999 Nicholas Beaird Fiammetta Straneo William Jenkins Characteristics of meltwater export from Jakobshavn Isbræ and Ilulissat Icefjord |
topic_facet |
glacier discharge icebergs ice/ocean interactions meltwater chemistry polar and subpolar oceans Meteorology. Climatology QC851-999 |
description |
Jakobshavn Isbræ, which terminates in Ilulissat Icefjord, has undergone rapid retreat and is currently the largest contributor to ice-sheet mass loss among Greenland's marine terminating glaciers. Accelerating mass loss is increasing fresh water discharge to the ocean, which can feed back on ice melt, impact marine ecosystems and potentially modify regional and larger scale ocean circulation. Here we present hydrographic observations, including inert geochemical tracers, that allow the first quantitative description of the glacially-modified waters exported from the Jakobshavn/Icefjord system. Observations within the fjord suggest a deep-reaching overturning cell driven by glacial buoyancy forcing. Modified waters containing submarine meltwater (up to 2.5 ± 0.12%), subglacial discharge (up to 6 ± 0.37%) and large portions of entrained ocean waters are seen to exit the fjord and flow north. The exported meltwaters form a buoyant coastal gravity current reaching to 100 m depth and extending 10 km offshore. |
format |
Article in Journal/Newspaper |
author |
Nicholas Beaird Fiammetta Straneo William Jenkins |
author_facet |
Nicholas Beaird Fiammetta Straneo William Jenkins |
author_sort |
Nicholas Beaird |
title |
Characteristics of meltwater export from Jakobshavn Isbræ and Ilulissat Icefjord |
title_short |
Characteristics of meltwater export from Jakobshavn Isbræ and Ilulissat Icefjord |
title_full |
Characteristics of meltwater export from Jakobshavn Isbræ and Ilulissat Icefjord |
title_fullStr |
Characteristics of meltwater export from Jakobshavn Isbræ and Ilulissat Icefjord |
title_full_unstemmed |
Characteristics of meltwater export from Jakobshavn Isbræ and Ilulissat Icefjord |
title_sort |
characteristics of meltwater export from jakobshavn isbræ and ilulissat icefjord |
publisher |
Cambridge University Press |
publishDate |
2017 |
url |
https://doi.org/10.1017/aog.2017.19 https://doaj.org/article/236d3413e1724d7fb0cb67f3de2d7aca |
long_lat |
ENVELOPE(-51.099,-51.099,69.220,69.220) ENVELOPE(-49.917,-49.917,69.167,69.167) |
geographic |
Ilulissat Jakobshavn Isbræ |
geographic_facet |
Ilulissat Jakobshavn Isbræ |
genre |
Annals of Glaciology Ice Sheet Ilulissat Jakobshavn Jakobshavn isbræ |
genre_facet |
Annals of Glaciology Ice Sheet Ilulissat Jakobshavn Jakobshavn isbræ |
op_source |
Annals of Glaciology, Vol 58, Pp 107-117 (2017) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0260305517000192/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2017.19 0260-3055 1727-5644 https://doaj.org/article/236d3413e1724d7fb0cb67f3de2d7aca |
op_doi |
https://doi.org/10.1017/aog.2017.19 |
container_title |
Annals of Glaciology |
container_volume |
58 |
container_issue |
74 |
container_start_page |
107 |
op_container_end_page |
117 |
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1766001138624102400 |