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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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Maud Naulier on behalf of the Authors (14 May 2015)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (19 May 2015) by Valérie Masson-Delmotte
RR by Valérie Daux (12 Jun 2015)
RR by Hans Linderholm (30 Jun 2015)
ED: Publish subject to minor revisions (review by Editor) (09 Jul 2015) by Valérie Masson-Delmotte
AR by Maud Naulier on behalf of the Authors (17 Jul 2015)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by Editor) (28 Jul 2015) by Valérie Masson-Delmotte
AR by Maud Naulier on behalf of the Authors (05 Aug 2015)  Author's response    Manuscript
ED: Publish as is (14 Aug 2015) by Valérie Masson-Delmotte
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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.