Ocean Kinetic Energy Backscatter Parametrization on Unstructured Grids: Impact on Global Eddy-Permitting Simulations

In this study we demonstrate the potential of a kinetic energy backscatter scheme for use in global ocean simulations. Ocean models commonly employ (bi)harmonic eddy viscosities causing excessive dissipation of kinetic energy in eddy-permitting simulations. Overdissipation not only affects the small...

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Published in:Journal of Advances in Modeling Earth Systems
Main Authors: Juricke, Stephan, Danilov, Sergey, Koldunov, Nikolay, Oliver, Marcel, Sidorenko, Dmitry
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.1029/2019MS001855
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9074
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author Juricke, Stephan
Danilov, Sergey
Koldunov, Nikolay
Oliver, Marcel
Sidorenko, Dmitry
author_facet Juricke, Stephan
Danilov, Sergey
Koldunov, Nikolay
Oliver, Marcel
Sidorenko, Dmitry
author_sort Juricke, Stephan
collection GEO-LEOe-docs (FID GEO)
container_issue 1
container_title Journal of Advances in Modeling Earth Systems
container_volume 12
description In this study we demonstrate the potential of a kinetic energy backscatter scheme for use in global ocean simulations. Ocean models commonly employ (bi)harmonic eddy viscosities causing excessive dissipation of kinetic energy in eddy-permitting simulations. Overdissipation not only affects the smallest resolved scales but also the generation of eddies through baroclinic instabilities, impacting the entire wave number spectrum. The backscatter scheme returns part of this overdissipated energy back into the resolved flow. We employ backscatter in the FESOM2 multiresolution ocean model with a quasi-uniform 1/4° mesh. In multidecadal ocean simulations, backscatter increases eddy activity by a factor 2 or more, moving the simulation closer to observational estimates of sea surface height variability. Moreover, mean sea surface height, temperature, and salinity biases are reduced. This amounts to a globally averaged bias reduction of around 10% for each field, which is even larger in the Antarctic Circumpolar Current. However, in some regions such as the coastal Kuroshio, backscatter leads to a slight overenergizing of the flow and, in the Antarctic, to an unrealistic reduction of sea ice. Some of the bias increases can be reduced by a retuning of the model, and we suggest related adjustments to the backscatter scheme. The backscatter simulation is about 2.5 times as expensive as a simulation without backscatter. Most of the increased cost is due to a halving of the time step to accommodate higher simulated velocities.
format Article in Journal/Newspaper
genre Antarc*
Antarctic
Sea ice
genre_facet Antarc*
Antarctic
Sea ice
geographic Antarctic
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op_doi https://doi.org/10.1029/2019MS001855
op_relation doi:10.1029/2019MS001855
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9074
op_rights This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.
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spelling ftsubggeo:oai:e-docs.geo-leo.de:11858/9074 2025-01-16T19:11:20+00:00 Ocean Kinetic Energy Backscatter Parametrization on Unstructured Grids: Impact on Global Eddy-Permitting Simulations Juricke, Stephan Danilov, Sergey Koldunov, Nikolay Oliver, Marcel Sidorenko, Dmitry 2020 https://doi.org/10.1029/2019MS001855 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9074 eng eng doi:10.1029/2019MS001855 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9074 This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. CC-BY ddc:551.46 ocean kinetic energy backscatter subgrid eddy parametrization inverse energy cascade viscosity closure eddy-permitting resolution doc-type:article 2020 ftsubggeo https://doi.org/10.1029/2019MS001855 2022-11-09T06:51:40Z In this study we demonstrate the potential of a kinetic energy backscatter scheme for use in global ocean simulations. Ocean models commonly employ (bi)harmonic eddy viscosities causing excessive dissipation of kinetic energy in eddy-permitting simulations. Overdissipation not only affects the smallest resolved scales but also the generation of eddies through baroclinic instabilities, impacting the entire wave number spectrum. The backscatter scheme returns part of this overdissipated energy back into the resolved flow. We employ backscatter in the FESOM2 multiresolution ocean model with a quasi-uniform 1/4° mesh. In multidecadal ocean simulations, backscatter increases eddy activity by a factor 2 or more, moving the simulation closer to observational estimates of sea surface height variability. Moreover, mean sea surface height, temperature, and salinity biases are reduced. This amounts to a globally averaged bias reduction of around 10% for each field, which is even larger in the Antarctic Circumpolar Current. However, in some regions such as the coastal Kuroshio, backscatter leads to a slight overenergizing of the flow and, in the Antarctic, to an unrealistic reduction of sea ice. Some of the bias increases can be reduced by a retuning of the model, and we suggest related adjustments to the backscatter scheme. The backscatter simulation is about 2.5 times as expensive as a simulation without backscatter. Most of the increased cost is due to a halving of the time step to accommodate higher simulated velocities. Article in Journal/Newspaper Antarc* Antarctic Sea ice GEO-LEOe-docs (FID GEO) Antarctic The Antarctic Journal of Advances in Modeling Earth Systems 12 1
spellingShingle ddc:551.46
ocean kinetic energy backscatter
subgrid eddy parametrization
inverse energy cascade
viscosity closure
eddy-permitting resolution
Juricke, Stephan
Danilov, Sergey
Koldunov, Nikolay
Oliver, Marcel
Sidorenko, Dmitry
Ocean Kinetic Energy Backscatter Parametrization on Unstructured Grids: Impact on Global Eddy-Permitting Simulations
title Ocean Kinetic Energy Backscatter Parametrization on Unstructured Grids: Impact on Global Eddy-Permitting Simulations
title_full Ocean Kinetic Energy Backscatter Parametrization on Unstructured Grids: Impact on Global Eddy-Permitting Simulations
title_fullStr Ocean Kinetic Energy Backscatter Parametrization on Unstructured Grids: Impact on Global Eddy-Permitting Simulations
title_full_unstemmed Ocean Kinetic Energy Backscatter Parametrization on Unstructured Grids: Impact on Global Eddy-Permitting Simulations
title_short Ocean Kinetic Energy Backscatter Parametrization on Unstructured Grids: Impact on Global Eddy-Permitting Simulations
title_sort ocean kinetic energy backscatter parametrization on unstructured grids: impact on global eddy-permitting simulations
topic ddc:551.46
ocean kinetic energy backscatter
subgrid eddy parametrization
inverse energy cascade
viscosity closure
eddy-permitting resolution
topic_facet ddc:551.46
ocean kinetic energy backscatter
subgrid eddy parametrization
inverse energy cascade
viscosity closure
eddy-permitting resolution
url https://doi.org/10.1029/2019MS001855
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9074