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

Abstract 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...

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Published in:Journal of Advances in Modeling Earth Systems
Main Authors: Stephan Juricke, Sergey Danilov, Nikolay Koldunov, Marcel Oliver, Dmitry Sidorenko
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU) 2020
Subjects:
Online Access:https://doi.org/10.1029/2019MS001855
https://doaj.org/article/3b05bcc09609423cbe1498e6b9fc5d55
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spelling ftdoajarticles:oai:doaj.org/article:3b05bcc09609423cbe1498e6b9fc5d55 2023-05-15T13:38:16+02:00 Ocean Kinetic Energy Backscatter Parametrization on Unstructured Grids: Impact on Global Eddy‐Permitting Simulations Stephan Juricke Sergey Danilov Nikolay Koldunov Marcel Oliver Dmitry Sidorenko 2020-01-01T00:00:00Z https://doi.org/10.1029/2019MS001855 https://doaj.org/article/3b05bcc09609423cbe1498e6b9fc5d55 EN eng American Geophysical Union (AGU) https://doi.org/10.1029/2019MS001855 https://doaj.org/toc/1942-2466 1942-2466 doi:10.1029/2019MS001855 https://doaj.org/article/3b05bcc09609423cbe1498e6b9fc5d55 Journal of Advances in Modeling Earth Systems, Vol 12, Iss 1, Pp n/a-n/a (2020) ocean kinetic energy backscatter subgrid eddy parametrization inverse energy cascade viscosity closure eddy‐permitting resolution Physical geography GB3-5030 Oceanography GC1-1581 article 2020 ftdoajarticles https://doi.org/10.1029/2019MS001855 2022-12-31T05:32:27Z Abstract 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 Directory of Open Access Journals: DOAJ Articles Antarctic The Antarctic Journal of Advances in Modeling Earth Systems 12 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic ocean kinetic energy backscatter
subgrid eddy parametrization
inverse energy cascade
viscosity closure
eddy‐permitting resolution
Physical geography
GB3-5030
Oceanography
GC1-1581
spellingShingle ocean kinetic energy backscatter
subgrid eddy parametrization
inverse energy cascade
viscosity closure
eddy‐permitting resolution
Physical geography
GB3-5030
Oceanography
GC1-1581
Stephan Juricke
Sergey Danilov
Nikolay Koldunov
Marcel Oliver
Dmitry Sidorenko
Ocean Kinetic Energy Backscatter Parametrization on Unstructured Grids: Impact on Global Eddy‐Permitting Simulations
topic_facet ocean kinetic energy backscatter
subgrid eddy parametrization
inverse energy cascade
viscosity closure
eddy‐permitting resolution
Physical geography
GB3-5030
Oceanography
GC1-1581
description Abstract 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
author Stephan Juricke
Sergey Danilov
Nikolay Koldunov
Marcel Oliver
Dmitry Sidorenko
author_facet Stephan Juricke
Sergey Danilov
Nikolay Koldunov
Marcel Oliver
Dmitry Sidorenko
author_sort Stephan Juricke
title 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_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_sort ocean kinetic energy backscatter parametrization on unstructured grids: impact on global eddy‐permitting simulations
publisher American Geophysical Union (AGU)
publishDate 2020
url https://doi.org/10.1029/2019MS001855
https://doaj.org/article/3b05bcc09609423cbe1498e6b9fc5d55
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Sea ice
genre_facet Antarc*
Antarctic
Sea ice
op_source Journal of Advances in Modeling Earth Systems, Vol 12, Iss 1, Pp n/a-n/a (2020)
op_relation https://doi.org/10.1029/2019MS001855
https://doaj.org/toc/1942-2466
1942-2466
doi:10.1029/2019MS001855
https://doaj.org/article/3b05bcc09609423cbe1498e6b9fc5d55
op_doi https://doi.org/10.1029/2019MS001855
container_title Journal of Advances in Modeling Earth Systems
container_volume 12
container_issue 1
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