Climatic Change

, Volume 49, Issue 1, pp 239–246

Spatial Response to Major Volcanic Events in or about AD 536, 934 and 1258: Frost Rings and Other Dendrochronological Evidence from Mongolia and Northern Siberia: Comment on R. B. Stothers, ‘Volcanic Dry Fogs, Climate Cooling, and Plague Pandemics in Europe and the Middle East’ (Climatic Change, 42, 1999)


  • Rosanne D'Arrigo
    • Tree-Ring Laboratory, Lamont-Doherty Earth Observatory
  • David Frank
    • Tree-Ring Laboratory, Lamont-Doherty Earth Observatory
  • Gordon Jacoby
    • Tree-Ring Laboratory, Lamont-Doherty Earth Observatory
  • Neil Pederson
    • Tree-Ring Laboratory, Lamont-Doherty Earth Observatory

DOI: 10.1023/A:1010727122905

Cite this article as:
D'Arrigo, R., Frank, D., Jacoby, G. et al. Climatic Change (2001) 49: 239. doi:10.1023/A:1010727122905


Hypothesized large-scale climatic extremes require verification from distantregions in order toconfirm the magnitude and timing of such events. Three of the most massivehypothesized volcanic events of the past two millennia, occurring in or aboutAD 536, 934 and1258, had profound climatic and demographic repercussions over much of Europe,the MiddleEast, and other areas, according to historical accounts recently described inStothers (1998, 1999,2000) as well as other research. Here we report on frost ring and otherdendrochronologicalevidence derived from a 1738-year tree-ring chronology from Mongolia andmillennial-scaletree-ring data from northern Siberia which demonstrate that these three eventsmay have alsoimpacted conditions in these distant regions.

Copyright information

© Kluwer Academic Publishers 2001