Tidewater glacier response to individual calving events

Tidewater glaciers have been observed to experience instantaneous, stepwise increases in velocity during iceberg-calving events due to a loss of resistive stresses. These changes in stress can potentially impact tidewater glacier stability by promoting additional calving and affecting the viscous de...

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Main Authors: Amundson, Jason M., Truffer, Martin, Zwinger, Thomas
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2022
Subjects:
Online Access:http://hdl.handle.net/11122/12861
id ftunivalaska:oai:scholarworks.alaska.edu:11122/12861
record_format openpolar
spelling ftunivalaska:oai:scholarworks.alaska.edu:11122/12861 2023-05-15T16:57:10+02:00 Tidewater glacier response to individual calving events Amundson, Jason M. Truffer, Martin Zwinger, Thomas 2022-03-15 http://hdl.handle.net/11122/12861 en_US eng Cambridge University Press Amundson JM, Truffer M, Zwinger T (2022). Tidewater glacier response to individual calving events. Journal of Glaciology 1–10. https://doi.org/10.1017/ jog.2022.26 http://hdl.handle.net/11122/12861 Journal of Glaciology Tidewater glaciers Calving Velocity Iceberg-calving events Perturbation theory Article 2022 ftunivalaska 2023-02-23T21:38:01Z Tidewater glaciers have been observed to experience instantaneous, stepwise increases in velocity during iceberg-calving events due to a loss of resistive stresses. These changes in stress can potentially impact tidewater glacier stability by promoting additional calving and affecting the viscous delivery of ice to the terminus. Using flow models and perturbation theory, we demonstrate that calving events and subsequent terminus readvance produce quasi-periodic, sawtooth oscillations in stress that originate at the terminus and propagate upstream. The stress perturbations travel at speeds much greater than the glacier velocities and, for laterally resisted glaciers, rapidly decay within a few ice thickness of the terminus. Consequently, because terminus fluctuations due to individual calving events tend to be much higher frequency than climate variations, individual calving events have little direct impact on the viscous delivery of ice to the terminus. This suggests that the primary mechanism by which calving events can trigger instability is by causing fluctuations in stress that weaken the ice and lead to additional calving and sustained terminus retreat. Our results further demonstrate a stronger response to calving events in simulations that include the full stress tensor, highlighting the importance of accounting for higher order stresses when developing calving parameterizations. © The Author(s), 2022. Published by Cambridge University Press. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. Yes Article in Journal/Newspaper Journal of Glaciology Tidewater University of Alaska: ScholarWorks@UA
institution Open Polar
collection University of Alaska: ScholarWorks@UA
op_collection_id ftunivalaska
language English
topic Tidewater glaciers
Calving
Velocity
Iceberg-calving events
Perturbation theory
spellingShingle Tidewater glaciers
Calving
Velocity
Iceberg-calving events
Perturbation theory
Amundson, Jason M.
Truffer, Martin
Zwinger, Thomas
Tidewater glacier response to individual calving events
topic_facet Tidewater glaciers
Calving
Velocity
Iceberg-calving events
Perturbation theory
description Tidewater glaciers have been observed to experience instantaneous, stepwise increases in velocity during iceberg-calving events due to a loss of resistive stresses. These changes in stress can potentially impact tidewater glacier stability by promoting additional calving and affecting the viscous delivery of ice to the terminus. Using flow models and perturbation theory, we demonstrate that calving events and subsequent terminus readvance produce quasi-periodic, sawtooth oscillations in stress that originate at the terminus and propagate upstream. The stress perturbations travel at speeds much greater than the glacier velocities and, for laterally resisted glaciers, rapidly decay within a few ice thickness of the terminus. Consequently, because terminus fluctuations due to individual calving events tend to be much higher frequency than climate variations, individual calving events have little direct impact on the viscous delivery of ice to the terminus. This suggests that the primary mechanism by which calving events can trigger instability is by causing fluctuations in stress that weaken the ice and lead to additional calving and sustained terminus retreat. Our results further demonstrate a stronger response to calving events in simulations that include the full stress tensor, highlighting the importance of accounting for higher order stresses when developing calving parameterizations. © The Author(s), 2022. Published by Cambridge University Press. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. Yes
format Article in Journal/Newspaper
author Amundson, Jason M.
Truffer, Martin
Zwinger, Thomas
author_facet Amundson, Jason M.
Truffer, Martin
Zwinger, Thomas
author_sort Amundson, Jason M.
title Tidewater glacier response to individual calving events
title_short Tidewater glacier response to individual calving events
title_full Tidewater glacier response to individual calving events
title_fullStr Tidewater glacier response to individual calving events
title_full_unstemmed Tidewater glacier response to individual calving events
title_sort tidewater glacier response to individual calving events
publisher Cambridge University Press
publishDate 2022
url http://hdl.handle.net/11122/12861
genre Journal of Glaciology
Tidewater
genre_facet Journal of Glaciology
Tidewater
op_relation Amundson JM, Truffer M, Zwinger T (2022). Tidewater glacier response to individual calving events. Journal of Glaciology 1–10. https://doi.org/10.1017/ jog.2022.26
http://hdl.handle.net/11122/12861
Journal of Glaciology
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