The Influence of a near-bottom Transport Parameterization on the Sensitivity of the Thermohaline Circulation

The effect of a near bottom transport scheme on the sensitivity of the thermohaline circulation is analyzed in a coupled model. In this model with idealized geometry of the Atlantic, it is shown that in the presence of a northern source of deep water, an accurate representation of the overflow proce...

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Main Author: Gerrit Lohmann
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.22.4773
http://www.mpimet.mpg.de/~lohmann.gerrit/./PSFILES/paper_over.ps
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.22.4773 2023-05-15T17:31:44+02:00 The Influence of a near-bottom Transport Parameterization on the Sensitivity of the Thermohaline Circulation Gerrit Lohmann The Pennsylvania State University CiteSeerX Archives application/postscript http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.22.4773 http://www.mpimet.mpg.de/~lohmann.gerrit/./PSFILES/paper_over.ps en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.22.4773 http://www.mpimet.mpg.de/~lohmann.gerrit/./PSFILES/paper_over.ps Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.mpimet.mpg.de/~lohmann.gerrit/./PSFILES/paper_over.ps text ftciteseerx 2016-01-07T18:14:38Z The effect of a near bottom transport scheme on the sensitivity of the thermohaline circulation is analyzed in a coupled model. In this model with idealized geometry of the Atlantic, it is shown that in the presence of a northern source of deep water, an accurate representation of the overflow process has a stabilizing effect on the thermohaline circulation for subpolar sea surface salinity perturbations. The large scale overturning circulation can be maintained in the presence of a continued deep water formation north of the sill. Experiments suggest that without a sufficient coupling across a sill in the northern North Atlantic, the response of the ocean's circulation to subpolar atmospheric variability may be too strong. 1 Text North Atlantic Unknown
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description The effect of a near bottom transport scheme on the sensitivity of the thermohaline circulation is analyzed in a coupled model. In this model with idealized geometry of the Atlantic, it is shown that in the presence of a northern source of deep water, an accurate representation of the overflow process has a stabilizing effect on the thermohaline circulation for subpolar sea surface salinity perturbations. The large scale overturning circulation can be maintained in the presence of a continued deep water formation north of the sill. Experiments suggest that without a sufficient coupling across a sill in the northern North Atlantic, the response of the ocean's circulation to subpolar atmospheric variability may be too strong. 1
author2 The Pennsylvania State University CiteSeerX Archives
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author Gerrit Lohmann
spellingShingle Gerrit Lohmann
The Influence of a near-bottom Transport Parameterization on the Sensitivity of the Thermohaline Circulation
author_facet Gerrit Lohmann
author_sort Gerrit Lohmann
title The Influence of a near-bottom Transport Parameterization on the Sensitivity of the Thermohaline Circulation
title_short The Influence of a near-bottom Transport Parameterization on the Sensitivity of the Thermohaline Circulation
title_full The Influence of a near-bottom Transport Parameterization on the Sensitivity of the Thermohaline Circulation
title_fullStr The Influence of a near-bottom Transport Parameterization on the Sensitivity of the Thermohaline Circulation
title_full_unstemmed The Influence of a near-bottom Transport Parameterization on the Sensitivity of the Thermohaline Circulation
title_sort influence of a near-bottom transport parameterization on the sensitivity of the thermohaline circulation
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.22.4773
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