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EsperJan
Krusic, Paul J.
Ljungqvist, Fredrik
Luterbacher, Jürg
Carrer, Marco
Cook, Ed
Davi, Nicole K.
Hartl-Meier, Claudia
Kirdyanov, A.
Konter, O.
Myglan, V.
Timonen, Mauri
Treydte, Kerstin
Trouet, Valerie
Villalba, Ricardo
Wilson, Rob S.
Yang, Bao
Büntgen, Ulf
2016-11-11T08:50:46Z
2016-11-11T08:50:46Z
2016-08
EsperJan. Ranking of tree-ring based temperature reconstructions of the past millennium [Текст] / EsperJan, Paul J. Krusic, Fredrik Ljungqvist, Jürg Luterbacher, Marco Carrer, Ed Cook, Nicole K. Davi, Claudia Hartl-Meier, A. Kirdyanov, O. Konter, V. Myglan, Mauri Timonen, Kerstin Treydte, Valerie Trouet, Ricardo Villalba, Rob S. Wilson, Bao Yang, Ulf Büntgen // Quaternary Science Reviews. — 2016. — Т. 145. — С. 134-151
02773791
http://elib.sfu-kras.ru/handle/2311/27896
Tree-ring chronologies are widely used to reconstruct high-to low-frequency variations in growing season temperatures over centuries to millennia. The relevance of these timeseries in large-scale climate reconstructions is often determined by the strength of their correlation against instrumental temperature data. However, this single criterion ignores several important quantitative and qualitative characteristics of tree-ring chronologies. Those characteristics are (i) data homogeneity, (ii) sample replication, (iii) growth coherence, (iv) chronology development, and (v) climate signal including the correlation with instrumental data. Based on these 5 characteristics, a reconstruction-scoring scheme is proposed and applied to 39 published, millennial-length temperature reconstructions from Asia, Europe, North America, and the Southern Hemisphere. Results reveal no reconstruction scores highest in every category and each has their own strengths and weaknesses. Reconstructions that perform better overall include N-Scan and Finland from Europe, E-Canada from North America, Yamal and Dzhelo from Asia. Reconstructions performing less well include W-Himalaya and Karakorum from Asia, Tatra and S-Finland from Europe, and Great Basin from North America. By providing a comprehensive set of criteria to evaluate tree-ring chronologies we hope to improve the development of large-scale temperature reconstructions spanning the past millennium. All reconstructions and their corresponding scores are provided at www.blogs.uni-mainz.de/fb09climatology.
http://dx.doi.org/10.1016/j.quascirev.2016.05.009
Paleoclimate
Climate change
Proxy data
Dendrochronology
Dendroclimatology
Ranking of tree-ring based temperature reconstructions of the past millennium
Journal Article
Journal Article Preprint
134-151
34.35
2016-11-11T08:50:46Z
10.1016/j.quascirev.2016.05.009
Научно-исследовательская часть
Quaternary Science Reviews
Q1
Q1


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