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Sökning: WFRF:(Kirdyanov Alexander) > Ranking of tree-rin...

LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00003768naa a2200541 4500
001oai:DiVA.org:su-133379
003SwePub
008160906s2016 | |||||||||||000 ||eng|
0247 a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1333792 URI
0247 a https://doi.org/10.1016/j.quascirev.2016.05.0092 DOI
040 a (SwePub)su
041 a engb eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
1001 a Esper, Jan4 aut
2451 0a Ranking of tree-ring based temperature reconstructions of the past millennium
264 1b Elsevier BV,c 2016
338 a print2 rdacarrier
520 a 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.
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
653 a Paleoclimate
653 a Climate change
653 a Proxy data
653 a Dendrochronology
653 a Dendroclimatology
7001 a Krusic, Paul J.u Stockholms universitet,Institutionen för naturgeografi,Navarino Environmental Observatory, Greece4 aut0 (Swepub:su)pakru
7001 a Charpentier Ljungqvist, Fredrik,d 1982-u Stockholms universitet,Historiska institutionen4 aut0 (Swepub:su)fchar
7001 a Luterbacher, Jürg4 aut
7001 a Carrer, Marco4 aut
7001 a Cook, Ed4 aut
7001 a Davi, Nicole K.4 aut
7001 a Hartl-Meier, Claudia4 aut
7001 a Kirdyanov, Alexander4 aut
7001 a Konter, Oliver4 aut
7001 a Myglan, Vladimir4 aut
7001 a Timonen, Mauri4 aut
7001 a Treydte, Kerstin4 aut
7001 a Trouet, Valerie4 aut
7001 a Villalba, Ricardo4 aut
7001 a Yang, Bao4 aut
7001 a Büntgen, Ulf4 aut
7102 a Stockholms universitetb Institutionen för naturgeografi4 org
7730 t Quaternary Science Reviewsd : Elsevier BVg 145, s. 134-151q 145<134-151x 0277-3791x 1873-457X
8564 u https://repository.arizona.edu/bitstream/10150/621352/1/JQSR-D-16-00018R1.pdf
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-133379
8564 8u https://doi.org/10.1016/j.quascirev.2016.05.009

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