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Regional extreme climate events on the northeastern Tibetan Plateau since AD 1450 inferred from tree rings
Copyright © 2010 Published by Elsevier B.V
November 15, 2010
Chun Qin, Bao Yang, Achim Bräuning, Dmitry M. Sonechkin and Kai Huang
Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, China
Institute of Geography, University of Erlangen-Nürnberg, Kochstrasse 4-4, Erlangen 91054, Germany
P.P. Shirshov Oceanology Institute, Russian Academy of Sciences, Nakhimovskii prospect 36, Moscow, 117997, Russia
Abstract
Qilian juniper (Juniperus przewalskii Kom.) is a widely distributed tree species growing on south-facing slopes in the northeastern Tibetan Plateau in arid northwestern China. We established a tree ring-width network based on two new chronologies and four previously-published chronologies. Correlation and response function analyses demonstrate that precipitation positively influences radial growth. Despite of minor differences in local climate-growth relations, precipitation for the annual window between previous July and current June shows consistent positive correlations with ring width at all study sites. Similar to the so called ‘pointer year’ approach, ‘anomalous’ growth years were defined to extract extreme climate events for the period AD 1450-2006. We defined a dryness-wetness grade series with five grades of climate events inferred from anomalous-year analysis. During the last 50 years, the frequency of wet events increased and that of drought events decreased noticeably, implying that the probability of occurrence of dry years in the northeastern Tibetan Plateau will be lower in the future if the global warming continues. Combining our proxy records with a historical dryness-wetness record from eastern China, we mapped dryness-wetness patterns over large parts of China. By analyzing the atmospheric pressure patterns at the 850 hPa level over China for selected extreme event years, we found that the confluence of cold and hot air is a precondition for a flood event in the northeastern Tibetan plateau. Thus, a counterclockwise atmospheric circulation centered in south of Lake Baikal only occurs in flood event years.
Keywords: Dendroclimatology; anomalous year; extreme climate events; atmospheric dynamics; northeastern Tibetan Plateau
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