Cookies

We use cookies to ensure that we give you the best experience on our website. You can change your cookie settings at any time. Otherwise, we'll assume you're OK to continue.


Durham Research Online
You are in:

Atlantic overturning circulation and Agulhas Leakage influences on SouthEast Atlantic upper ocean hydrography during Marine Isotope Stage 11.

Dickson, A.J. and Leng, M.J. and Maslin, M.A. and Sloane, H.J. and Green, J. and Bendle, J.A. and McClymont, E.L. and Pancost, R.D. (2010) 'Atlantic overturning circulation and Agulhas Leakage influences on SouthEast Atlantic upper ocean hydrography during Marine Isotope Stage 11.', Paleoceanography., 25 . PA3208.

Abstract

Climate dynamics during the marine isotope stage (MIS) 11 interglacial may provide information about how the climate system will evolve under the conditions of low-amplitude orbital forcing that are also found during the late Holocene. New stable isotope and alkenone data are presented from southeast Atlantic Ocean Drilling Program Site 1085, providing detailed information on interglacial climate evolution and the impacts of Atlantic meridional overturning circulation (MOC) and Agulhas leakage on the regional upper ocean hydrography. The data suggest that although warm surface ocean conditions were maintained at approximate Holocene levels for 40,000 years during MIS 11, subsurface temperature and salinity recorded by deeper-dwelling planktonic foraminifera species were maintained at their highest values for only 7000–8000 years. Surface water temperature and salinity data suggest that the interocean exchange of warm, salty waters into the southeast Atlantic Ocean was directly related to changes in the activity of the MOC during the study interval. Specifically, transient regional warming events during periods of weakened overturning circulation may have been amplified by the continuous interocean exchange of warm, salty Indian Ocean waters that primed the MOC for abrupt resumptions into a vigorous mode of operation. Conversely, a peak in interocean exchange at the end of the MIS 11 interglacial optimum may reflect enhanced trade wind forcing of surface waters whose export to the North Atlantic Ocean could have contributed to renewed ice sheet buildup during the MIS 11 to 10 glacial inception.

Item Type:Article
Full text:PDF - Published Version (997Kb)
Status:Peer-reviewed
Publisher Web site:http://dx.doi.org/10.1029/2009PA001830
Publisher statement:©2010 American Geophysical Union. Dickson, A.J. and Leng, M.J. and Maslin, M.A. and Sloane, H.J. and Green, J. and Bendle, J.A. and McClymont, E.L. and Pancost, R.D. (2010) 'Atlantic overturning circulation and Agulhas Leakage influences on SouthEast Atlantic upper ocean hydrography during Marine Isotope Stage 11.', Paleoceanography., 25 . PA3208, 10.1029/2009PA001830. To view the published open abstract, go to http://dx.doi.org and enter the DOI.
Record Created:11 Nov 2011 15:50
Last Modified:15 Nov 2011 11:15

Social bookmarking: del.icio.usConnoteaBibSonomyCiteULikeFacebookTwitterExport: EndNote, Zotero | BibTex
Usage statisticsLook up in GoogleScholar | Find in a UK Library