BÜNTGEN, Ulf, Dominique ARSENEAULT, Etienne BOUCHER, Olga V. CHURAKOVA SIDOROVA, Fabio GENNARETTI, Alan CRIVELLARO, Malcolm K. HUGHES, Alexander V. KIRDYANOV, Lara KLIPPEL, Paul J. KRUSIC, Hans W. LINDERHOLM, Fredrik C. LJUNGQVIST, Josef LUDESCHER, Michael MCCORMICK, Vladimir S. MYGLAN, Kurt NICOLUSSI, Alma PIERMATTEI, Clive OPPENHEIMER, Frederick REINIG, Michael SIGL, Eugene A. VAGANOV and Jan ESPER. Recognising bias in Common Era temperature reconstructions. Dendrochronologia. Munich: Elsevier GmbH, 2022, vol. 74, August, p. 1-3. ISSN 1125-7865. Available from: https://dx.doi.org/10.1016/j.dendro.2022.125982.
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Basic information
Original name Recognising bias in Common Era temperature reconstructions
Authors BÜNTGEN, Ulf (276 Germany, guarantor, belonging to the institution), Dominique ARSENEAULT, Etienne BOUCHER, Olga V. CHURAKOVA SIDOROVA, Fabio GENNARETTI, Alan CRIVELLARO, Malcolm K. HUGHES, Alexander V. KIRDYANOV, Lara KLIPPEL, Paul J. KRUSIC, Hans W. LINDERHOLM, Fredrik C. LJUNGQVIST, Josef LUDESCHER, Michael MCCORMICK, Vladimir S. MYGLAN, Kurt NICOLUSSI, Alma PIERMATTEI, Clive OPPENHEIMER, Frederick REINIG, Michael SIGL, Eugene A. VAGANOV and Jan ESPER.
Edition Dendrochronologia, Munich, Elsevier GmbH, 2022, 1125-7865.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher Germany
Confidentiality degree is not subject to a state or trade secret
WWW URL
Impact factor Impact factor: 3.000
RIV identification code RIV/00216224:14310/22:00127303
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1016/j.dendro.2022.125982
UT WoS 000826976900002
Keywords in English Climate variation; Common Era; IPCC; Large-scale network; Multi -proxy reconstruction; Science communication; Tree rings
Tags rivok
Tags International impact, Reviewed
Changed by Changed by: Mgr. Marie Šípková, DiS., učo 437722. Changed: 30/11/2022 15:35.
Abstract
A steep decline in the quality and quantity of available climate proxy records before medieval times challenges any comparison of reconstructed temperature and hydroclimate trends and extremes between the first and second half of the Common Era. Understanding of the physical causes, ecological responses and societal consequences of past climatic changes, however, demands highly-resolved, spatially-explicit, seasonally-defined and absolutely-dated archives over the entire period in question. Continuous efforts to improve existing proxy records and reconstruction methods and to develop new ones, as well as clear communication of all uncertainties (within and beyond academia) must be central tasks for the paleoclimate community.
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