Abstract
Research Article| March 01, 2015 Solar forcing of Holocene summer sea-surface temperatures in the northern North Atlantic Hui Jiang; Hui Jiang * 1Key Laboratory of Geographic Information Science and State Key Laboratory of Estuarine and Coastal Research, East China Normal University, 200062 Shanghai, People’s Republic of China *E-mails: hjiang@geo.ecnu.edu.cn; raimund.muscheler@geol.lu.se Search for other works by this author on: GSW Google Scholar Raimund Muscheler; Raimund Muscheler * 2Department of Geology, Quaternary Sciences, Lund University, Sölvegatan 12, 22362 Lund, Sweden *E-mails: hjiang@geo.ecnu.edu.cn; raimund.muscheler@geol.lu.se Search for other works by this author on: GSW Google Scholar Svante Björck; Svante Björck 2Department of Geology, Quaternary Sciences, Lund University, Sölvegatan 12, 22362 Lund, Sweden Search for other works by this author on: GSW Google Scholar Marit-Solveig Seidenkrantz; Marit-Solveig Seidenkrantz 3Centre for Past Climate Studies and Arctic Research Centre, Department of Geoscience, Aarhus University, DK-8000 Aarhus C, Denmark Search for other works by this author on: GSW Google Scholar Jesper Olsen; Jesper Olsen 4Department of Physics and Astronomy, Aarhus University, DK-8000 Aarhus C, Denmark Search for other works by this author on: GSW Google Scholar Longbin Sha; Longbin Sha 1Key Laboratory of Geographic Information Science and State Key Laboratory of Estuarine and Coastal Research, East China Normal University, 200062 Shanghai, People’s Republic of China3Centre for Past Climate Studies and Arctic Research Centre, Department of Geoscience, Aarhus University, DK-8000 Aarhus C, Denmark Search for other works by this author on: GSW Google Scholar Jesper Sjolte; Jesper Sjolte 2Department of Geology, Quaternary Sciences, Lund University, Sölvegatan 12, 22362 Lund, Sweden Search for other works by this author on: GSW Google Scholar Jón Eiríksson; Jón Eiríksson 5Institute of Earth Science, University of Iceland, Askja, IS-101-Reykjavík, Iceland Search for other works by this author on: GSW Google Scholar Lihua Ran; Lihua Ran 6Second Institute of Oceanography, State Oceanic Administration, 310012 Hangzhou, People’s Republic of China Search for other works by this author on: GSW Google Scholar Karen-Luise Knudsen; Karen-Luise Knudsen 3Centre for Past Climate Studies and Arctic Research Centre, Department of Geoscience, Aarhus University, DK-8000 Aarhus C, Denmark Search for other works by this author on: GSW Google Scholar Mads F. Knudsen Mads F. Knudsen 3Centre for Past Climate Studies and Arctic Research Centre, Department of Geoscience, Aarhus University, DK-8000 Aarhus C, Denmark Search for other works by this author on: GSW Google Scholar Geology (2015) 43 (3): 203–206. https://doi.org/10.1130/G36377.1 Article history received: 21 Oct 2014 rev-recd: 09 Dec 2014 accepted: 10 Dec 2014 first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Hui Jiang, Raimund Muscheler, Svante Björck, Marit-Solveig Seidenkrantz, Jesper Olsen, Longbin Sha, Jesper Sjolte, Jón Eiríksson, Lihua Ran, Karen-Luise Knudsen, Mads F. Knudsen; Solar forcing of Holocene summer sea-surface temperatures in the northern North Atlantic. Geology 2015;; 43 (3): 203–206. doi: https://doi.org/10.1130/G36377.1 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 Mounting evidence from proxy records suggests that variations in solar activity have played a significant role in triggering past climate changes. However, the mechanisms for sun-climate links remain a topic of debate. Here we present a high-resolution summer sea-surface temperature (SST) record covering the past 9300 yr from a site located at the present-day boundary between polar and Atlantic surface-water masses. The record is age constrained via the identification of 15 independently dated tephra markers from terrestrial archives, circumventing marine reservoir age variability problems. Our results indicate a close link between solar activity and SSTs in the northern North Atlantic during the past 4000 yr; they suggest that the climate system in this area is more susceptible to the influence of solar variations during cool periods with less vigorous ocean circulation. Furthermore, the high-resolution SST record indicates that climate in the North Atlantic regions follows solar activity variations on multidecadal to centennial time scales. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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