Artigo Revisado por pares

Synchronous variability changes in Alpine temperature and tree-ring data over the past two centuries

2005; Wiley; Volume: 34; Issue: 4 Linguagem: Inglês

10.1080/03009480500231443

ISSN

1502-3885

Autores

David Frank, Rob Wilson, Jan Esper,

Tópico(s)

Climate variability and models

Resumo

BoreasVolume 34, Issue 4 p. 498-505 Free to Read Synchronous variability changes in Alpine temperature and tree-ring data over the past two centuries DAVID FRANK, DAVID FRANK (e-mail: [email protected]) Swiss Federal Research Institute WSL, Zürcherstrasse 111, 8903 Birmensdorf SwitzerlandSearch for more papers by this authorROBERT WILSON, ROBERT WILSON School of Geosciences, Grant Institute, Edinburgh University, West Mains Road, Edinburgh, EH9 3JW, United KingdomSearch for more papers by this authorJAN ESPER, JAN ESPER (e-mail: [email protected]) Swiss Federal Research Institute WSL, Zürcherstrasse 111, 8903 Birmensdorf SwitzerlandSearch for more papers by this author DAVID FRANK, DAVID FRANK (e-mail: [email protected]) Swiss Federal Research Institute WSL, Zürcherstrasse 111, 8903 Birmensdorf SwitzerlandSearch for more papers by this authorROBERT WILSON, ROBERT WILSON School of Geosciences, Grant Institute, Edinburgh University, West Mains Road, Edinburgh, EH9 3JW, United KingdomSearch for more papers by this authorJAN ESPER, JAN ESPER (e-mail: [email protected]) Swiss Federal Research Institute WSL, Zürcherstrasse 111, 8903 Birmensdorf SwitzerlandSearch for more papers by this author First published: 28 June 2008 https://doi.org/10.1080/03009480500231443Citations: 20AboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onEmailFacebookTwitterLinkedInRedditWechat Abstract The understanding of extremes and their temporal distribution is useful in characterizing the behaviour of the climate system, and necessary for understanding their social and economic costs and risks. This task is analogous to the study of pointer years in dendrochronological investigations. Commonly used dendroclimatological methods, however, tend to result in an equalization of variance throughout the record by normalizing variability within moving windows. Here, we analyse a larger network of high-elevation temperature-sensitive tree sites from the European Alps processed to preserve the relative frequency and magnitude of extreme events. In so doing, temporal changes in year-to-year tree-ring width variability were found. These decadal length periods of increased or decreased likelihood of extremes coincide with variability measures from a long-instrumental summer temperature record representative of high-elevation conditions in the Alps. Intervention analysis, using an F-test to identify shifts in variance, on both the tree-ring and instrumental series, resulted in the identification of common transitional years. Based on a well-replicated network of sites reflecting common climatic variation, our study demonstrates that the annual growth rings of trees can be utilized to quantify past frequency and amplitude changes in extreme variability. Furthermore, the approach outlined is suited to address questions about the role of external forcing, ocean—atmosphere interactions, or synoptic scale changes in determining patterns of observed extremes prior to the instrumental period. References Benestad, R. E. 2004: Record-values, nonstationarity tests and extreme value distributions. 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