Parameter Optimization in Sea Ice Models with Elastic-Viscoplastic Rheology

Ice rheology formulation is the key component of the modern sea ice modeling. In the CICE6 community model, rheology and landfast grounding/arching effects are simulated by functions of the sea ice thickness and concentration with a set of fixed parameters empirically adjusted to optimize the model...

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Main Authors: Panteleev, Gleb, Yaremchuk, Max, Stroh, Jacob N., Francis, Oceana P., Allard, Richard
Format: Text
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.5194/tc-2019-219
https://tc.copernicus.org/preprints/tc-2019-219/
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spelling ftcopernicus:oai:publications.copernicus.org:tcd80082 2023-05-15T18:16:16+02:00 Parameter Optimization in Sea Ice Models with Elastic-Viscoplastic Rheology Panteleev, Gleb Yaremchuk, Max Stroh, Jacob N. Francis, Oceana P. Allard, Richard 2019-10-29 application/pdf https://doi.org/10.5194/tc-2019-219 https://tc.copernicus.org/preprints/tc-2019-219/ eng eng doi:10.5194/tc-2019-219 https://tc.copernicus.org/preprints/tc-2019-219/ eISSN: 1994-0424 Text 2019 ftcopernicus https://doi.org/10.5194/tc-2019-219 2020-07-20T16:22:36Z Ice rheology formulation is the key component of the modern sea ice modeling. In the CICE6 community model, rheology and landfast grounding/arching effects are simulated by functions of the sea ice thickness and concentration with a set of fixed parameters empirically adjusted to optimize the model performance. In this study we consider a spatially variable extension of representing these parameters in the two-dimensional EVP sea ice model with a formulation similar to CICE6. Feasibility of optimization of the rheological and landfast sea ice parameters is assessed by applying variational data assimilation to the synthetic observations of ice concentration, thickness and velocity. It is found that the tangent linear and adjoint models featuring EVP rheology are unstable, but can be stabilized by adding Newtonian damping term into the adjoint equation. The set of the observation system simulation experiments shows that landfast parameter distributions can be reconstructed after 5–10 iterations of the minimization procedure. Optimization of the sea ice initial conditions and spatially varying parameters in the equation for the stress tensor requires more computation, but provides a better hindcast of the sea ice state and the internal stress tensor. Analysis of the inaccuracy in the wind forcing and errors in the sea ice thickness observations have shown reasonable robustness of the variational DA approach and feasibility of its application to the available and incoming observations. Text Sea ice Copernicus Publications: E-Journals
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Ice rheology formulation is the key component of the modern sea ice modeling. In the CICE6 community model, rheology and landfast grounding/arching effects are simulated by functions of the sea ice thickness and concentration with a set of fixed parameters empirically adjusted to optimize the model performance. In this study we consider a spatially variable extension of representing these parameters in the two-dimensional EVP sea ice model with a formulation similar to CICE6. Feasibility of optimization of the rheological and landfast sea ice parameters is assessed by applying variational data assimilation to the synthetic observations of ice concentration, thickness and velocity. It is found that the tangent linear and adjoint models featuring EVP rheology are unstable, but can be stabilized by adding Newtonian damping term into the adjoint equation. The set of the observation system simulation experiments shows that landfast parameter distributions can be reconstructed after 5–10 iterations of the minimization procedure. Optimization of the sea ice initial conditions and spatially varying parameters in the equation for the stress tensor requires more computation, but provides a better hindcast of the sea ice state and the internal stress tensor. Analysis of the inaccuracy in the wind forcing and errors in the sea ice thickness observations have shown reasonable robustness of the variational DA approach and feasibility of its application to the available and incoming observations.
format Text
author Panteleev, Gleb
Yaremchuk, Max
Stroh, Jacob N.
Francis, Oceana P.
Allard, Richard
spellingShingle Panteleev, Gleb
Yaremchuk, Max
Stroh, Jacob N.
Francis, Oceana P.
Allard, Richard
Parameter Optimization in Sea Ice Models with Elastic-Viscoplastic Rheology
author_facet Panteleev, Gleb
Yaremchuk, Max
Stroh, Jacob N.
Francis, Oceana P.
Allard, Richard
author_sort Panteleev, Gleb
title Parameter Optimization in Sea Ice Models with Elastic-Viscoplastic Rheology
title_short Parameter Optimization in Sea Ice Models with Elastic-Viscoplastic Rheology
title_full Parameter Optimization in Sea Ice Models with Elastic-Viscoplastic Rheology
title_fullStr Parameter Optimization in Sea Ice Models with Elastic-Viscoplastic Rheology
title_full_unstemmed Parameter Optimization in Sea Ice Models with Elastic-Viscoplastic Rheology
title_sort parameter optimization in sea ice models with elastic-viscoplastic rheology
publishDate 2019
url https://doi.org/10.5194/tc-2019-219
https://tc.copernicus.org/preprints/tc-2019-219/
genre Sea ice
genre_facet Sea ice
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-2019-219
https://tc.copernicus.org/preprints/tc-2019-219/
op_doi https://doi.org/10.5194/tc-2019-219
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