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Is the thermohaline circulation changing?

Is the thermohaline circulation changing?
Is the thermohaline circulation changing?
Analyses of ocean observations and model simulations suggest that there have been considerable changes in the thermohaline circulation (THC) during the last century. These changes are likely to be the result of natural multidecadal climate variability and are driven by low-frequency variations of the North Atlantic Oscillation (NAO) through changes in Labrador Sea convection. Indications of a sustained THC weakening are not seen during the last few decades. Instead, a strengthening since the 1980s is observed. The combined assessment of ocean hydrography data and model results indicates that the expected anthropogenic weakening of the THC will remain within the range of natural variability during the next several decades.
0894-8755
4631-4637
Latif, M.
d1729715-2cf5-457f-84a8-75978399e42a
Böning, C.
1a5ca782-5209-44d8-9ffe-11e04f0576ec
Willebrand, J.
cc3a87d9-467f-4bc4-8d35-dbc97ee5f8be
Biastoch, A.
fa7df768-2a47-4071-aafc-30f36910def8
Dengg, J.
8980e0c2-8c60-4986-af69-0e254cc6ce79
Keenlyside, N.
f27d222a-76c0-4ebc-b93e-c16c986cec8c
Schweckendiek, U.
afd437d2-55ee-4370-bfcd-c7e5a62e7119
Madec, G.
7e2ec04b-896a-4861-b2d0-b74f39d748c2
Latif, M.
d1729715-2cf5-457f-84a8-75978399e42a
Böning, C.
1a5ca782-5209-44d8-9ffe-11e04f0576ec
Willebrand, J.
cc3a87d9-467f-4bc4-8d35-dbc97ee5f8be
Biastoch, A.
fa7df768-2a47-4071-aafc-30f36910def8
Dengg, J.
8980e0c2-8c60-4986-af69-0e254cc6ce79
Keenlyside, N.
f27d222a-76c0-4ebc-b93e-c16c986cec8c
Schweckendiek, U.
afd437d2-55ee-4370-bfcd-c7e5a62e7119
Madec, G.
7e2ec04b-896a-4861-b2d0-b74f39d748c2

Latif, M., Böning, C., Willebrand, J., Biastoch, A., Dengg, J., Keenlyside, N., Schweckendiek, U. and Madec, G. (2006) Is the thermohaline circulation changing? Journal of Climate, 19 (18), 4631-4637. (doi:10.1175/JCLI3876.1).

Record type: Article

Abstract

Analyses of ocean observations and model simulations suggest that there have been considerable changes in the thermohaline circulation (THC) during the last century. These changes are likely to be the result of natural multidecadal climate variability and are driven by low-frequency variations of the North Atlantic Oscillation (NAO) through changes in Labrador Sea convection. Indications of a sustained THC weakening are not seen during the last few decades. Instead, a strengthening since the 1980s is observed. The combined assessment of ocean hydrography data and model results indicates that the expected anthropogenic weakening of the THC will remain within the range of natural variability during the next several decades.

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Published date: September 2006

Identifiers

Local EPrints ID: 64359
URI: http://eprints.soton.ac.uk/id/eprint/64359
ISSN: 0894-8755
PURE UUID: 83d6063a-40ae-4f05-9a88-1363a2f6f399

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Date deposited: 10 Dec 2008
Last modified: 15 Mar 2024 11:48

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Contributors

Author: M. Latif
Author: C. Böning
Author: J. Willebrand
Author: A. Biastoch
Author: J. Dengg
Author: N. Keenlyside
Author: U. Schweckendiek
Author: G. Madec

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