Solar forcing has been invoked to explain persistent, millennial-scale climate variations during the Holocene. Two climate reconstructions, one based on sea-ice drift and one on North Atlantic storminess, call this link into question.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 12 print issues and online access
$259.00 per year
only $21.58 per issue
Rent or buy this article
Prices vary by article type
from$1.95
to$39.95
Prices may be subject to local taxes which are calculated during checkout
References
Bond, G. et al. Science 294, 2130–2136 (2001).
Sorrel, P. et al. Nature Geosci. 5, http://dx.doi.org/10.1038/ngeo1619 (2012).
Darby, D. A., Ortiz, J. D., Grosch, C. E. & Lund, S. P. Nature Geosci. 5, http://dx.doi.org/10.1038/ngeo1629 (2012).
Thompson, D. W. J., Wallace, J. M. & Hegerl, G. C. J. Clim. 13, 1018–1036 (2000).
Gray, L. J. et al. Rev. Geophys. 48, RG4001 (2010).
Olsen, J., Anderson, N. J. & Knudsen, M. F. Nature Geosci. 5, 808–812 (2012).
Martin-Puertas, C. et al. Nature Geosci. 5, 397–401 (2012).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Muscheler, R. The enigmatic 1,500-year cycle. Nature Geosci 5, 850–851 (2012). https://doi.org/10.1038/ngeo1640
Published:
Issue Date:
DOI: https://doi.org/10.1038/ngeo1640