Evaluation of four calving laws for Antarctic ice shelves

Many floating ice shelves in Antarctica buttress the ice streams feeding them, thereby reducing the discharge of icebergs into the ocean. The rate at which ice shelves calve icebergs and how fast they flow determine whether they advance, retreat, or remain stable, exerting a first-order control on i...

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Published in:The Cryosphere
Main Authors: Wilner, Joel A., Morlighem, Mathieu, Cheng, Gong
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-4889-2023
https://tc.copernicus.org/articles/17/4889/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:tc112130 2024-09-15T17:41:12+00:00 Evaluation of four calving laws for Antarctic ice shelves Wilner, Joel A. Morlighem, Mathieu Cheng, Gong 2023-11-21 application/pdf https://doi.org/10.5194/tc-17-4889-2023 https://tc.copernicus.org/articles/17/4889/2023/ eng eng doi:10.5194/tc-17-4889-2023 https://tc.copernicus.org/articles/17/4889/2023/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-17-4889-2023 2024-08-28T05:24:15Z Many floating ice shelves in Antarctica buttress the ice streams feeding them, thereby reducing the discharge of icebergs into the ocean. The rate at which ice shelves calve icebergs and how fast they flow determine whether they advance, retreat, or remain stable, exerting a first-order control on ice discharge. To parameterize calving within ice sheet models, several empirical and physical calving “laws” have been proposed in the past few decades. Such laws emphasize dissimilar features, including along- and across-flow strain rates (the eigencalving law), a fracture yield criterion (the von Mises law), longitudinal stretching (the crevasse depth law), and a simple ice thickness threshold (the minimum thickness law), among others. Despite the multitude of established calving laws, these laws remain largely unvalidated for the Antarctic Ice Sheet, rendering it difficult to assess the broad applicability of any given law in Antarctica. We address this shortcoming through a set of numerical experiments that evaluate existing calving laws for 10 ice shelves around the Antarctic Ice Sheet. We utilize the Ice-sheet and Sea-level System Model (ISSM) and implement four calving laws under constant external forcing, calibrating the free parameter of each of these calving laws for each ice shelf by assuming that the current position of the ice front is in steady state and finding the set of parameters that best achieves this position over a simulation of 200 years. We find that, in general, the eigencalving and von Mises laws best reproduce observed calving front positions under the steady-state position assumption. These results will streamline future modeling efforts of Antarctic ice shelves by better informing the relevant physics of Antarctic-style calving on a shelf-by-shelf basis. Text Antarc* Antarctic Antarctica Ice Sheet Ice Shelf Ice Shelves Iceberg* Copernicus Publications: E-Journals The Cryosphere 17 11 4889 4901
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Many floating ice shelves in Antarctica buttress the ice streams feeding them, thereby reducing the discharge of icebergs into the ocean. The rate at which ice shelves calve icebergs and how fast they flow determine whether they advance, retreat, or remain stable, exerting a first-order control on ice discharge. To parameterize calving within ice sheet models, several empirical and physical calving “laws” have been proposed in the past few decades. Such laws emphasize dissimilar features, including along- and across-flow strain rates (the eigencalving law), a fracture yield criterion (the von Mises law), longitudinal stretching (the crevasse depth law), and a simple ice thickness threshold (the minimum thickness law), among others. Despite the multitude of established calving laws, these laws remain largely unvalidated for the Antarctic Ice Sheet, rendering it difficult to assess the broad applicability of any given law in Antarctica. We address this shortcoming through a set of numerical experiments that evaluate existing calving laws for 10 ice shelves around the Antarctic Ice Sheet. We utilize the Ice-sheet and Sea-level System Model (ISSM) and implement four calving laws under constant external forcing, calibrating the free parameter of each of these calving laws for each ice shelf by assuming that the current position of the ice front is in steady state and finding the set of parameters that best achieves this position over a simulation of 200 years. We find that, in general, the eigencalving and von Mises laws best reproduce observed calving front positions under the steady-state position assumption. These results will streamline future modeling efforts of Antarctic ice shelves by better informing the relevant physics of Antarctic-style calving on a shelf-by-shelf basis.
format Text
author Wilner, Joel A.
Morlighem, Mathieu
Cheng, Gong
spellingShingle Wilner, Joel A.
Morlighem, Mathieu
Cheng, Gong
Evaluation of four calving laws for Antarctic ice shelves
author_facet Wilner, Joel A.
Morlighem, Mathieu
Cheng, Gong
author_sort Wilner, Joel A.
title Evaluation of four calving laws for Antarctic ice shelves
title_short Evaluation of four calving laws for Antarctic ice shelves
title_full Evaluation of four calving laws for Antarctic ice shelves
title_fullStr Evaluation of four calving laws for Antarctic ice shelves
title_full_unstemmed Evaluation of four calving laws for Antarctic ice shelves
title_sort evaluation of four calving laws for antarctic ice shelves
publishDate 2023
url https://doi.org/10.5194/tc-17-4889-2023
https://tc.copernicus.org/articles/17/4889/2023/
genre Antarc*
Antarctic
Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
Iceberg*
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
Iceberg*
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-17-4889-2023
https://tc.copernicus.org/articles/17/4889/2023/
op_doi https://doi.org/10.5194/tc-17-4889-2023
container_title The Cryosphere
container_volume 17
container_issue 11
container_start_page 4889
op_container_end_page 4901
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