Marine ice sheet experiments with the Community Ice Sheet Model

Ice sheet models differ in their numerical treatment of dynamical processes. Simulations of marine-based ice are sensitive to the choice of Stokes flow approximation and basal friction law and to the treatment of stresses and melt rates near the grounding line. We study the effects of these numerica...

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Published in:The Cryosphere
Main Authors: Leguy, Gunter R., Lipscomb, William H., Asay-Davis, Xylar S.
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/tc-15-3229-2021
https://tc.copernicus.org/articles/15/3229/2021/
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spelling ftcopernicus:oai:publications.copernicus.org:tc90369 2023-05-15T16:39:39+02:00 Marine ice sheet experiments with the Community Ice Sheet Model Leguy, Gunter R. Lipscomb, William H. Asay-Davis, Xylar S. 2021-07-14 application/pdf https://doi.org/10.5194/tc-15-3229-2021 https://tc.copernicus.org/articles/15/3229/2021/ eng eng doi:10.5194/tc-15-3229-2021 https://tc.copernicus.org/articles/15/3229/2021/ eISSN: 1994-0424 Text 2021 ftcopernicus https://doi.org/10.5194/tc-15-3229-2021 2021-07-19T16:22:26Z Ice sheet models differ in their numerical treatment of dynamical processes. Simulations of marine-based ice are sensitive to the choice of Stokes flow approximation and basal friction law and to the treatment of stresses and melt rates near the grounding line. We study the effects of these numerical choices on marine ice sheet dynamics in the Community Ice Sheet Model (CISM). In the framework of the Marine Ice Sheet Model Intercomparison Project 3d (MISMIP3d), we show that a depth-integrated, higher-order solver gives results similar to a 3D (Blatter–Pattyn) solver. We confirm that using a grounding line parameterization to approximate stresses in the grounding zone leads to accurate representation of ice sheet flow with a resolution of ∼2 km, as opposed to ∼0.5 km without the parameterization. In the MISMIP+ experimental framework, we compare different treatments of sub-shelf melting near the grounding line. In contrast to recent studies arguing that melting should not be applied in partly grounded cells, it is usually beneficial in CISM simulations to apply some melting in these cells. This suggests that the optimal treatment of melting near the grounding line can depend on ice sheet geometry, forcing, or model numerics. In both experimental frameworks, ice flow is sensitive to the choice of basal friction law. To study this sensitivity, we evaluate friction laws that vary the connectivity between the basal hydrological system and the ocean near the grounding line. CISM yields accurate results in steady-state and perturbation experiments at a resolution of ∼2 km (arguably 4 km) when the connectivity is low or moderate and ∼1 km (arguably 2 km) when the connectivity is strong. Text Ice Sheet Copernicus Publications: E-Journals The Cryosphere 15 7 3229 3253
institution Open Polar
collection Copernicus Publications: E-Journals
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language English
description Ice sheet models differ in their numerical treatment of dynamical processes. Simulations of marine-based ice are sensitive to the choice of Stokes flow approximation and basal friction law and to the treatment of stresses and melt rates near the grounding line. We study the effects of these numerical choices on marine ice sheet dynamics in the Community Ice Sheet Model (CISM). In the framework of the Marine Ice Sheet Model Intercomparison Project 3d (MISMIP3d), we show that a depth-integrated, higher-order solver gives results similar to a 3D (Blatter–Pattyn) solver. We confirm that using a grounding line parameterization to approximate stresses in the grounding zone leads to accurate representation of ice sheet flow with a resolution of ∼2 km, as opposed to ∼0.5 km without the parameterization. In the MISMIP+ experimental framework, we compare different treatments of sub-shelf melting near the grounding line. In contrast to recent studies arguing that melting should not be applied in partly grounded cells, it is usually beneficial in CISM simulations to apply some melting in these cells. This suggests that the optimal treatment of melting near the grounding line can depend on ice sheet geometry, forcing, or model numerics. In both experimental frameworks, ice flow is sensitive to the choice of basal friction law. To study this sensitivity, we evaluate friction laws that vary the connectivity between the basal hydrological system and the ocean near the grounding line. CISM yields accurate results in steady-state and perturbation experiments at a resolution of ∼2 km (arguably 4 km) when the connectivity is low or moderate and ∼1 km (arguably 2 km) when the connectivity is strong.
format Text
author Leguy, Gunter R.
Lipscomb, William H.
Asay-Davis, Xylar S.
spellingShingle Leguy, Gunter R.
Lipscomb, William H.
Asay-Davis, Xylar S.
Marine ice sheet experiments with the Community Ice Sheet Model
author_facet Leguy, Gunter R.
Lipscomb, William H.
Asay-Davis, Xylar S.
author_sort Leguy, Gunter R.
title Marine ice sheet experiments with the Community Ice Sheet Model
title_short Marine ice sheet experiments with the Community Ice Sheet Model
title_full Marine ice sheet experiments with the Community Ice Sheet Model
title_fullStr Marine ice sheet experiments with the Community Ice Sheet Model
title_full_unstemmed Marine ice sheet experiments with the Community Ice Sheet Model
title_sort marine ice sheet experiments with the community ice sheet model
publishDate 2021
url https://doi.org/10.5194/tc-15-3229-2021
https://tc.copernicus.org/articles/15/3229/2021/
genre Ice Sheet
genre_facet Ice Sheet
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-15-3229-2021
https://tc.copernicus.org/articles/15/3229/2021/
op_doi https://doi.org/10.5194/tc-15-3229-2021
container_title The Cryosphere
container_volume 15
container_issue 7
container_start_page 3229
op_container_end_page 3253
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