Calving on tidewater glaciers amplified by submarine frontal melting ...

While it has been shown repeatedly that ocean conditions exhibit an important control on the behaviour of grounded tidewater glaciers, modelling studies have focused largely on the effects of basal and surface melting. Here, a finite-element model of stresses near the front of a tidewater glacier is...

Full description

Bibliographic Details
Main Authors: O'Leary, Martin, Christoffersen, Poul
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2019
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.45338
https://www.repository.cam.ac.uk/handle/1810/298283
id ftdatacite:10.17863/cam.45338
record_format openpolar
spelling ftdatacite:10.17863/cam.45338 2024-02-04T09:55:34+01:00 Calving on tidewater glaciers amplified by submarine frontal melting ... O'Leary, Martin Christoffersen, Poul 2019 https://dx.doi.org/10.17863/cam.45338 https://www.repository.cam.ac.uk/handle/1810/298283 en eng Copernicus Publications open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 Article ScholarlyArticle JournalArticle article-journal 2019 ftdatacite https://doi.org/10.17863/cam.45338 2024-01-05T09:50:49Z While it has been shown repeatedly that ocean conditions exhibit an important control on the behaviour of grounded tidewater glaciers, modelling studies have focused largely on the effects of basal and surface melting. Here, a finite-element model of stresses near the front of a tidewater glacier is used to investigate the effects of frontal melting on calving, independently of the calving criterion used. Applications of the stress model to idealized scenarios reveal that undercutting of the ice front due to frontal melting can drive calving at up to ten times the mean melt rate. Factors which cause increased frontal melt-driven calving include a strong thermal gradient in the ice, and a concentration of frontal melt at the base of the glacier. These properties are typical of both Arctic and Antarctic tidewater glaciers. The finding that frontal melt near the base is a strong driver of calving leads to the conclusion that water temperatures near the bed of the glacier are critically important to the glacier ... Article in Journal/Newspaper Antarc* Antarctic Arctic Tidewater DataCite Metadata Store (German National Library of Science and Technology) Antarctic Arctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description While it has been shown repeatedly that ocean conditions exhibit an important control on the behaviour of grounded tidewater glaciers, modelling studies have focused largely on the effects of basal and surface melting. Here, a finite-element model of stresses near the front of a tidewater glacier is used to investigate the effects of frontal melting on calving, independently of the calving criterion used. Applications of the stress model to idealized scenarios reveal that undercutting of the ice front due to frontal melting can drive calving at up to ten times the mean melt rate. Factors which cause increased frontal melt-driven calving include a strong thermal gradient in the ice, and a concentration of frontal melt at the base of the glacier. These properties are typical of both Arctic and Antarctic tidewater glaciers. The finding that frontal melt near the base is a strong driver of calving leads to the conclusion that water temperatures near the bed of the glacier are critically important to the glacier ...
format Article in Journal/Newspaper
author O'Leary, Martin
Christoffersen, Poul
spellingShingle O'Leary, Martin
Christoffersen, Poul
Calving on tidewater glaciers amplified by submarine frontal melting ...
author_facet O'Leary, Martin
Christoffersen, Poul
author_sort O'Leary, Martin
title Calving on tidewater glaciers amplified by submarine frontal melting ...
title_short Calving on tidewater glaciers amplified by submarine frontal melting ...
title_full Calving on tidewater glaciers amplified by submarine frontal melting ...
title_fullStr Calving on tidewater glaciers amplified by submarine frontal melting ...
title_full_unstemmed Calving on tidewater glaciers amplified by submarine frontal melting ...
title_sort calving on tidewater glaciers amplified by submarine frontal melting ...
publisher Copernicus Publications
publishDate 2019
url https://dx.doi.org/10.17863/cam.45338
https://www.repository.cam.ac.uk/handle/1810/298283
geographic Antarctic
Arctic
geographic_facet Antarctic
Arctic
genre Antarc*
Antarctic
Arctic
Tidewater
genre_facet Antarc*
Antarctic
Arctic
Tidewater
op_rights open.access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
http://purl.org/coar/access_right/c_abf2
op_doi https://doi.org/10.17863/cam.45338
_version_ 1789959591330578432