Parameter sensitivity analysis of dynamic ice sheet models – numerical computations

The friction coefficient and the base topography of a stationary and a dynamic ice sheet are perturbed in two models for the ice: the full Stokes equations and the shallow shelf approximation. The sensitivity to the perturbations of the velocity and the height at the surface is quantified by solving...

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Published in:The Cryosphere
Main Authors: Cheng, Gong, Lötstedt, Per
Format: Text
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.5194/tc-14-673-2020
https://tc.copernicus.org/articles/14/673/2020/
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spelling ftcopernicus:oai:publications.copernicus.org:tc77627 2023-05-15T16:40:21+02:00 Parameter sensitivity analysis of dynamic ice sheet models – numerical computations Cheng, Gong Lötstedt, Per 2020-02-17 application/pdf https://doi.org/10.5194/tc-14-673-2020 https://tc.copernicus.org/articles/14/673/2020/ eng eng doi:10.5194/tc-14-673-2020 https://tc.copernicus.org/articles/14/673/2020/ eISSN: 1994-0424 Text 2020 ftcopernicus https://doi.org/10.5194/tc-14-673-2020 2020-07-20T16:22:25Z The friction coefficient and the base topography of a stationary and a dynamic ice sheet are perturbed in two models for the ice: the full Stokes equations and the shallow shelf approximation. The sensitivity to the perturbations of the velocity and the height at the surface is quantified by solving the adjoint equations of the stress and the height equations providing weights for the perturbed data. The adjoint equations are solved numerically and the sensitivity is computed in several examples in two dimensions. A transfer matrix couples the perturbations at the base with the perturbations at the top. Comparisons are made with analytical solutions to simplified problems. The sensitivity to perturbations depends on their wavelengths and the distance to the grounding line. A perturbation in the topography has a direct effect at the ice surface above it, while a change in the friction coefficient is less visible there. Text Ice Sheet Copernicus Publications: E-Journals The Cryosphere 14 2 673 691
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The friction coefficient and the base topography of a stationary and a dynamic ice sheet are perturbed in two models for the ice: the full Stokes equations and the shallow shelf approximation. The sensitivity to the perturbations of the velocity and the height at the surface is quantified by solving the adjoint equations of the stress and the height equations providing weights for the perturbed data. The adjoint equations are solved numerically and the sensitivity is computed in several examples in two dimensions. A transfer matrix couples the perturbations at the base with the perturbations at the top. Comparisons are made with analytical solutions to simplified problems. The sensitivity to perturbations depends on their wavelengths and the distance to the grounding line. A perturbation in the topography has a direct effect at the ice surface above it, while a change in the friction coefficient is less visible there.
format Text
author Cheng, Gong
Lötstedt, Per
spellingShingle Cheng, Gong
Lötstedt, Per
Parameter sensitivity analysis of dynamic ice sheet models – numerical computations
author_facet Cheng, Gong
Lötstedt, Per
author_sort Cheng, Gong
title Parameter sensitivity analysis of dynamic ice sheet models – numerical computations
title_short Parameter sensitivity analysis of dynamic ice sheet models – numerical computations
title_full Parameter sensitivity analysis of dynamic ice sheet models – numerical computations
title_fullStr Parameter sensitivity analysis of dynamic ice sheet models – numerical computations
title_full_unstemmed Parameter sensitivity analysis of dynamic ice sheet models – numerical computations
title_sort parameter sensitivity analysis of dynamic ice sheet models – numerical computations
publishDate 2020
url https://doi.org/10.5194/tc-14-673-2020
https://tc.copernicus.org/articles/14/673/2020/
genre Ice Sheet
genre_facet Ice Sheet
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-14-673-2020
https://tc.copernicus.org/articles/14/673/2020/
op_doi https://doi.org/10.5194/tc-14-673-2020
container_title The Cryosphere
container_volume 14
container_issue 2
container_start_page 673
op_container_end_page 691
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