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Persistent link between solar activity and Greenland climate during the Last Glacial Maximum
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2014 (English)In: Nature Geoscience, ISSN 1752-0894, E-ISSN 1752-0908, Vol. 7, no 9, 662-666 p.Article in journal (Refereed) Published
Abstract [en]

Changes in solar activity have previously been proposed to cause decadal- to millennial-scale fluctuations in both the modern and Holocene climates(1). Direct observational records of solar activity, such as sunspot numbers, exist for only the past few hundred years, so solar variability for earlier periods is typically reconstructed from measurements of cosmogenic radionuclides such as Be-10 and C-14 from ice cores and tree rings(2,3). Here we present a high-resolution Be-10 record from the ice core collected from central Greenland by the Greenland Ice Core Project (GRIP). The record spans from 22,500 to 10,000 years ago, and is based on new and compiled data(4-6). Using C-14 records(7,8) to control for climate-related influences on Be-10 deposition, we reconstruct centennial changes in solar activity. We find that during the Last Glacial Maximum, solar minima correlate with more negative delta O-18 values of ice and are accompanied by increased snow accumulation and sea-salt input over central Greenland. We suggest that solar minima could have induced changes in the stratosphere that favour the development of high-pressure blocking systems located to the south of Greenland, as has been found in observations and model simulations for recent climate(9,10). We conclude that the mechanism behind solar forcing of regional climate change may have been similar under both modern and Last Glacial Maximum climate conditions.

Place, publisher, year, edition, pages
2014. Vol. 7, no 9, 662-666 p.
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Geology
Identifiers
URN: urn:nbn:se:uu:diva-234176DOI: 10.1038/NGEO2225ISI: 000341635600015OAI: oai:DiVA.org:uu-234176DiVA: diva2:755805
Funder
Swedish Research Council, 2013-8421
Available from: 2014-10-15 Created: 2014-10-14 Last updated: 2017-12-05Bibliographically approved

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Possnert, Göran

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