J 2012

Multi-archive summer temperature reconstruction for the European Alps, AD 1053-1996

TRACHSEL, Mathias, Christian KAMENIK, Martin GROSJEAN, Danny MCCARROL, Anders MOBERG et. al.

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

Language

English

Type of outcome

Článek v odborném periodiku

Field of Study

10500 1.5. Earth and related environmental sciences

Country of publisher

United Kingdom of Great Britain and Northern Ireland

Confidentiality degree

není předmětem státního či obchodního tajemství

Impact factor

Impact factor: 4.076

RIV identification code

RIV/00216224:14310/12:00061673

Organization unit

Faculty of Science

UT WoS

000306350400005

Keywords in English

Paleoclimate; Alps; Last millennium; Multi-proxy; Climate reconstruction; Climate

Tags

Změněno: 10/4/2013 20:52, Ing. Andrea Mikešková

Abstract

V originále

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.