Basal hydrofractures near sticky patches

Basal crevasses are macroscopic structural discontinuities at the base of ice sheets and glaciers that arise by fracture. Motivated by observations and by the mechanics of elastic fracture, we hypothesise that spatial variations in basal stress (in the presence of basal water pressure) can promote a...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Hanwen Zhang, Timothy Davis, Richard F. Katz, Laura A. Stevens, Dave A. May
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2023
Subjects:
Online Access:https://doi.org/10.1017/jog.2022.75
https://doaj.org/article/68bb383bd8964d56b06e7ffc46ce750d
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spelling ftdoajarticles:oai:doaj.org/article:68bb383bd8964d56b06e7ffc46ce750d 2023-06-11T04:12:49+02:00 Basal hydrofractures near sticky patches Hanwen Zhang Timothy Davis Richard F. Katz Laura A. Stevens Dave A. May 2023-06-01T00:00:00Z https://doi.org/10.1017/jog.2022.75 https://doaj.org/article/68bb383bd8964d56b06e7ffc46ce750d EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143022000752/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.75 0022-1430 1727-5652 https://doaj.org/article/68bb383bd8964d56b06e7ffc46ce750d Journal of Glaciology, Vol 69, Pp 475-486 (2023) Calving crevasses glacier modelling ice-sheet modelling Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1017/jog.2022.75 2023-05-28T00:37:02Z Basal crevasses are macroscopic structural discontinuities at the base of ice sheets and glaciers that arise by fracture. Motivated by observations and by the mechanics of elastic fracture, we hypothesise that spatial variations in basal stress (in the presence of basal water pressure) can promote and localise basal crevassing. We quantify this process in the theoretical context of linear elastic fracture mechanics. We develop a model evaluating the effect of shear-stress variation on the growth of basal crevasses. Our results indicate that sticky patches promote the propagation of basal crevasses, increase their length of propagation into the ice and, under some conditions, give them curved trajectories that incline upstream. A detailed exploration of the parameter space is conducted to gain a better understanding of the conditions under which sticky-patch-induced basal crevassing is expected beneath ice sheets and glaciers. Article in Journal/Newspaper Ice Sheet Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 1 12
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Calving
crevasses
glacier modelling
ice-sheet modelling
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Calving
crevasses
glacier modelling
ice-sheet modelling
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Hanwen Zhang
Timothy Davis
Richard F. Katz
Laura A. Stevens
Dave A. May
Basal hydrofractures near sticky patches
topic_facet Calving
crevasses
glacier modelling
ice-sheet modelling
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Basal crevasses are macroscopic structural discontinuities at the base of ice sheets and glaciers that arise by fracture. Motivated by observations and by the mechanics of elastic fracture, we hypothesise that spatial variations in basal stress (in the presence of basal water pressure) can promote and localise basal crevassing. We quantify this process in the theoretical context of linear elastic fracture mechanics. We develop a model evaluating the effect of shear-stress variation on the growth of basal crevasses. Our results indicate that sticky patches promote the propagation of basal crevasses, increase their length of propagation into the ice and, under some conditions, give them curved trajectories that incline upstream. A detailed exploration of the parameter space is conducted to gain a better understanding of the conditions under which sticky-patch-induced basal crevassing is expected beneath ice sheets and glaciers.
format Article in Journal/Newspaper
author Hanwen Zhang
Timothy Davis
Richard F. Katz
Laura A. Stevens
Dave A. May
author_facet Hanwen Zhang
Timothy Davis
Richard F. Katz
Laura A. Stevens
Dave A. May
author_sort Hanwen Zhang
title Basal hydrofractures near sticky patches
title_short Basal hydrofractures near sticky patches
title_full Basal hydrofractures near sticky patches
title_fullStr Basal hydrofractures near sticky patches
title_full_unstemmed Basal hydrofractures near sticky patches
title_sort basal hydrofractures near sticky patches
publisher Cambridge University Press
publishDate 2023
url https://doi.org/10.1017/jog.2022.75
https://doaj.org/article/68bb383bd8964d56b06e7ffc46ce750d
genre Ice Sheet
Journal of Glaciology
genre_facet Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology, Vol 69, Pp 475-486 (2023)
op_relation https://www.cambridge.org/core/product/identifier/S0022143022000752/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2022.75
0022-1430
1727-5652
https://doaj.org/article/68bb383bd8964d56b06e7ffc46ce750d
op_doi https://doi.org/10.1017/jog.2022.75
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 12
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