Articles | Volume 11, issue 9
Clim. Past, 11, 1153–1164, 2015
https://doi.org/10.5194/cp-11-1153-2015
Clim. Past, 11, 1153–1164, 2015
https://doi.org/10.5194/cp-11-1153-2015

Research article 17 Sep 2015

Research article | 17 Sep 2015

A millennial summer temperature reconstruction for northeastern Canada using oxygen isotopes in subfossil trees

M. Naulier et al.

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Cited articles

Anchukaitis, K. J., D'Arrigo, R. D., Andreu-Hayles, L., Frank, D., Verstege, A., Curtis, A., Buckley, B. M., Jacoby, G. C., and Cook, E. R.: Tree-ring reconstructed summer temperatures from northwestern North America during the last nine centuries, J. Climate, 3001–3012, https://doi.org/10.1175/jcli-d-11-00139.1, 2012.
Arseneault, D., Dy, B., Gennaretti, F., Autin, J., and Bégin, Y.: Developing millennial tree ring chronologies in the fire-prone North American boreal forest, J. Quat. Sci., 28, 283–292, https://doi.org/10.1002/jqs.2612, 2013.
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Short summary
This paper presents a millennial δ18O series and the reconstruction of the maximal temperature. The maximal replication and annual resolution have been obtained by using cohort sampling method. Three contrasted climatic periods have been identified: the medieval warm period (~997-1250; the warmest), the little ice age (~1450-1880) and the modern period (1970-2000) that is one of the fastest warming over the last millennium.