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dc.contributor.authorAnchukaitis, Kevin J.
dc.contributor.authorWilson, Rob
dc.contributor.authorBriffa, Keith R.
dc.contributor.authorBüntgen, Ulf
dc.contributor.authorCook, Edward R.
dc.contributor.authorD'Arrigo, Rosanne
dc.contributor.authorDavi, Nicole
dc.contributor.authorEsper, Jan
dc.contributor.authorFrank, David
dc.contributor.authorGunnarson, Björn E.
dc.contributor.authorHegerl, Gabi
dc.contributor.authorHelama, Samuli
dc.contributor.authorKlesse, Stefan
dc.contributor.authorKrusic, Paul J.
dc.contributor.authorLinderholm, Hans W.
dc.contributor.authorMyglan, Vladimir
dc.contributor.authorOsborn, Timothy J.
dc.contributor.authorZhang, Peng
dc.contributor.authorRydval, Miloš
dc.contributor.authorSchneider, Lea
dc.contributor.authorSchurer, Andrew
dc.contributor.authorWiles, Greg
dc.contributor.authorZorita, Eduardo
dc.date.accessioned2018-03-09T00:33:13Z
dc.date.available2018-03-09T00:33:13Z
dc.date.issued2017-05-01
dc.identifier.citationAnchukaitis , K J , Wilson , R , Briffa , K R , Büntgen , U , Cook , E R , D'Arrigo , R , Davi , N , Esper , J , Frank , D , Gunnarson , B E , Hegerl , G , Helama , S , Klesse , S , Krusic , P J , Linderholm , H W , Myglan , V , Osborn , T J , Zhang , P , Rydval , M , Schneider , L , Schurer , A , Wiles , G & Zorita , E 2017 , ' Last millennium Northern Hemisphere summer temperatures from tree rings : part II, spatially resolved reconstructions ' , Quaternary Science Reviews , vol. 163 , pp. 1-22 . https://doi.org/10.1016/j.quascirev.2017.02.020en
dc.identifier.issn0277-3791
dc.identifier.otherPURE: 249338118
dc.identifier.otherPURE UUID: f67d5d0f-9d95-46c6-b08a-adffe82fdb97
dc.identifier.otherRIS: urn:1C1908CB195CE358500D336415EDDCA5
dc.identifier.otherScopus: 85014656159
dc.identifier.otherORCID: /0000-0003-4486-8904/work/59953632
dc.identifier.otherWOS: 000401204200001
dc.identifier.urihttp://hdl.handle.net/10023/12885
dc.descriptionRW: UK Natural Environment Research Council (NERC - NE/K003097/1) and Leverhulme Trust project (F/00 268/BG)en
dc.description.abstractClimate field reconstructions from networks of tree-ring proxy data can be used to characterize regional-scale climate changes, reveal spatial anomaly patterns associated with atmospheric circulation changes, radiative forcing, and large-scale modes of ocean-atmosphere variability, and provide spatiotemporal targets for climate model comparison and evaluation. Here we use a multiproxy network of tree-ring chronologies to reconstruct spatially resolved warm season (May–August) mean temperatures across the extratropical Northern Hemisphere (40-90°N) using Point-by-Point Regression (PPR). The resulting annual maps of temperature anomalies (750–1988 CE) reveal a consistent imprint of volcanism, with 96% of reconstructed grid points experiencing colder conditions following eruptions. Solar influences are detected at the bicentennial (de Vries) frequency, although at other time scales the influence of insolation variability is weak. Approximately 90% of reconstructed grid points show warmer temperatures during the Medieval Climate Anomaly when compared to the Little Ice Age, although the magnitude varies spatially across the hemisphere. Estimates of field reconstruction skill through time and over space can guide future temporal extension and spatial expansion of the proxy network.
dc.format.extent22
dc.language.isoeng
dc.relation.ispartofQuaternary Science Reviewsen
dc.rights© 2017 Elsevier Ltd. All rights reserved. This work has been made available online in accordance with the publisher’s policies. This is the author created, accepted version manuscript following peer review and may differ slightly from the final published version. The final published version of this work is available at: https://doi.org/10.1016/j.quascirev.2017.02.020en
dc.subjectTree-ringsen
dc.subjectNorthern Hemisphereen
dc.subjectLast millenniumen
dc.subjectCommon Eraen
dc.subjectSummer temperaturesen
dc.subjectReconstructionen
dc.subjectSpatialen
dc.subjectGE Environmental Sciencesen
dc.subjectDASen
dc.subject.lccGEen
dc.titleLast millennium Northern Hemisphere summer temperatures from tree rings : part II, spatially resolved reconstructionsen
dc.typeJournal articleen
dc.description.versionPostprinten
dc.contributor.institutionUniversity of St Andrews.Earth and Environmental Sciencesen
dc.contributor.institutionUniversity of St Andrews.Scottish Oceans Instituteen
dc.contributor.institutionUniversity of St Andrews.St Andrews Sustainability Instituteen
dc.identifier.doihttps://doi.org/10.1016/j.quascirev.2017.02.020
dc.description.statusPeer revieweden
dc.date.embargoedUntil2018-03-08


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