A phase field model for fractures in ice shelves

Abstract Ice shelves are large floating ice masses, that are formed when glaciers are becoming afloat at the margin of ice sheets. One dominating mass loss mechanism of ice shelves is calving, describing the detachment of icebergs at the front. Ice shelves stabilize inland ice glaciers due to buttre...

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Published in:PAMM
Main Authors: Sondershaus, Rabea, Humbert, Angelika, Müller, Ralf
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:http://dx.doi.org/10.1002/pamm.202200256
https://onlinelibrary.wiley.com/doi/pdf/10.1002/pamm.202200256
id crwiley:10.1002/pamm.202200256
record_format openpolar
spelling crwiley:10.1002/pamm.202200256 2024-06-02T07:55:25+00:00 A phase field model for fractures in ice shelves Sondershaus, Rabea Humbert, Angelika Müller, Ralf 2023 http://dx.doi.org/10.1002/pamm.202200256 https://onlinelibrary.wiley.com/doi/pdf/10.1002/pamm.202200256 en eng Wiley http://creativecommons.org/licenses/by-nc-nd/4.0/ PAMM volume 22, issue 1 ISSN 1617-7061 1617-7061 journal-article 2023 crwiley https://doi.org/10.1002/pamm.202200256 2024-05-03T11:43:58Z Abstract Ice shelves are large floating ice masses, that are formed when glaciers are becoming afloat at the margin of ice sheets. One dominating mass loss mechanism of ice shelves is calving, describing the detachment of icebergs at the front. Ice shelves stabilize inland ice glaciers due to buttressing. If the stabilizing effect of an ice shelf vanishes because of disintegration or thinning, the corresponding glacier accelerates resulting in sea level rise. To describe calving and disintegration of ice shelves, it is important to investigate fracture propagation in ice. A powerful method in fracture mechanics is the phase field method which is based on Griffith's theory. It approximates cracks in a diffuse manner by using a continuous scalar field. We propose a phase field fracture model for ice considering its characteristic material properties. The material behavior of ice depends on the considered time scales. On short time scales it behaves like a solid and while it acts like a fluid on long time scales, which classifies it as a viscoelastic material of Maxwell type. This has been verified by observations. The phase field method allows us to simulate typical fracture situations of ice shelves in Antarctica and Greenland. Article in Journal/Newspaper Antarc* Antarctica glacier Greenland Ice Shelf Ice Shelves Wiley Online Library Greenland PAMM 22 1
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Ice shelves are large floating ice masses, that are formed when glaciers are becoming afloat at the margin of ice sheets. One dominating mass loss mechanism of ice shelves is calving, describing the detachment of icebergs at the front. Ice shelves stabilize inland ice glaciers due to buttressing. If the stabilizing effect of an ice shelf vanishes because of disintegration or thinning, the corresponding glacier accelerates resulting in sea level rise. To describe calving and disintegration of ice shelves, it is important to investigate fracture propagation in ice. A powerful method in fracture mechanics is the phase field method which is based on Griffith's theory. It approximates cracks in a diffuse manner by using a continuous scalar field. We propose a phase field fracture model for ice considering its characteristic material properties. The material behavior of ice depends on the considered time scales. On short time scales it behaves like a solid and while it acts like a fluid on long time scales, which classifies it as a viscoelastic material of Maxwell type. This has been verified by observations. The phase field method allows us to simulate typical fracture situations of ice shelves in Antarctica and Greenland.
format Article in Journal/Newspaper
author Sondershaus, Rabea
Humbert, Angelika
Müller, Ralf
spellingShingle Sondershaus, Rabea
Humbert, Angelika
Müller, Ralf
A phase field model for fractures in ice shelves
author_facet Sondershaus, Rabea
Humbert, Angelika
Müller, Ralf
author_sort Sondershaus, Rabea
title A phase field model for fractures in ice shelves
title_short A phase field model for fractures in ice shelves
title_full A phase field model for fractures in ice shelves
title_fullStr A phase field model for fractures in ice shelves
title_full_unstemmed A phase field model for fractures in ice shelves
title_sort phase field model for fractures in ice shelves
publisher Wiley
publishDate 2023
url http://dx.doi.org/10.1002/pamm.202200256
https://onlinelibrary.wiley.com/doi/pdf/10.1002/pamm.202200256
geographic Greenland
geographic_facet Greenland
genre Antarc*
Antarctica
glacier
Greenland
Ice Shelf
Ice Shelves
genre_facet Antarc*
Antarctica
glacier
Greenland
Ice Shelf
Ice Shelves
op_source PAMM
volume 22, issue 1
ISSN 1617-7061 1617-7061
op_rights http://creativecommons.org/licenses/by-nc-nd/4.0/
op_doi https://doi.org/10.1002/pamm.202200256
container_title PAMM
container_volume 22
container_issue 1
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