Climatic Change

, Volume 43, Issue 1, pp 151–168

European Tree Rings and Climate in the 16th Century

Authors

  • K.R. Briffa
    • Climatic Research UnitUniversity of East Anglia
  • P.D. Jones
    • Climatic Research UnitUniversity of East Anglia
  • R.B. Vogel
    • Snow and Landscape ResearchSwiss Federal Institute for Forest
  • F.H. Schweingruber
    • Snow and Landscape ResearchSwiss Federal Institute for Forest
  • M.G.L. Baillie
    • Palaeoecology Centre, School of GeosciencesQueen's University
  • S.G. Shiyatov
    • Institute of Plant and Animal EcologyUral Branch of the Russian Academy of Sciences
  • E.A. Vaganov
    • Institute of ForestSiberian Branch of the Russian Academy of Sciences
Article

DOI: 10.1023/A:1005529830082

Cite this article as:
Briffa, K., Jones, P., Vogel, R. et al. Climatic Change (1999) 43: 151. doi:10.1023/A:1005529830082

Abstract

We present a selective review of tree-ring variability and inferred climate changes in Europe during the 16th century. The dendroclimatological evidence is assessed within the context of the last 500 years and some interpretational problems are discussed. The tree-ring evidence is compared with various non-dendroclimatic evidence. The body of evidence shows that a large region of mid and northern Europe experienced a sharp cooling at around 1570/80 that, at least in the north, marked a shift towards a prolonged period of cool conditions. This region had its southern boundary in the Alps and there is little evidence for a major cooling in southern Europe.

Copyright information

© Kluwer Academic Publishers 1999