A Kinematic Kinetic Energy Backscatter Parametrization: From Implementation to Global Ocean Simulations

Abstract Ocean models at eddy‐permitting resolution are generally overdissipative, damping the intensity of the mesoscale eddy field. To reduce overdissipation, we propose a simplified, kinematic energy backscatter parametrization built into the viscosity operator in conjunction with a new flow‐depe...

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Main Authors: S. Juricke, S. Danilov, N. Koldunov, M. Oliver, D. V. Sein, D. Sidorenko, Q. Wang
Format: Article
Language:English
Published: American Geophysical Union (AGU) 2020-12-01
Series:Journal of Advances in Modeling Earth Systems
Subjects:
Online Access:https://doi.org/10.1029/2020MS002175
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spelling doaj-cf765c74416b485482fcceeb2f3717e02021-02-10T19:50:18ZengAmerican Geophysical Union (AGU)Journal of Advances in Modeling Earth Systems1942-24662020-12-011212n/an/a10.1029/2020MS002175A Kinematic Kinetic Energy Backscatter Parametrization: From Implementation to Global Ocean SimulationsS. Juricke0S. Danilov1N. Koldunov2M. Oliver3D. V. Sein4D. Sidorenko5Q. Wang6Department of Mathematics & Logistics Jacobs University Bremen GermanyDepartment of Mathematics & Logistics Jacobs University Bremen GermanyAlfred Wegener Institute for Polar and Marine Research Bremerhaven GermanyDepartment of Mathematics & Logistics Jacobs University Bremen GermanyAlfred Wegener Institute for Polar and Marine Research Bremerhaven GermanyAlfred Wegener Institute for Polar and Marine Research Bremerhaven GermanyAlfred Wegener Institute for Polar and Marine Research Bremerhaven GermanyAbstract Ocean models at eddy‐permitting resolution are generally overdissipative, damping the intensity of the mesoscale eddy field. To reduce overdissipation, we propose a simplified, kinematic energy backscatter parametrization built into the viscosity operator in conjunction with a new flow‐dependent coefficient of viscosity based on nearest neighbor velocity differences. The new scheme mitigates excessive dissipation of energy and improves global ocean simulations at eddy‐permitting resolution. We find that kinematic backscatter substantially raises simulated eddy kinetic energy, similar to an alternative, previously proposed dynamic backscatter parametrization. While dynamic backscatter is scale‐aware and energetically more consistent, its implementation is more complex. Furthermore, it turns out to be computationally more expensive, as it applies, among other things, an additional prognostic subgrid energy equation. The kinematic backscatter proposed here, by contrast, comes at no additional computational cost, following the principle of simplicity. Our primary focus is the discretization on triangular unstructured meshes with cell placement of velocities (an analog of B‐grids), as employed by the Finite‐volumE Sea ice‐Ocean Model (FESOM2). The kinematic backscatter scheme with the new viscosity coefficient is implemented in FESOM2 and tested in the simplified geometry of a zonally reentrant channel as well as in a global ocean simulation on a 1/4° mesh. This first version of the new kinematic backscatter needs to be tuned to the specific resolution regime of the simulation. However, the tuning relies on a single parameter, emphasizing the overall practicality of the approach.https://doi.org/10.1029/2020MS002175kinetic energy backscatterviscosity closuresmesoscale eddiesocean modelingeddy‐permitting resolutionoverdissipation
collection DOAJ
language English
format Article
sources DOAJ
author S. Juricke
S. Danilov
N. Koldunov
M. Oliver
D. V. Sein
D. Sidorenko
Q. Wang
spellingShingle S. Juricke
S. Danilov
N. Koldunov
M. Oliver
D. V. Sein
D. Sidorenko
Q. Wang
A Kinematic Kinetic Energy Backscatter Parametrization: From Implementation to Global Ocean Simulations
Journal of Advances in Modeling Earth Systems
kinetic energy backscatter
viscosity closures
mesoscale eddies
ocean modeling
eddy‐permitting resolution
overdissipation
author_facet S. Juricke
S. Danilov
N. Koldunov
M. Oliver
D. V. Sein
D. Sidorenko
Q. Wang
author_sort S. Juricke
title A Kinematic Kinetic Energy Backscatter Parametrization: From Implementation to Global Ocean Simulations
title_short A Kinematic Kinetic Energy Backscatter Parametrization: From Implementation to Global Ocean Simulations
title_full A Kinematic Kinetic Energy Backscatter Parametrization: From Implementation to Global Ocean Simulations
title_fullStr A Kinematic Kinetic Energy Backscatter Parametrization: From Implementation to Global Ocean Simulations
title_full_unstemmed A Kinematic Kinetic Energy Backscatter Parametrization: From Implementation to Global Ocean Simulations
title_sort kinematic kinetic energy backscatter parametrization: from implementation to global ocean simulations
publisher American Geophysical Union (AGU)
series Journal of Advances in Modeling Earth Systems
issn 1942-2466
publishDate 2020-12-01
description Abstract Ocean models at eddy‐permitting resolution are generally overdissipative, damping the intensity of the mesoscale eddy field. To reduce overdissipation, we propose a simplified, kinematic energy backscatter parametrization built into the viscosity operator in conjunction with a new flow‐dependent coefficient of viscosity based on nearest neighbor velocity differences. The new scheme mitigates excessive dissipation of energy and improves global ocean simulations at eddy‐permitting resolution. We find that kinematic backscatter substantially raises simulated eddy kinetic energy, similar to an alternative, previously proposed dynamic backscatter parametrization. While dynamic backscatter is scale‐aware and energetically more consistent, its implementation is more complex. Furthermore, it turns out to be computationally more expensive, as it applies, among other things, an additional prognostic subgrid energy equation. The kinematic backscatter proposed here, by contrast, comes at no additional computational cost, following the principle of simplicity. Our primary focus is the discretization on triangular unstructured meshes with cell placement of velocities (an analog of B‐grids), as employed by the Finite‐volumE Sea ice‐Ocean Model (FESOM2). The kinematic backscatter scheme with the new viscosity coefficient is implemented in FESOM2 and tested in the simplified geometry of a zonally reentrant channel as well as in a global ocean simulation on a 1/4° mesh. This first version of the new kinematic backscatter needs to be tuned to the specific resolution regime of the simulation. However, the tuning relies on a single parameter, emphasizing the overall practicality of the approach.
topic kinetic energy backscatter
viscosity closures
mesoscale eddies
ocean modeling
eddy‐permitting resolution
overdissipation
url https://doi.org/10.1029/2020MS002175
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