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A preliminary seasonal precipitation reconstruction from tree-ring stable carbon isotopes at Mt. Helan, China, since AD 1804

机译:利用Mt树木年轮稳定碳同位素初步进行季节降水重建。中国贺兰,始建于1804年

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摘要

The relationship between the stable carbon isotope composition of tree rings from Mt. Helan, China, and precipitation was investigated for the period AD 1804-1997. The results reveal that in the Mt. Helan region, δ~(13)C of tree rings negatively correlates with the total precipitation from February to July. We calculated discrimination (Δ) to remove the effects of δ~(13)C of atmospheric CO_2 on the tree-ring δ~(13)C series, and reconstructed February to July precipitation back to 1804 using linear regression (R~2 = 0.415, R_(adj)~2= 0.394, F= 19.88, P<0.0001), with best chronology replication for AD 1845-1991. The reconstruction shows annual to decadal wetness/dryness fluctuations. The historically documented drought of 1926-1930, and the wet period in the 1940s were found in our reconstruction.
机译:山地树木年轮的稳定碳同位素组成之间的关系。研究了中国贺兰和公元1804-1997年期间的降水。结果表明,在山。贺兰地区树木年轮的δ〜(13)C与2月至7月的总降水量呈负相关。我们计算了判别力(Δ)以消除大气CO_2的δ〜(13)C对树环δ〜(13)C系列的影响,并使用线性回归将2月到7月的降水重建回到1804年(R〜2 = 0.415,R_(adj)〜2 = 0.394,F = 19.88,P <0.0001),最好的时间顺序复制适用于AD 1845-1991。重建显示每年到十年的湿度/干燥度波动。在我们的重建工作中发现了有历史记载的1926-1930年干旱,以及1940年代的湿润时期。

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