Ice-ocean interactions in Milne Fiord ...

Widespread break up of ice shelves, glacier tongues, and the loss of ice-dammed epishelf lakes on the northern coast of Ellesmere Island has motivated a need to understand fjord dynamics, yet the oceanography of fjords here is not well studied. Here, we present ocean profiling and mooring data colle...

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Main Author: Hamilton, Andrew Kent
Format: Text
Language:English
Published: University of British Columbia 2016
Subjects:
Online Access:https://dx.doi.org/10.14288/1.0314106
https://doi.library.ubc.ca/10.14288/1.0314106
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spelling ftdatacite:10.14288/1.0314106 2024-04-28T08:10:25+00:00 Ice-ocean interactions in Milne Fiord ... Hamilton, Andrew Kent 2016 https://dx.doi.org/10.14288/1.0314106 https://doi.library.ubc.ca/10.14288/1.0314106 en eng University of British Columbia article-journal Text ScholarlyArticle 2016 ftdatacite https://doi.org/10.14288/1.0314106 2024-04-02T09:28:50Z Widespread break up of ice shelves, glacier tongues, and the loss of ice-dammed epishelf lakes on the northern coast of Ellesmere Island has motivated a need to understand fjord dynamics, yet the oceanography of fjords here is not well studied. Here, we present ocean profiling and mooring data collected from 2011 to 2015 in Milne Fiord, the last ice shelf-epishelf lake-glacier tongue fjord in the Arctic. The data reveal that seasonal and interannual variations of fjord water properties and circulation are strongly impacted by the presence of the Milne Ice Shelf. The ice shelf forms a floating dam that traps surface runoff resulting in strong stratification and an elevated fjord heat content. Water exchange below the ice shelf is restricted to a narrow basal channel, prolonging the export of fjord-modified water, including subglacial runoff, by several months. In contrast, intermediate waters that penetrate to the Milne Glacier grounding line are freely exchanged and respond to offshore variations, with ... Text Arctic Ellesmere Island Ice Shelf Ice Shelves Milne Fiord Milne Ice Shelf DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description Widespread break up of ice shelves, glacier tongues, and the loss of ice-dammed epishelf lakes on the northern coast of Ellesmere Island has motivated a need to understand fjord dynamics, yet the oceanography of fjords here is not well studied. Here, we present ocean profiling and mooring data collected from 2011 to 2015 in Milne Fiord, the last ice shelf-epishelf lake-glacier tongue fjord in the Arctic. The data reveal that seasonal and interannual variations of fjord water properties and circulation are strongly impacted by the presence of the Milne Ice Shelf. The ice shelf forms a floating dam that traps surface runoff resulting in strong stratification and an elevated fjord heat content. Water exchange below the ice shelf is restricted to a narrow basal channel, prolonging the export of fjord-modified water, including subglacial runoff, by several months. In contrast, intermediate waters that penetrate to the Milne Glacier grounding line are freely exchanged and respond to offshore variations, with ...
format Text
author Hamilton, Andrew Kent
spellingShingle Hamilton, Andrew Kent
Ice-ocean interactions in Milne Fiord ...
author_facet Hamilton, Andrew Kent
author_sort Hamilton, Andrew Kent
title Ice-ocean interactions in Milne Fiord ...
title_short Ice-ocean interactions in Milne Fiord ...
title_full Ice-ocean interactions in Milne Fiord ...
title_fullStr Ice-ocean interactions in Milne Fiord ...
title_full_unstemmed Ice-ocean interactions in Milne Fiord ...
title_sort ice-ocean interactions in milne fiord ...
publisher University of British Columbia
publishDate 2016
url https://dx.doi.org/10.14288/1.0314106
https://doi.library.ubc.ca/10.14288/1.0314106
genre Arctic
Ellesmere Island
Ice Shelf
Ice Shelves
Milne Fiord
Milne Ice Shelf
genre_facet Arctic
Ellesmere Island
Ice Shelf
Ice Shelves
Milne Fiord
Milne Ice Shelf
op_doi https://doi.org/10.14288/1.0314106
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