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• W2100069672 abstract "Research Article| October 01, 1999 Low-latitude forcing of meridional temperature and salinity gradients in the subpolar North Atlantic and the growth of glacial ice sheets Mark R. Chapman; Mark R. Chapman 1Godwin Laboratory, Department of Earth Sciences, University of Cambridge, Pembroke Street, Cambridge CB2 3SA, UK Search for other works by this author on: GSW Google Scholar Mark A. Maslin Mark A. Maslin 2Environmental Change Research Centre, Department of Geography, University College London, 26 Bedford Way, London WC1H 0AP, UK Search for other works by this author on: GSW Google Scholar Geology (1999) 27 (10): 875–878. https://doi.org/10.1130/0091-7613(1999)027<0875:LLFOMT>2.3.CO;2 Article history first online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Mark R. Chapman, Mark A. Maslin; Low-latitude forcing of meridional temperature and salinity gradients in the subpolar North Atlantic and the growth of glacial ice sheets. Geology 1999;; 27 (10): 875–878. doi: https://doi.org/10.1130/0091-7613(1999)027<0875:LLFOMT>2.3.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Sea-surface temperature (SST) and salinity (SSS) records obtained from two deep-sea cores have been used to reconstruct meridional gradients in the mid-latitude North Atlantic over the past 40 k.y. During the buildup of ice sheets toward the last glacial maximum, SST and SSS gradients between 40° and 50°N increased by 6–8 °C and ∼2‰, respectively. This trend represents a two-fold increase in surface-water gradients between 40 and 20 ka and strongly overprints the signal of high-frequency climatic oscillations. We attribute the gradual intensification of meridional SST and SSS gradients to a precession-driven increase in advection within the glacial North Atlantic Current resulting from changes in low-latitude insolation and seasonality. A strongly zonal ocean circulation pattern, maintained by greater advection and enhanced heat storage within the subtropical ocean at the last glacial maximum, persisted until ca. 20 ka, when a decrease in glacial SST gradients, coincident with a reduction in low-latitude climate forcing, marked the initiation of the last deglaciation. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2100069672 title "Low-latitude forcing of meridional temperature and salinity gradients in the subpolar North Atlantic and the growth of glacial ice sheets" @default.
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• W2100069672 doi "https://doi.org/10.1130/0091-7613(1999)027<0875:llfomt>2.3.co;2" @default.
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