Orbital forcing of tree-ring data

Jan Esper (), David C. Frank, Mauri Timonen, Eduardo Zorita, Rob J. S. Wilson, Jürg Luterbacher, Steffen Holzkämper, Nils Fischer, Sebastian Wagner, Daniel Nievergelt, Anne Verstege and Ulf Büntgen
Additional contact information
Jan Esper: Johannes Gutenberg University
David C. Frank: Swiss Federal Research Institute WSL
Mauri Timonen: Finnish Forest Research Institute, Rovaniemi Research Unit
Eduardo Zorita: Institute for Coastal Research, HZG Research Centre
Rob J. S. Wilson: School of Geography and Geosciences, University of St Andrews
Jürg Luterbacher: Climatology, Climate Dynamics and Climate Change, Justus-Liebig University
Steffen Holzkämper: Johannes Gutenberg University
Nils Fischer: Max Planck Institute for Meteorology
Sebastian Wagner: Institute for Coastal Research, HZG Research Centre
Daniel Nievergelt: Swiss Federal Research Institute WSL
Anne Verstege: Swiss Federal Research Institute WSL
Ulf Büntgen: Swiss Federal Research Institute WSL

Nature Climate Change, 2012, vol. 2, issue 12, 862-866

Abstract: Based on an analysis of maximum latewood density data from northern Scandinavia, along with published dendrochronological records, this study finds evidence that previous tree-ring-reliant reconstructions of large-scale near-surface air temperature underestimated long-term pre-industrial warmth during Medieval and Roman times.

Date: 2012
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DOI: 10.1038/nclimate1589

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