A 3,500-year tree-ring record of annual precipitation on the northeastern Tibetan Plateau
Time Factors
550
Geography
Climate Change
Rain
15. Life on land
Tibet
01 natural sciences
Trees
900
13. Climate action
Snow
History, Ancient
0105 earth and related environmental sciences
DOI:
10.1073/pnas.1319238111
Publication Date:
2014-02-11T06:09:20Z
AUTHORS (7)
ABSTRACT
SignificanceThis paper describes the production and climatic interpretation of a tree-ring width chronology that is currently the longest, absolutely dated series produced for the northeastern Tibetan Plateau and one of the longest in the world. The method of chronology construction enables comparison of variations in precipitation totals over long timescales as well as shorter periods. Precipitation in this region during the last 50 years has been historically high—likely higher than for any equivalent length period in at least 3,500 years, even when considering the chronology and interpretational uncertainty. Notable dry periods occurred in the 4th century BCE and in the second half of the 15th century CE.
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