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Towards a parametrization of river discharges into ocean general circulation models: a closure through energy conservation

Towards a parametrization of river discharges into ocean general circulation models: a closure through energy conservation
Towards a parametrization of river discharges into ocean general circulation models: a closure through energy conservation
Diagnostic methods are defined in order to compare two numerical simulations of ocean dynamics in a region of freshwater influence. The first one is a river plume simulation based on a high resolution numerical configuration of the POM coastal ocean model in which mixing parametrizations have been previously defined. The second one is a simulation based on the NEMO Global Ocean Model used for climate simulations in its half-a-degree configuration in which a river inflow is represented as precipitation on two coastal grid cells. Both simulations are forced with the same freshwater inflows and wind stresses. The divergence of volumetric fluxes above and below the halocline are compared. Results show that when an upwelling wind blows, the two models display similar behavior although the impact of lack of precision can be observed in the NEMO configuration. When a downwelling wind blows, the NEMO Global Ocean configuration can not reproduce the coastally trapped baroclinic dynamics because its grid resolution is too coarse. To find a parametrization to help represent these dynamics in ocean general circulation models, a method based on energy conservation is investigated. This method shows that it is possible to link the energy fluxes provided by river inflows to the divergence of energy fluxes integrated over the grid cells of ocean general circulation models. A parametrization of the dynamics created by freshwater inflows is deduced from this method. This enabled creation of a box model that proved to have the same behavior as the fluxes previously computed from the high resolution configuration.
River inflows, Freshwater plumes, OGCMs, Subgrid-scale, Energy conservation
0930-7575
891-908
Hordoir, R.
fbb1a7cb-7daf-4693-b3e0-41e322aa9aad
Polcher, J.
74c10aa8-30cd-44b1-b28d-32f3ba87502f
Brun-Cottan, J-C.
f112b522-2b3b-4c75-83d7-aff98b023fe9
Madec, G.
7e2ec04b-896a-4861-b2d0-b74f39d748c2
Hordoir, R.
fbb1a7cb-7daf-4693-b3e0-41e322aa9aad
Polcher, J.
74c10aa8-30cd-44b1-b28d-32f3ba87502f
Brun-Cottan, J-C.
f112b522-2b3b-4c75-83d7-aff98b023fe9
Madec, G.
7e2ec04b-896a-4861-b2d0-b74f39d748c2

Hordoir, R., Polcher, J., Brun-Cottan, J-C. and Madec, G. (2008) Towards a parametrization of river discharges into ocean general circulation models: a closure through energy conservation. Climate Dynamics, 31 (7-8), 891-908. (doi:10.1007/s00382-008-0416-4).

Record type: Article

Abstract

Diagnostic methods are defined in order to compare two numerical simulations of ocean dynamics in a region of freshwater influence. The first one is a river plume simulation based on a high resolution numerical configuration of the POM coastal ocean model in which mixing parametrizations have been previously defined. The second one is a simulation based on the NEMO Global Ocean Model used for climate simulations in its half-a-degree configuration in which a river inflow is represented as precipitation on two coastal grid cells. Both simulations are forced with the same freshwater inflows and wind stresses. The divergence of volumetric fluxes above and below the halocline are compared. Results show that when an upwelling wind blows, the two models display similar behavior although the impact of lack of precision can be observed in the NEMO configuration. When a downwelling wind blows, the NEMO Global Ocean configuration can not reproduce the coastally trapped baroclinic dynamics because its grid resolution is too coarse. To find a parametrization to help represent these dynamics in ocean general circulation models, a method based on energy conservation is investigated. This method shows that it is possible to link the energy fluxes provided by river inflows to the divergence of energy fluxes integrated over the grid cells of ocean general circulation models. A parametrization of the dynamics created by freshwater inflows is deduced from this method. This enabled creation of a box model that proved to have the same behavior as the fluxes previously computed from the high resolution configuration.

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More information

Published date: December 2008
Additional Information: Electronic supplementary material The online version of this article (doi:10.1007/s00382-008-0416-4) contains supplementary material, which is available to authorized users.
Keywords: River inflows, Freshwater plumes, OGCMs, Subgrid-scale, Energy conservation

Identifiers

Local EPrints ID: 64318
URI: http://eprints.soton.ac.uk/id/eprint/64318
ISSN: 0930-7575
PURE UUID: 1081e48c-c0a3-463e-b2ed-b967f1a31ad1

Catalogue record

Date deposited: 09 Dec 2008
Last modified: 15 Mar 2024 11:48

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Contributors

Author: R. Hordoir
Author: J. Polcher
Author: J-C. Brun-Cottan
Author: G. Madec

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