Damaging viscous-plastic sea ice

We implement a damage parametrization in the standard viscous-plastic sea ice model to disentangle its effect from model physics (visco-elastic or elasto-brittle vs. visco-plastic) on its ability to reproduce observed scaling laws of deformation. To this end, we compare scaling properties and multif...

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Main Authors: Savard, Antoine, Tremblay, Bruno
Format: Other/Unknown Material
Language:unknown
Published: Authorea, Inc. 2023
Subjects:
Online Access:http://dx.doi.org/10.22541/essoar.168614539.94346287/v1
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spelling crwinnower:10.22541/essoar.168614539.94346287/v1 2024-06-02T08:14:15+00:00 Damaging viscous-plastic sea ice Savard, Antoine Tremblay, Bruno 2023 http://dx.doi.org/10.22541/essoar.168614539.94346287/v1 unknown Authorea, Inc. posted-content 2023 crwinnower https://doi.org/10.22541/essoar.168614539.94346287/v1 2024-05-07T14:19:10Z We implement a damage parametrization in the standard viscous-plastic sea ice model to disentangle its effect from model physics (visco-elastic or elasto-brittle vs. visco-plastic) on its ability to reproduce observed scaling laws of deformation. To this end, we compare scaling properties and multifractality of simulated divergence and shear strain rate (as proposed in SIREx1), with those derived from the RADARSAT Geophysical Processor System (RGPS). Results show that including a damage parametrization in the standard viscous-plastic model increases the spatial, but decreases temporal localization of simulated Linear Kinematic Features, and brings all spatial deformation rate statistics in line with observations from RGPS without the need to increase the mechanical shear strength of sea ice as recently proposed for lower resolution viscous-plastic sea ice models. In fact, including damage an healing timescale of $t_h=30\>$days and an increased mechanical strength unveil multifractal behavior that does not fit the theory. Therefore, a damage parametrization is a powerful tuning knob affecting the deformation statistics. Other/Unknown Material Sea ice The Winnower
institution Open Polar
collection The Winnower
op_collection_id crwinnower
language unknown
description We implement a damage parametrization in the standard viscous-plastic sea ice model to disentangle its effect from model physics (visco-elastic or elasto-brittle vs. visco-plastic) on its ability to reproduce observed scaling laws of deformation. To this end, we compare scaling properties and multifractality of simulated divergence and shear strain rate (as proposed in SIREx1), with those derived from the RADARSAT Geophysical Processor System (RGPS). Results show that including a damage parametrization in the standard viscous-plastic model increases the spatial, but decreases temporal localization of simulated Linear Kinematic Features, and brings all spatial deformation rate statistics in line with observations from RGPS without the need to increase the mechanical shear strength of sea ice as recently proposed for lower resolution viscous-plastic sea ice models. In fact, including damage an healing timescale of $t_h=30\>$days and an increased mechanical strength unveil multifractal behavior that does not fit the theory. Therefore, a damage parametrization is a powerful tuning knob affecting the deformation statistics.
format Other/Unknown Material
author Savard, Antoine
Tremblay, Bruno
spellingShingle Savard, Antoine
Tremblay, Bruno
Damaging viscous-plastic sea ice
author_facet Savard, Antoine
Tremblay, Bruno
author_sort Savard, Antoine
title Damaging viscous-plastic sea ice
title_short Damaging viscous-plastic sea ice
title_full Damaging viscous-plastic sea ice
title_fullStr Damaging viscous-plastic sea ice
title_full_unstemmed Damaging viscous-plastic sea ice
title_sort damaging viscous-plastic sea ice
publisher Authorea, Inc.
publishDate 2023
url http://dx.doi.org/10.22541/essoar.168614539.94346287/v1
genre Sea ice
genre_facet Sea ice
op_doi https://doi.org/10.22541/essoar.168614539.94346287/v1
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