TRACHSEL, Mathias, Christian KAMENIK, Martin GROSJEAN, Danny MCCARROL, Anders MOBERG, Rudolf BRÁZDIL, Ulf BUENTGEN, Petr DOBROVOLNÝ, Jan ESPER, David C. FRANK, Michael FRIEDRICH, Ruediger GLASER, Isabelle LAROCQUE-TOBLER, Kurt NICOLUSSI and Dirk RIEMANN. Multi-archive summer temperature reconstruction for the European Alps, AD 1053-1996. Quaternary Science Reviews. 2012, vol. 46, 16. 6., p. 66-79. ISSN 0277-3791. Available from: https://dx.doi.org/10.1016/j.quascirev.2012.04.021.
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Basic information
Original name Multi-archive summer temperature reconstruction for the European Alps, AD 1053-1996
Authors TRACHSEL, Mathias (756 Switzerland, guarantor), Christian KAMENIK (756 Switzerland), Martin GROSJEAN (756 Switzerland), Danny MCCARROL (826 United Kingdom of Great Britain and Northern Ireland), Anders MOBERG (752 Sweden), Rudolf BRÁZDIL (203 Czech Republic, belonging to the institution), Ulf BUENTGEN (756 Switzerland), Petr DOBROVOLNÝ (203 Czech Republic, belonging to the institution), Jan ESPER (276 Germany), David C. FRANK (756 Switzerland), Michael FRIEDRICH (276 Germany), Ruediger GLASER (276 Germany), Isabelle LAROCQUE-TOBLER (756 Switzerland), Kurt NICOLUSSI (40 Austria) and Dirk RIEMANN (276 Germany).
Edition Quaternary Science Reviews, 2012, 0277-3791.
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 United Kingdom of Great Britain and Northern Ireland
Confidentiality degree is not subject to a state or trade secret
Impact factor Impact factor: 4.076
RIV identification code RIV/00216224:14310/12:00061673
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1016/j.quascirev.2012.04.021
UT WoS 000306350400005
Keywords in English Paleoclimate; Alps; Last millennium; Multi-proxy; Climate reconstruction; Climate
Tags AKR, rivok
Changed by Changed by: Ing. Andrea Mikešková, učo 137293. Changed: 10/4/2013 20:52.
Abstract
We present a multiarchive, multi-proxy summer temperature reconstruction for the European Alps covering the period AD 1053-1996 using tree-ring and lake sediment data. The new reconstruction is based on nine different calibration approaches and errors were estimated conservatively. Summer temperatures of the last millennium are characterised by two warm (AD 1053-1171 and 1823-1996) and two cold phases (AD 1172-1379 and 1573-1822). Highest pre-industrial summer temperatures of the 12th century were 0.3 deg. C warmer than the 20th century mean but 0.35 deg. C colder than proxy derived temperatures at the end of the 20th century. The lowest temperatures at the end of the 16th century were approx. 1 deg. C lower than the 20th century mean.
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