Numerical Modeling Shows Increased Fracturing Due to Melt-Undercutting Prior to Major Calving at Bowdoin Glacier

Projections of future ice sheet mass loss and thus sea level rise rely on the parametrization of iceberg calving in ice sheet models. The interconnection between submarine melt-induced undercutting and calving is still poorly understood, which makes predicted contributions of tidewater glaciers to s...

Full description

Bibliographic Details
Main Authors: van Dongen, Eef, Åström, Jan A., Jouvet, Guillaume, Todd, Joe, Benn, Douglas I., Funk, Martin
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media 2020
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/430415
https://doi.org/10.3929/ethz-b-000430415
id ftethz:oai:www.research-collection.ethz.ch:20.500.11850/430415
record_format openpolar
spelling ftethz:oai:www.research-collection.ethz.ch:20.500.11850/430415 2023-05-15T16:21:10+02:00 Numerical Modeling Shows Increased Fracturing Due to Melt-Undercutting Prior to Major Calving at Bowdoin Glacier van Dongen, Eef Åström, Jan A. Jouvet, Guillaume Todd, Joe Benn, Douglas I. Funk, Martin 2020 application/application/pdf https://hdl.handle.net/20.500.11850/430415 https://doi.org/10.3929/ethz-b-000430415 en eng Frontiers Media info:eu-repo/semantics/altIdentifier/doi/10.3389/feart.2020.00253 info:eu-repo/semantics/altIdentifier/wos/000556571000001 info:eu-repo/grantAgreement/SNF/Projektförderung in Mathematik, Natur- und Ingenieurwissenschaften (Abteilung II)/153179 http://hdl.handle.net/20.500.11850/430415 doi:10.3929/ethz-b-000430415 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International CC-BY Frontiers in Earth Science, 8 Glacier modeling Iceberg calving Numerical modeling Submarine melt Undercutting Crevasses Northwest Greenland info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2020 ftethz https://doi.org/20.500.11850/430415 https://doi.org/10.3929/ethz-b-000430415 https://doi.org/10.3389/feart.2020.00253 2022-04-25T14:17:23Z Projections of future ice sheet mass loss and thus sea level rise rely on the parametrization of iceberg calving in ice sheet models. The interconnection between submarine melt-induced undercutting and calving is still poorly understood, which makes predicted contributions of tidewater glaciers to sea level rise uncertain. Here, we compare detailed 3-D simulations of fracture initiation obtained with the Helsinki Discrete Element Model (HiDEM) to observations, prior to a major calving event at Bowdoin Glacier, Northwest Greenland. Observations of a plume surfacing at the calving location suggest that local melt-undercutting influenced the size of the major calving event. Therefore, several experiments are conducted with various local and distributed (front-wide) undercut geometries. Although the number of undercut experiments is limited by computational requirements, one of the conjectured undercut geometries reproduces the crevasse leading to the observed major calving event in great detail. Our simulations show that undercutting leads to initiation of wider fractures more than 100 m upstream of the terminus, well-beyond the directly undercut region. When combining a moderate distributed undercut with local amplified undercuts at the two observed plumes, fracture initiation also increases in between the local undercuts. Thus, our results agree with previous studies suggesting the existence of a “calving amplifier” effect by submarine melt, both upglacier and across-glacier. Consequently, the simulations show the potentially large impact of submarine melt-induced undercutting on iceberg size. ISSN:2296-6463 Article in Journal/Newspaper glacier Greenland Ice Sheet Tidewater ETH Zürich Research Collection Bowdoin ENVELOPE(-69.317,-69.317,77.683,77.683) Greenland
institution Open Polar
collection ETH Zürich Research Collection
op_collection_id ftethz
language English
topic Glacier modeling
Iceberg calving
Numerical modeling
Submarine melt
Undercutting
Crevasses
Northwest Greenland
spellingShingle Glacier modeling
Iceberg calving
Numerical modeling
Submarine melt
Undercutting
Crevasses
Northwest Greenland
van Dongen, Eef
Åström, Jan A.
Jouvet, Guillaume
Todd, Joe
Benn, Douglas I.
Funk, Martin
Numerical Modeling Shows Increased Fracturing Due to Melt-Undercutting Prior to Major Calving at Bowdoin Glacier
topic_facet Glacier modeling
Iceberg calving
Numerical modeling
Submarine melt
Undercutting
Crevasses
Northwest Greenland
description Projections of future ice sheet mass loss and thus sea level rise rely on the parametrization of iceberg calving in ice sheet models. The interconnection between submarine melt-induced undercutting and calving is still poorly understood, which makes predicted contributions of tidewater glaciers to sea level rise uncertain. Here, we compare detailed 3-D simulations of fracture initiation obtained with the Helsinki Discrete Element Model (HiDEM) to observations, prior to a major calving event at Bowdoin Glacier, Northwest Greenland. Observations of a plume surfacing at the calving location suggest that local melt-undercutting influenced the size of the major calving event. Therefore, several experiments are conducted with various local and distributed (front-wide) undercut geometries. Although the number of undercut experiments is limited by computational requirements, one of the conjectured undercut geometries reproduces the crevasse leading to the observed major calving event in great detail. Our simulations show that undercutting leads to initiation of wider fractures more than 100 m upstream of the terminus, well-beyond the directly undercut region. When combining a moderate distributed undercut with local amplified undercuts at the two observed plumes, fracture initiation also increases in between the local undercuts. Thus, our results agree with previous studies suggesting the existence of a “calving amplifier” effect by submarine melt, both upglacier and across-glacier. Consequently, the simulations show the potentially large impact of submarine melt-induced undercutting on iceberg size. ISSN:2296-6463
format Article in Journal/Newspaper
author van Dongen, Eef
Åström, Jan A.
Jouvet, Guillaume
Todd, Joe
Benn, Douglas I.
Funk, Martin
author_facet van Dongen, Eef
Åström, Jan A.
Jouvet, Guillaume
Todd, Joe
Benn, Douglas I.
Funk, Martin
author_sort van Dongen, Eef
title Numerical Modeling Shows Increased Fracturing Due to Melt-Undercutting Prior to Major Calving at Bowdoin Glacier
title_short Numerical Modeling Shows Increased Fracturing Due to Melt-Undercutting Prior to Major Calving at Bowdoin Glacier
title_full Numerical Modeling Shows Increased Fracturing Due to Melt-Undercutting Prior to Major Calving at Bowdoin Glacier
title_fullStr Numerical Modeling Shows Increased Fracturing Due to Melt-Undercutting Prior to Major Calving at Bowdoin Glacier
title_full_unstemmed Numerical Modeling Shows Increased Fracturing Due to Melt-Undercutting Prior to Major Calving at Bowdoin Glacier
title_sort numerical modeling shows increased fracturing due to melt-undercutting prior to major calving at bowdoin glacier
publisher Frontiers Media
publishDate 2020
url https://hdl.handle.net/20.500.11850/430415
https://doi.org/10.3929/ethz-b-000430415
long_lat ENVELOPE(-69.317,-69.317,77.683,77.683)
geographic Bowdoin
Greenland
geographic_facet Bowdoin
Greenland
genre glacier
Greenland
Ice Sheet
Tidewater
genre_facet glacier
Greenland
Ice Sheet
Tidewater
op_source Frontiers in Earth Science, 8
op_relation info:eu-repo/semantics/altIdentifier/doi/10.3389/feart.2020.00253
info:eu-repo/semantics/altIdentifier/wos/000556571000001
info:eu-repo/grantAgreement/SNF/Projektförderung in Mathematik, Natur- und Ingenieurwissenschaften (Abteilung II)/153179
http://hdl.handle.net/20.500.11850/430415
doi:10.3929/ethz-b-000430415
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International
op_rightsnorm CC-BY
op_doi https://doi.org/20.500.11850/430415
https://doi.org/10.3929/ethz-b-000430415
https://doi.org/10.3389/feart.2020.00253
_version_ 1766009183431294976