Climate of the Past Discussions www.clim-past-discuss.net 1814-9340 1814-9359 5 2 2009 10.5194/cpd-5-1215-2009 http://www.clim-past-discuss.net/5/1215/2009/ http://www.clim-past-discuss.net/5/1215/2009/cpd-5-1215-2009.html http://www.clim-past-discuss.net/5/1215/2009/cpd-5-1215-2009.pdf 1215 1229 2009-04-15 Tree ring-based February–April temperature reconstruction for Changbai Mountain in Northeast China and its implication for East Asian Winter Monsoon H. F. Zhu X. Q. Fang xfang@bnu.edu.cn X. M. Shao Z. Y. Yin Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China School of Geography, Beijing Normal University, Beijing, China Department of Marine Science and Environmental Studies, University of San Diego, San Diego, USA Long-term climatic records are scarce in the northeast Asia for understanding the behavior of the East Asian Winter Monsoon. Here we describe a 250-year February–April temperature reconstruction (TCBM) based on tree-ring widths of Korean Pines from the Changbai Mountain area, Northeast China. The reconstruction can account for 45.7% of the temperature variance in the instrumental period (1953 to 2001). Four cold events including 1784–1815, 1827–1851, 1878–1889 and 1911–1945, and two warm events of 1750–1783 and 1855–1877 were identified before the instrumental period. Four regime shifts were also detected at 1781, 1857, 1878 and 1989. Good agreements between TCBM and other temperature records of East Asia suggest that the reconstruction is of good reliability and captures the regional cold/warm events of East Asia. Moreover, TCBM shows negative correlations with the instrumental or proxy-based EAWM intensity records. The known weakening of the EAWM in the late 1980s is in agreement with the regime shift at 1989 in TCBM. 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