Impact of Fjord Geometry on Grounding Line Stability

Recent and past retreat of marine-terminating glaciers are broadly consistent with observed ocean warming, yet responses vary significantly within regions experiencing similar ocean conditions. We assess how fjord geometry modulates glacier response to a regional ocean warming on decadal to millenni...

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Published in:Frontiers in Earth Science
Main Authors: Åkesson, Henning, Nisancioglu, Kerim Hestnes, Nick, Faezeh M.
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers 2018
Subjects:
Online Access:https://hdl.handle.net/1956/18160
https://doi.org/10.3389/feart.2018.00071
id ftunivbergen:oai:bora.uib.no:1956/18160
record_format openpolar
spelling ftunivbergen:oai:bora.uib.no:1956/18160 2023-05-15T16:41:59+02:00 Impact of Fjord Geometry on Grounding Line Stability Åkesson, Henning Nisancioglu, Kerim Hestnes Nick, Faezeh M. 2018-06-05 application/pdf https://hdl.handle.net/1956/18160 https://doi.org/10.3389/feart.2018.00071 eng eng Frontiers Deglaciation of the Norwegian fjords urn:issn:2296-6463 https://hdl.handle.net/1956/18160 https://doi.org/10.3389/feart.2018.00071 cristin:1589149 Attribution CC BY http://creativecommons.org/licenses/by/4.0 Copyright 2018 The Author(s) 71 Frontiers in Earth Science 6 grounding lines Fjords marine-terminating glaciers calving numerical modeling ice shelves moraines ocean warming Peer reviewed Journal article 2018 ftunivbergen https://doi.org/10.3389/feart.2018.00071 2023-03-14T17:40:00Z Recent and past retreat of marine-terminating glaciers are broadly consistent with observed ocean warming, yet responses vary significantly within regions experiencing similar ocean conditions. We assess how fjord geometry modulates glacier response to a regional ocean warming on decadal to millennial time scales, by using an idealized, numerical model of fast-flowing glaciers including a crevasse-depth calving criterion. Our simulations show that, given identical climate forcing, grounding line responses can differ by tens of kilometers due to variations in channel width. We identify fjord mouths and embayments as vulnerable geometries, showing that glaciers in these fjords are prone to rapid, irreversible retreat, independent of the presence of a fjord sill. This irreversible retreat has relevance for the potential future recovery of marine ice sheets, if the current anthropogenic warming is reduced, or reversed, as well as for the response of marine ice sheets to past climate states; including the warm Bølling-Allerød interstadial, the Younger Dryas cold reversal and the Little Ice Age. publishedVersion Article in Journal/Newspaper Ice Shelves University of Bergen: Bergen Open Research Archive (BORA-UiB) Frontiers in Earth Science 6
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
topic grounding lines
Fjords
marine-terminating glaciers
calving
numerical modeling
ice shelves
moraines
ocean warming
spellingShingle grounding lines
Fjords
marine-terminating glaciers
calving
numerical modeling
ice shelves
moraines
ocean warming
Åkesson, Henning
Nisancioglu, Kerim Hestnes
Nick, Faezeh M.
Impact of Fjord Geometry on Grounding Line Stability
topic_facet grounding lines
Fjords
marine-terminating glaciers
calving
numerical modeling
ice shelves
moraines
ocean warming
description Recent and past retreat of marine-terminating glaciers are broadly consistent with observed ocean warming, yet responses vary significantly within regions experiencing similar ocean conditions. We assess how fjord geometry modulates glacier response to a regional ocean warming on decadal to millennial time scales, by using an idealized, numerical model of fast-flowing glaciers including a crevasse-depth calving criterion. Our simulations show that, given identical climate forcing, grounding line responses can differ by tens of kilometers due to variations in channel width. We identify fjord mouths and embayments as vulnerable geometries, showing that glaciers in these fjords are prone to rapid, irreversible retreat, independent of the presence of a fjord sill. This irreversible retreat has relevance for the potential future recovery of marine ice sheets, if the current anthropogenic warming is reduced, or reversed, as well as for the response of marine ice sheets to past climate states; including the warm Bølling-Allerød interstadial, the Younger Dryas cold reversal and the Little Ice Age. publishedVersion
format Article in Journal/Newspaper
author Åkesson, Henning
Nisancioglu, Kerim Hestnes
Nick, Faezeh M.
author_facet Åkesson, Henning
Nisancioglu, Kerim Hestnes
Nick, Faezeh M.
author_sort Åkesson, Henning
title Impact of Fjord Geometry on Grounding Line Stability
title_short Impact of Fjord Geometry on Grounding Line Stability
title_full Impact of Fjord Geometry on Grounding Line Stability
title_fullStr Impact of Fjord Geometry on Grounding Line Stability
title_full_unstemmed Impact of Fjord Geometry on Grounding Line Stability
title_sort impact of fjord geometry on grounding line stability
publisher Frontiers
publishDate 2018
url https://hdl.handle.net/1956/18160
https://doi.org/10.3389/feart.2018.00071
genre Ice Shelves
genre_facet Ice Shelves
op_source 71
Frontiers in Earth Science
6
op_relation Deglaciation of the Norwegian fjords
urn:issn:2296-6463
https://hdl.handle.net/1956/18160
https://doi.org/10.3389/feart.2018.00071
cristin:1589149
op_rights Attribution CC BY
http://creativecommons.org/licenses/by/4.0
Copyright 2018 The Author(s)
op_doi https://doi.org/10.3389/feart.2018.00071
container_title Frontiers in Earth Science
container_volume 6
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