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    • Tree-Ring Research, Volume 63 (2007)
    • Tree-Ring Research, Volume 63, Issue 1 (Jun 2007)
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    Tree-Ring-Derived Precipitation Records From Inner Mongolia, China, Since A.D. 1627

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    Author
    Liu, Yu
    Sun, Junyan
    Yang, Yinke
    Cai, Qiufang
    Song, Huiming
    Shi, Jiangfeng
    An, Zhisheng
    Li, Xuxiang
    Affiliation
    The State Key Laboratory of Loess and Quaternary Geology, The Institute of Earth Environment, Chinese Academy of Sciences Xi’an 710075, China
    Department of Environment Engineering, School of Energy and Power Engineering of Xi’an Jiaotong University
    Graduate School of the Chinese Academy of Sciences, Beijing 100049, China
    Issue Date
    2007-06
    Keywords
    Dendrochronology
    Tree Rings
    Inner Mongolia
    Pinus tabulaeformis Carriere
    Precipitation Reconstruction
    
    Metadata
    Show full item record
    Rights
    Copyright © Tree-Ring Society. All rights reserved.
    Collection Information
    This item is part of the Tree-Ring Research (formerly Tree-Ring Bulletin) archive. For more information about this peer-reviewed scholarly journal, please email the Editor of Tree-Ring Research at editor@treeringsociety.org.
    Publisher
    Tree-Ring Society
    Journal
    Tree-Ring Research
    Citation
    Liu, Y., Sun, J., Yang, Y., Cai, Q., Song, H., Shi, J., An, Z., Li, X., 2007. Tree-ring-derived precipitation records from Inner Mongolia, China, since A.D. 1627. Tree-Ring Research 63(1):3-14.
    Abstract
    Two Chinese pine (Pinus tabulaeformis) tree-ring width chronologies up to 375 years long were used to reconstruct rainfall from February to early July for the Wu Dangzhao region and from February to mid-July for the La Madong region, Inner Mongolia, China. The predictor variables account for 44.3% and 42.7% of the variance in precipitation, respectively. Both historical records and two other tree-ring based precipitation reconstructions from the environmentally sensitive zone (the northern Helan Mountain range and Baiyinaobao) confirm our results. After applying a 10-year moving average, the trends of four tree-ring based precipitation reconstructions vary synchronously. Periods with below-normal precipitation occurred during the 1720s–1730s, 1740s–1750s, 1790s, early 1810s, late 1830s–1860s, 1880s–1910s, late 1920s–1930s and after the late 1960s–early 1970s. Periods with above-normal precipitation occurred in the 1760s to early 1770s, 1820s to early 1830s, 1870s–1880s, early 1920s, 1940s to early 1960s, and 1990s. The late 1920s period was the most severe drought over a broad area in north China in the last 375 years. In contrast, the wettest period was in the late 1990s.
    ISSN
    2162-4585
    1536-1098
    Additional Links
    http://www.treeringsociety.org
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    Tree-Ring Research, Volume 63, Issue 1 (Jun 2007)

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