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From centennial to millennial oscillation of the thermohaline circulation

From centennial to millennial oscillation of the thermohaline circulation
From centennial to millennial oscillation of the thermohaline circulation
The freshwater flux intensity is used as the main control parameter to destabilize the ThermoHaline
Circulation (THC): as it increases, the classical bifurcation scenario, thermal stable steady state, millennial oscillation and haline stable steady state are reproduced in a 2D zonally-averaged ocean model under mixed boundary conditions. Both bifurcations arise through global bifurcations leading to an infinite period of the limit cycle. Here we highlight a centennial oscillation important for the instability of the thermal phase of the millennial oscillation and which could be considered as a precursor to the collapse of the THC. It is suggested that the existence or the absence of this centennial oscillation leads to dramatic changes in the collapse time scale of the THC going from several thousand years to only a few decades. This bifurcation scenario is shown to be sensitive to the value of the dissipation.
0022-2402
723-742
Sévellec, Florian
01569d6c-65b0-4270-af2a-35b0a77c9140
Huck, Thierry
3de8511b-db7b-4ed1-bc27-92d2bbc7c6b9
de Verdière, Alain Colin
b3372448-3b63-41da-b1c1-526157f7e627
Sévellec, Florian
01569d6c-65b0-4270-af2a-35b0a77c9140
Huck, Thierry
3de8511b-db7b-4ed1-bc27-92d2bbc7c6b9
de Verdière, Alain Colin
b3372448-3b63-41da-b1c1-526157f7e627

Sévellec, Florian, Huck, Thierry and de Verdière, Alain Colin (2010) From centennial to millennial oscillation of the thermohaline circulation. Journal of Marine Research, 68 (5), 723-742. (doi:10.1357/002224011795977635).

Record type: Article

Abstract

The freshwater flux intensity is used as the main control parameter to destabilize the ThermoHaline
Circulation (THC): as it increases, the classical bifurcation scenario, thermal stable steady state, millennial oscillation and haline stable steady state are reproduced in a 2D zonally-averaged ocean model under mixed boundary conditions. Both bifurcations arise through global bifurcations leading to an infinite period of the limit cycle. Here we highlight a centennial oscillation important for the instability of the thermal phase of the millennial oscillation and which could be considered as a precursor to the collapse of the THC. It is suggested that the existence or the absence of this centennial oscillation leads to dramatic changes in the collapse time scale of the THC going from several thousand years to only a few decades. This bifurcation scenario is shown to be sensitive to the value of the dissipation.

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Published date: September 2010
Organisations: Physical Oceanography

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Local EPrints ID: 339739
URI: http://eprints.soton.ac.uk/id/eprint/339739
ISSN: 0022-2402
PURE UUID: ae281d41-61a3-4daf-ab49-18c5500fa74e

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Date deposited: 29 May 2012 16:10
Last modified: 14 Mar 2024 11:14

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Contributors

Author: Thierry Huck
Author: Alain Colin de Verdière

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