Monsoonal precipitation variation in the East Asia since A.D. 1840 Tree-ring evidences from China and Korea

Three tree-ring rainfall reconstructions from China and Korea are used in this paper to investigate the East Asian summer monsoon-related precipitation variation over the past 160 years. Statistically, there is no linear correlation on a year-by-year basis between Chinese and Korean monsoon rainfall...

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Published inScience in China. Series D, Earth sciences Vol. 46; no. 10; pp. 1031 - 1039
Main Authors Liu, Yu, Won-Kyu, Park, Cai, Qiufang, Jung-Wook, Seo, Hyun-Sook, Jung
Format Journal Article
LanguageEnglish
Published 01.10.2003
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Summary:Three tree-ring rainfall reconstructions from China and Korea are used in this paper to investigate the East Asian summer monsoon-related precipitation variation over the past 160 years. Statistically, there is no linear correlation on a year-by-year basis between Chinese and Korean monsoon rainfall, but region-wide synchronous variation on a decadal-scale was observed. More rainfall intervals were 1860-1890, 1910-1925, and 1940-1960, and dry or even drought periods were 1890-1910, 1925-1940, and 1960-present. Reconstructions also display that the East Asian summer monsoon precipitation suddenly changed from more into less around mid-1920. These tree-ring precipitation records were also confirmed by Chinese historical dryness/wetness index and Korean historical rain gauge data.
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ISSN:1006-9313
1862-2801
DOI:10.1007/BF02959398