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Promotion of meridional overturning by Mediterranean-derived salt during the last deglaciation

Promotion of meridional overturning by Mediterranean-derived salt during the last deglaciation
Promotion of meridional overturning by Mediterranean-derived salt during the last deglaciation
We demonstrate that changes in the behavior of the Mediterranean Outflow Water (MOW) prior to and through the last deglaciation played an important role in promoting Meridional Overturning Circulation (MOC). Estimation of past MOW salt and heat fluxes indicates that they gradually increased through the last deglaciation. Between 17.5 and 14.6 thousand years ago (ka B.P., where B.P. references year 1950), net evaporation from the Mediterranean exported sufficient fresh water from the North Atlantic catchment to cause an average salinity increase of 0.5 psu throughout the upper 2000 m of the entire North Atlantic to the north of 25
last deglaciation, mediterranean outflow, salt export
0883-8305
PA4101-8pp.
Rogerson, M.
b044e358-2bac-4dd6-8224-661a752912c2
Rohling, E.J.
a2a27ef2-fcce-4c71-907b-e692b5ecc685
Weaver, P.P.E.
1ab10035-6132-46aa-8a5c-6fb23a1b8ab4
Rogerson, M.
b044e358-2bac-4dd6-8224-661a752912c2
Rohling, E.J.
a2a27ef2-fcce-4c71-907b-e692b5ecc685
Weaver, P.P.E.
1ab10035-6132-46aa-8a5c-6fb23a1b8ab4

Rogerson, M., Rohling, E.J. and Weaver, P.P.E. (2006) Promotion of meridional overturning by Mediterranean-derived salt during the last deglaciation. Paleoceanography, 21 (4), PA4101-8pp.. (doi:10.1029/2006PA001306).

Record type: Article

Abstract

We demonstrate that changes in the behavior of the Mediterranean Outflow Water (MOW) prior to and through the last deglaciation played an important role in promoting Meridional Overturning Circulation (MOC). Estimation of past MOW salt and heat fluxes indicates that they gradually increased through the last deglaciation. Between 17.5 and 14.6 thousand years ago (ka B.P., where B.P. references year 1950), net evaporation from the Mediterranean exported sufficient fresh water from the North Atlantic catchment to cause an average salinity increase of 0.5 psu throughout the upper 2000 m of the entire North Atlantic to the north of 25

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More information

Published date: November 2006
Keywords: last deglaciation, mediterranean outflow, salt export

Identifiers

Local EPrints ID: 42025
URI: http://eprints.soton.ac.uk/id/eprint/42025
ISSN: 0883-8305
PURE UUID: aa63dea8-ea87-4d21-ac92-b7702f303f74
ORCID for E.J. Rohling: ORCID iD orcid.org/0000-0001-5349-2158

Catalogue record

Date deposited: 07 Nov 2006
Last modified: 16 Mar 2024 02:46

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Contributors

Author: M. Rogerson
Author: E.J. Rohling ORCID iD
Author: P.P.E. Weaver

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