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dc.contributor.authorHantemirov, R. M.en
dc.contributor.authorCorona, C.en
dc.contributor.authorGuillet, S.en
dc.contributor.authorShiyatov, S. G.en
dc.contributor.authorStoffel, M.en
dc.contributor.authorOsborn, T. J.en
dc.contributor.authorMelvin, T. M.en
dc.contributor.authorGorlanova, L. A.en
dc.contributor.authorKukarskih, V. V.en
dc.contributor.authorSurkov, A. Y.en
dc.contributor.authorvon Arx, G.en
dc.contributor.authorFonti, P.en
dc.date.accessioned2022-10-19T05:21:25Z-
dc.date.available2022-10-19T05:21:25Z-
dc.date.issued2022-
dc.identifier.citationCurrent Siberian heating is unprecedented during the past seven millennia / R. M. Hantemirov, C. Corona, S. Guillet et al. // Nature Communications. — 2022. — Vol. 13. — Iss. 1. — 4968.en
dc.identifier.issn20411723-
dc.identifier.otherhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85137051121&doi=10.1038%2fs41467-022-32629-x&partnerID=40&md5=be42b617d7d2ce1f405c40c22404ee4clink
dc.identifier.urihttp://elar.urfu.ru/handle/10995/118073-
dc.description.abstractThe Arctic is warming faster than any other region on Earth. Putting this rapid warming into perspective is challenging because instrumental records are often short or incomplete in polar regions and precisely-dated temperature proxies with high temporal resolution are largely lacking. Here, we provide this long-term perspective by reconstructing past summer temperature variability at Yamal Peninsula – a hotspot of recent warming – over the past 7638 years using annually resolved tree-ring records. We demonstrate that the recent anthropogenic warming interrupted a multi-millennial cooling trend. We find the industrial-era warming to be unprecedented in rate and to have elevated the summer temperature to levels above those reconstructed for the past seven millennia (in both 30-year mean and the frequency of extreme summers). This is undoubtedly of concern for the natural and human systems that are being impacted by climatic changes that lie outside the envelope of natural climatic variations for this region. © 2022, The Author(s).en
dc.description.sponsorshipNatural Environment Research Council, NERC: NE/S015582/1; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung, SNF: 183571; Russian Foundation for Basic Research, РФФИ: 18-05-00575; Russian Science Foundation, RSF: 182398, 21-14-00330en
dc.description.sponsorshipR.M.H., S.G.S., A.Y.S., and L.A.G. received funding from the Russian Foundation for Basic Research (no. 18-05-00575). M.S., C.C., S.G., and P.F. received funding from the SNF Sinergia project CALDERA (no. 183571). V.V.K. acknowledges support from the Russian Science Foundation (no. 21-14-00330). G.vA. acknowledges support from the SNF project XELLCLIM (no. 182398). T.J.O. acknowledges support from UK NERC project GloSAT (no. NE/S015582/1).en
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.publisherNature Researchen
dc.relationinfo:eu-repo/grantAgreement/RSF//21-14-00330en
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.sourceNature Communicationsen
dc.subjectCLIMATE CHANGEen
dc.subjectCOOLINGen
dc.subjectHEATINGen
dc.subjectHUMAN ACTIVITYen
dc.subjectTEMPERATURE PROFILEen
dc.subjectTREE RINGen
dc.subjectARTICLEen
dc.subjectCLIMATE CHANGEen
dc.subjectCOOLINGen
dc.subjectHEATINGen
dc.subjectHUMANen
dc.subjectSUMMERen
dc.subjectWARMINGen
dc.subjectARCTICen
dc.subjectSEASONen
dc.subjectTEMPERATUREen
dc.subjectTREEen
dc.subjectRUSSIAN FEDERATIONen
dc.subjectSIBERIAen
dc.subjectYAMAL PENINSULAen
dc.subjectYAMALO-NENETSen
dc.subjectARCTIC REGIONSen
dc.subjectHEATINGen
dc.subjectHUMANSen
dc.subjectSEASONSen
dc.subjectTEMPERATUREen
dc.subjectTREESen
dc.titleCurrent Siberian heating is unprecedented during the past seven millenniaen
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.identifier.doi10.1038/s41467-022-32629-x-
dc.identifier.scopus85137051121-
local.contributor.employeeHantemirov, R.M., Institute of Plant and Animal Ecology, Ural Division of the Russian Academy of Sciences, Ekaterinburg, 620144, Russian Federation, Ural Federal University, Ekaterinburg, 620002, Russian Federationen
local.contributor.employeeCorona, C., Climate Change Impacts and Risks in the Anthropocene (C-CIA), Institute for Environmental Sciences, University of Geneva, Geneva, 1205, Switzerland, Geolab, UMR 6042 CNRS, Université Clermont Auvergne, Clermont-Ferrand, F-63057, France, Department F.A. Forel for Environmental and Aquatic Sciences, University of Geneva, Geneva, 1205, Switzerlanden
local.contributor.employeeGuillet, S., Climate Change Impacts and Risks in the Anthropocene (C-CIA), Institute for Environmental Sciences, University of Geneva, Geneva, 1205, Switzerlanden
local.contributor.employeeShiyatov, S.G., Institute of Plant and Animal Ecology, Ural Division of the Russian Academy of Sciences, Ekaterinburg, 620144, Russian Federationen
local.contributor.employeeStoffel, M., Climate Change Impacts and Risks in the Anthropocene (C-CIA), Institute for Environmental Sciences, University of Geneva, Geneva, 1205, Switzerland, Department F.A. Forel for Environmental and Aquatic Sciences, University of Geneva, Geneva, 1205, Switzerland, Department of Earth Sciences, University of Geneva, Geneva, 1205, Switzerlanden
local.contributor.employeeOsborn, T.J., Climatic Research Unit, School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, United Kingdomen
local.contributor.employeeMelvin, T.M., Climatic Research Unit, School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, United Kingdomen
local.contributor.employeeGorlanova, L.A., Institute of Plant and Animal Ecology, Ural Division of the Russian Academy of Sciences, Ekaterinburg, 620144, Russian Federationen
local.contributor.employeeKukarskih, V.V., Institute of Plant and Animal Ecology, Ural Division of the Russian Academy of Sciences, Ekaterinburg, 620144, Russian Federation, Ural Federal University, Ekaterinburg, 620002, Russian Federationen
local.contributor.employeeSurkov, A.Y., Institute of Plant and Animal Ecology, Ural Division of the Russian Academy of Sciences, Ekaterinburg, 620144, Russian Federationen
local.contributor.employeevon Arx, G., Swiss Federal Research Institute WSL, Birmensdorf, 8903, Switzerland, Oeschger Centre for Climate Change Research, University of Bern, Bern, 3012, Switzerlanden
local.contributor.employeeFonti, P., Swiss Federal Research Institute WSL, Birmensdorf, 8903, Switzerlanden
local.issue1-
local.volume13-
dc.identifier.wos000845603400044-
local.contributor.departmentInstitute of Plant and Animal Ecology, Ural Division of the Russian Academy of Sciences, Ekaterinburg, 620144, Russian Federationen
local.contributor.departmentUral Federal University, Ekaterinburg, 620002, Russian Federationen
local.contributor.departmentClimate Change Impacts and Risks in the Anthropocene (C-CIA), Institute for Environmental Sciences, University of Geneva, Geneva, 1205, Switzerlanden
local.contributor.departmentGeolab, UMR 6042 CNRS, Université Clermont Auvergne, Clermont-Ferrand, F-63057, Franceen
local.contributor.departmentDepartment F.A. Forel for Environmental and Aquatic Sciences, University of Geneva, Geneva, 1205, Switzerlanden
local.contributor.departmentDepartment of Earth Sciences, University of Geneva, Geneva, 1205, Switzerlanden
local.contributor.departmentClimatic Research Unit, School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, United Kingdomen
local.contributor.departmentSwiss Federal Research Institute WSL, Birmensdorf, 8903, Switzerlanden
local.contributor.departmentOeschger Centre for Climate Change Research, University of Bern, Bern, 3012, Switzerlanden
local.identifier.pure30844663-
local.description.order4968-
local.identifier.eid2-s2.0-85137051121-
local.fund.rsf21-14-00330-
local.identifier.wosWOS:000845603400044-
local.identifier.pmid36008406-
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