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首页> 外文期刊>Dendrochronologia >Annual precipitation variability inferred from tree-ring width chronologies in the Changling-Shoulu region, China, during AD 1853-2007
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Annual precipitation variability inferred from tree-ring width chronologies in the Changling-Shoulu region, China, during AD 1853-2007

机译:根据公元1853-2007年中国长岭-寿路地区树木年轮宽度的年代学推断出年降水量变化

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On the basis of a significant correlation between the tree-ring width series from Changling-Shoulu (CLSL) in north-central China and observed instrumental data, the annual total precipitation of the previous July to the current June was reconstructed since 1853 for the studied region, with the predictor variables accounting for 41.2% of the variance in the precipitation data. Distinct wet periods with precipitation levels greater than the mean (315 mm) occurred in 1864-1876 and 1934-1960. Notable dry periods with precipitation less than the mean occurred in 1877-1888 and 1923-1933. The precipitation fluctuated dramatically during 1940-1970, and became relatively stable around the mean value from 1960. The CLSL precipitation series showed significant correlations with precipitation reconstructions from Mt. Xinglong, Mt. Helan, Ningwu and eastern China, suggesting that these five rainfall curves represent the general precipitation variations in the western-central environmentally sensitive zone of northern China. The calculations of the CRU grid points also indicate the existence of significant spatial correlation among these sites. Periodicity analysis showed clear 23.33-, 8.24-, 2.64- and 2.59-year cycles at a 99% confidence level for the reconstructed series during the past 155 years
机译:基于中国中北部长岭-寿鹿(CLSL)的年轮宽度序列与观测仪器数据之间的显着相关性,对1853年以来的7月至6月的年降水总量进行了重建。区域,预测变量占降水数据方差的41.2%。 1864-1876年和1934-1960年出现了明显高于平均水平(315 mm)的明显湿润时期。降雨量低于平均值的明显干旱期发生在1877-1888年和1923-1933年。降水量在1940-1970年期间剧烈波动,并在1960年的平均值附近变得相对稳定。兴隆山贺兰,宁武和华东地区表明这五条降雨曲线代表了华北中西部环境敏感区的总体降水变化。 CRU网格点的计算也表明这些站点之间存在显着的空间相关性。周期性分析显示在过去155年中,重建系列的清晰23.33年,8.24年,2.64年和2.59年周期,置信水平为99%

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