Hydraulic suppression of basal glacier melt in sill fjords

Using a conceptual model, we examine how hydraulically controlled exchange flows in silled fjords affect the relationship between the basal glacier melt and the features of warm intermediate Atlantic Water (AW) outside the fjords. We show that an exchange flow can be forced to transit into the hydra...

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Published in:The Cryosphere
Main Authors: Nilsson, Johan, van Dongen, Eef, Jakobsson, Martin, O'Regan, Matt, Stranne, Christian
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-2455-2023
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spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00067248 2023-07-16T03:58:34+02:00 Hydraulic suppression of basal glacier melt in sill fjords Nilsson, Johan van Dongen, Eef Jakobsson, Martin O'Regan, Matt Stranne, Christian 2023-06 electronic https://doi.org/10.5194/tc-17-2455-2023 https://noa.gwlb.de/receive/cop_mods_00067248 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00065712/tc-17-2455-2023.pdf https://tc.copernicus.org/articles/17/2455/2023/tc-17-2455-2023.pdf eng eng Copernicus Publications The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-17-2455-2023 https://noa.gwlb.de/receive/cop_mods_00067248 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00065712/tc-17-2455-2023.pdf https://tc.copernicus.org/articles/17/2455/2023/tc-17-2455-2023.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2023 ftnonlinearchiv https://doi.org/10.5194/tc-17-2455-2023 2023-06-25T23:18:50Z Using a conceptual model, we examine how hydraulically controlled exchange flows in silled fjords affect the relationship between the basal glacier melt and the features of warm intermediate Atlantic Water (AW) outside the fjords. We show that an exchange flow can be forced to transit into the hydraulic regime if the AW interface height decreases, the AW temperature increases, or the production of glacially modified water is boosted by subglacial discharge. In the hydraulic regime, the heat transport across the sill becomes a rate-limiting factor for the basal melt, which is suppressed. An interplay between processes near the ice–ocean boundary and the hydraulically controlled exchange flow determines the melt dynamics, and the sensitivity of the basal melt to changes in the AW temperature is reduced. The model results are discussed in relation to observations from the Petermann, Ryder, and 79∘ N glaciers in northern Greenland. Article in Journal/Newspaper glacier Greenland The Cryosphere Niedersächsisches Online-Archiv NOA Greenland Ryder ENVELOPE(-68.333,-68.333,-67.566,-67.566) The Cryosphere 17 6 2455 2476
institution Open Polar
collection Niedersächsisches Online-Archiv NOA
op_collection_id ftnonlinearchiv
language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Nilsson, Johan
van Dongen, Eef
Jakobsson, Martin
O'Regan, Matt
Stranne, Christian
Hydraulic suppression of basal glacier melt in sill fjords
topic_facet article
Verlagsveröffentlichung
description Using a conceptual model, we examine how hydraulically controlled exchange flows in silled fjords affect the relationship between the basal glacier melt and the features of warm intermediate Atlantic Water (AW) outside the fjords. We show that an exchange flow can be forced to transit into the hydraulic regime if the AW interface height decreases, the AW temperature increases, or the production of glacially modified water is boosted by subglacial discharge. In the hydraulic regime, the heat transport across the sill becomes a rate-limiting factor for the basal melt, which is suppressed. An interplay between processes near the ice–ocean boundary and the hydraulically controlled exchange flow determines the melt dynamics, and the sensitivity of the basal melt to changes in the AW temperature is reduced. The model results are discussed in relation to observations from the Petermann, Ryder, and 79∘ N glaciers in northern Greenland.
format Article in Journal/Newspaper
author Nilsson, Johan
van Dongen, Eef
Jakobsson, Martin
O'Regan, Matt
Stranne, Christian
author_facet Nilsson, Johan
van Dongen, Eef
Jakobsson, Martin
O'Regan, Matt
Stranne, Christian
author_sort Nilsson, Johan
title Hydraulic suppression of basal glacier melt in sill fjords
title_short Hydraulic suppression of basal glacier melt in sill fjords
title_full Hydraulic suppression of basal glacier melt in sill fjords
title_fullStr Hydraulic suppression of basal glacier melt in sill fjords
title_full_unstemmed Hydraulic suppression of basal glacier melt in sill fjords
title_sort hydraulic suppression of basal glacier melt in sill fjords
publisher Copernicus Publications
publishDate 2023
url https://doi.org/10.5194/tc-17-2455-2023
https://noa.gwlb.de/receive/cop_mods_00067248
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00065712/tc-17-2455-2023.pdf
https://tc.copernicus.org/articles/17/2455/2023/tc-17-2455-2023.pdf
long_lat ENVELOPE(-68.333,-68.333,-67.566,-67.566)
geographic Greenland
Ryder
geographic_facet Greenland
Ryder
genre glacier
Greenland
The Cryosphere
genre_facet glacier
Greenland
The Cryosphere
op_relation The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424
https://doi.org/10.5194/tc-17-2455-2023
https://noa.gwlb.de/receive/cop_mods_00067248
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00065712/tc-17-2455-2023.pdf
https://tc.copernicus.org/articles/17/2455/2023/tc-17-2455-2023.pdf
op_rights https://creativecommons.org/licenses/by/4.0/
uneingeschränkt
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/tc-17-2455-2023
container_title The Cryosphere
container_volume 17
container_issue 6
container_start_page 2455
op_container_end_page 2476
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