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How momentum advection schemes influence current-topography interactions at eddy permitting resolution

How momentum advection schemes influence current-topography interactions at eddy permitting resolution
How momentum advection schemes influence current-topography interactions at eddy permitting resolution
Recent studies have shown that the use of an enstrophy-and-energy-conserving momentum advection scheme substantially reduces widespread biases of mean currents in the global 1/4° DRAKKAR model. This paper investigates the origin of these improvements. A series of sensitivity simulations with different momentum advection schemes is performed with the North Atlantic 1/4° DRAKKAR model. Three second order momentum advection schemes conserving, respectively, enstrophy (ens), energy (efx) and both quantities (een) are tested and their impact on the model solution are compared.
The mean kinetic energy vertical profile is found to change up to 10% depending on the chosen scheme. This sensitivity is maximum in bottom layers. The analysis of the vorticity tendency due to horizontal momentum advection reveals that the three schemes differ mostly in bottom layers as well. The average magnitude of this term is enhanced with the efx scheme and reduced with the een scheme. These differences are found to be consistent with the instantaneous tendency of each scheme.
In addition, we show that the differences between the schemes are related to the grid-scale irregularity of the velocity field. Both the grid scale irregularity and the differences between the schemes are found to be enhanced in bottom layers. We conclude that the model solution depends crucially on the ability of the momentum advection scheme to handle under-resolved flows close to the bottom topography. This work emphasizes the critical influence of topography in eddy-active regions on mean circulation features such as the position of the North-Atlantic current or the Gulf Stream separation.
Momentum advection schemes, Topography, z-level models
1463-5003
1-14
Le Sommer, Julien
d442f04e-83e5-4818-a148-eeca9cb4e36a
Penduff, Thierry
8b85eadc-4bb4-436a-a58a-9b2e279363bc
Theetten, Sébastien
1e869f79-df2c-44f7-b7bb-61e03f5aeb23
Madec, Gurvan
ffb28deb-4bbd-4a4c-914f-492f813e4864
Barnier, Bernard
af67a33e-f7c3-4681-b37b-1fbebf74983a
Le Sommer, Julien
d442f04e-83e5-4818-a148-eeca9cb4e36a
Penduff, Thierry
8b85eadc-4bb4-436a-a58a-9b2e279363bc
Theetten, Sébastien
1e869f79-df2c-44f7-b7bb-61e03f5aeb23
Madec, Gurvan
ffb28deb-4bbd-4a4c-914f-492f813e4864
Barnier, Bernard
af67a33e-f7c3-4681-b37b-1fbebf74983a

Le Sommer, Julien, Penduff, Thierry, Theetten, Sébastien, Madec, Gurvan and Barnier, Bernard (2009) How momentum advection schemes influence current-topography interactions at eddy permitting resolution. Ocean Modelling, 29 (1), 1-14. (doi:10.1016/j.ocemod.2008.11.007).

Record type: Article

Abstract

Recent studies have shown that the use of an enstrophy-and-energy-conserving momentum advection scheme substantially reduces widespread biases of mean currents in the global 1/4° DRAKKAR model. This paper investigates the origin of these improvements. A series of sensitivity simulations with different momentum advection schemes is performed with the North Atlantic 1/4° DRAKKAR model. Three second order momentum advection schemes conserving, respectively, enstrophy (ens), energy (efx) and both quantities (een) are tested and their impact on the model solution are compared.
The mean kinetic energy vertical profile is found to change up to 10% depending on the chosen scheme. This sensitivity is maximum in bottom layers. The analysis of the vorticity tendency due to horizontal momentum advection reveals that the three schemes differ mostly in bottom layers as well. The average magnitude of this term is enhanced with the efx scheme and reduced with the een scheme. These differences are found to be consistent with the instantaneous tendency of each scheme.
In addition, we show that the differences between the schemes are related to the grid-scale irregularity of the velocity field. Both the grid scale irregularity and the differences between the schemes are found to be enhanced in bottom layers. We conclude that the model solution depends crucially on the ability of the momentum advection scheme to handle under-resolved flows close to the bottom topography. This work emphasizes the critical influence of topography in eddy-active regions on mean circulation features such as the position of the North-Atlantic current or the Gulf Stream separation.

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More information

Published date: 2009
Keywords: Momentum advection schemes, Topography, z-level models

Identifiers

Local EPrints ID: 66223
URI: http://eprints.soton.ac.uk/id/eprint/66223
ISSN: 1463-5003
PURE UUID: 434c0766-73d9-48ed-a6d4-dbdf01b79a26

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Date deposited: 14 May 2009
Last modified: 13 Mar 2024 18:11

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Contributors

Author: Julien Le Sommer
Author: Thierry Penduff
Author: Sébastien Theetten
Author: Gurvan Madec
Author: Bernard Barnier

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