Precursor of disintegration of Greenland's largest floating ice tongue

The largest floating tongue of Greenland’s ice sheet, Nioghalvfjerdsbræ, has been relatively stable with respect to areal retreat until 2022. Draining more than 6 % of the ice sheet, a disintegration of Nioghalvfjerdsbræ's floating tongue and subsequent acceleration due to loss in buttressing a...

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Published in:The Cryosphere
Main Authors: Humbert, Angelika, Helm, Veit, Neckel, Niklas, Zeising, Ole, Rückamp, Martin, Khan, Shfaqat Abbas, Loebel, Erik, Brauchle, Jörg, Stebner, Karsten, Gross, Dietmar, Sondershaus, Rabea, Müller, Ralf
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-2851-2023
https://tc.copernicus.org/articles/17/2851/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:tc106042 2023-07-30T04:04:12+02:00 Precursor of disintegration of Greenland's largest floating ice tongue Humbert, Angelika Helm, Veit Neckel, Niklas Zeising, Ole Rückamp, Martin Khan, Shfaqat Abbas Loebel, Erik Brauchle, Jörg Stebner, Karsten Gross, Dietmar Sondershaus, Rabea Müller, Ralf 2023-07-14 application/pdf https://doi.org/10.5194/tc-17-2851-2023 https://tc.copernicus.org/articles/17/2851/2023/ eng eng doi:10.5194/tc-17-2851-2023 https://tc.copernicus.org/articles/17/2851/2023/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-17-2851-2023 2023-07-17T16:24:17Z The largest floating tongue of Greenland’s ice sheet, Nioghalvfjerdsbræ, has been relatively stable with respect to areal retreat until 2022. Draining more than 6 % of the ice sheet, a disintegration of Nioghalvfjerdsbræ's floating tongue and subsequent acceleration due to loss in buttressing are likely to lead to sea level rise. Therefore, the stability of the floating tongue is a focus of this study. We employed a suite of observational methods to detect recent changes at the calving front. We found that the calving style has changed since 2016 at the southern part of the eastern calving front, from tongue-type calving to a crack evolution initiated at frontal ice rises reaching 5–7 km and progressing further upstream compared to 2010. The calving front area is further weakened by an area upstream of the main calving front that consists of open water and an ice mélange that has substantially expanded, leading to the formation of a narrow ice bridge. These geometric and mechanical changes may be a precursor of instability of the floating tongue. We complement our study by numerical ice flow simulations to estimate the impact of future ice-front retreat and complete ice shelf disintegration on the discharge of grounded ice. These idealized scenarios reveal that a loss of the south-eastern area of the ice shelf would lead to a 0.2 % increase in ice discharge at the grounding line, while a sudden collapse of the frontal area (46 % of the floating tongue area) will enhance the ice discharge by 5.1 % due to loss in buttressing. Eventually, a full collapse of the floating tongue increases the grounding line flux by 166 %. Text Ice Sheet Ice Shelf Copernicus Publications: E-Journals The Cryosphere 17 7 2851 2870
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The largest floating tongue of Greenland’s ice sheet, Nioghalvfjerdsbræ, has been relatively stable with respect to areal retreat until 2022. Draining more than 6 % of the ice sheet, a disintegration of Nioghalvfjerdsbræ's floating tongue and subsequent acceleration due to loss in buttressing are likely to lead to sea level rise. Therefore, the stability of the floating tongue is a focus of this study. We employed a suite of observational methods to detect recent changes at the calving front. We found that the calving style has changed since 2016 at the southern part of the eastern calving front, from tongue-type calving to a crack evolution initiated at frontal ice rises reaching 5–7 km and progressing further upstream compared to 2010. The calving front area is further weakened by an area upstream of the main calving front that consists of open water and an ice mélange that has substantially expanded, leading to the formation of a narrow ice bridge. These geometric and mechanical changes may be a precursor of instability of the floating tongue. We complement our study by numerical ice flow simulations to estimate the impact of future ice-front retreat and complete ice shelf disintegration on the discharge of grounded ice. These idealized scenarios reveal that a loss of the south-eastern area of the ice shelf would lead to a 0.2 % increase in ice discharge at the grounding line, while a sudden collapse of the frontal area (46 % of the floating tongue area) will enhance the ice discharge by 5.1 % due to loss in buttressing. Eventually, a full collapse of the floating tongue increases the grounding line flux by 166 %.
format Text
author Humbert, Angelika
Helm, Veit
Neckel, Niklas
Zeising, Ole
Rückamp, Martin
Khan, Shfaqat Abbas
Loebel, Erik
Brauchle, Jörg
Stebner, Karsten
Gross, Dietmar
Sondershaus, Rabea
Müller, Ralf
spellingShingle Humbert, Angelika
Helm, Veit
Neckel, Niklas
Zeising, Ole
Rückamp, Martin
Khan, Shfaqat Abbas
Loebel, Erik
Brauchle, Jörg
Stebner, Karsten
Gross, Dietmar
Sondershaus, Rabea
Müller, Ralf
Precursor of disintegration of Greenland's largest floating ice tongue
author_facet Humbert, Angelika
Helm, Veit
Neckel, Niklas
Zeising, Ole
Rückamp, Martin
Khan, Shfaqat Abbas
Loebel, Erik
Brauchle, Jörg
Stebner, Karsten
Gross, Dietmar
Sondershaus, Rabea
Müller, Ralf
author_sort Humbert, Angelika
title Precursor of disintegration of Greenland's largest floating ice tongue
title_short Precursor of disintegration of Greenland's largest floating ice tongue
title_full Precursor of disintegration of Greenland's largest floating ice tongue
title_fullStr Precursor of disintegration of Greenland's largest floating ice tongue
title_full_unstemmed Precursor of disintegration of Greenland's largest floating ice tongue
title_sort precursor of disintegration of greenland's largest floating ice tongue
publishDate 2023
url https://doi.org/10.5194/tc-17-2851-2023
https://tc.copernicus.org/articles/17/2851/2023/
genre Ice Sheet
Ice Shelf
genre_facet Ice Sheet
Ice Shelf
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-17-2851-2023
https://tc.copernicus.org/articles/17/2851/2023/
op_doi https://doi.org/10.5194/tc-17-2851-2023
container_title The Cryosphere
container_volume 17
container_issue 7
container_start_page 2851
op_container_end_page 2870
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