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
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
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