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Growing-season precipitation since 1872 in the coastal area of subtropical southeast China reconstructed from tree rings and its relationship with the East Asian summer monsoon system

机译:从树木年轮重建的1872年以来中国亚热带东南沿海地区的生长季节降水及其与东亚夏季风系统的关系

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摘要

Tree rings from temperate zones of the world have provided abundant palaeo-ecological and paleo-hydroclimatic information. However, tree rings from subtropical to tropical regions remain relatively scarce, which greatly limit our fully understanding about the climate change issues. In the present work, tree-ring-width (TRW) measurements of Masson pine from Fujian province, the coastal area of subtropical southeast China were successfully crossdated and a TRW STD chronology was developed from 1854 to 2012. Significantly positive correlation was identified between the tree rings and April November total precipitation (r = 0.71, p < 0.01). The reconstructed April November precipitation exhibited two comparatively wet (1876-1886 and 1957-1962) and one comparatively dry (1986-2004) periods. An evident drying trend since 1959 was seen and it was mitigated after 1993. Most of the extreme low-precipitation years in the reconstruction were supported by the historical records. As revealed by the spatial correlation patterns, our precipitation reconstruction was also consistent with other hydroclimatic records along the coastal areas of southeast China, proving its ability to capture the large-scale hydrological signal in southeast China (mainly refers to the south of the middle-lower reaches of Yangtze River). The reconstructed precipitation showed significant correlation with the East Asian summer Monsoon (EASM) index. Moreover, it also indicated simultaneous variation with the monsoon precipitation in North China on a decadal scale, implying that growing season precipitation variations in both regions were influenced by the EASM strength. This work highlights the potential of using tree-ring width to reconstruct precipitation in subtropical southeast China, while the relevant issues about precipitation variation in this region is far from resolved.
机译:来自世界温带地区的年轮提供了丰富的古生态和古水文气候信息。但是,从亚热带到热带地区的年轮仍然相对稀少,这极大地限制了我们对气候变化问题的充分理解。在目前的工作中,成功地横穿了来自福建省,中国亚热带东南沿海地区的马尾松的年轮宽度(TRW)测量,并开发了1854年至2012年的TRW STD年表。年轮和四月十一月的总降水量(r = 0.71,p <0.01)。重建的4月11月降水表现出两个相对较湿的时期(1876-1886年和1957-1962年)和一个相对较干的时期(1986-2004年)。自1959年以来就出现了明显的干燥趋势,1993年以后有所减轻。在重建过程中,大多数极端低降水年份都得到了历史记录的支持。正如空间相关性模式所揭示的,我们的降水重建也与中国东南沿海地区的其他水文气候记录相吻合,证明了其捕获中国东南部大型水文信号的能力(主要指中南部)。长江下游)。重建的降水与东亚夏季风(EASM)指数显示显着相关。而且,这也表明华北地区季风降水同时发生了十年的变化,这表明这两个地区的生长期降水变化都受到了EASM强度的影响。这项工作突显了利用树轮宽度重建中国亚热带东南部地区降水的潜力,而与该地区降水变化有关的问题尚未得到解决。

著录项

  • 来源
    《Ecological indicators》 |2017年第11期|441-450|共10页
  • 作者单位

    Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Shaanxi, Peoples R China|Beijing Normal Univ, Interdisciplinary Res Ctr Earth Sci Frontier IRCE, Beijing 100875, Peoples R China|Beijing Normal Univ, JCGCS, Beijing 100875, Peoples R China;

    Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Shaanxi, Peoples R China|Beijing Normal Univ, Interdisciplinary Res Ctr Earth Sci Frontier IRCE, Beijing 100875, Peoples R China|Beijing Normal Univ, JCGCS, Beijing 100875, Peoples R China|Xi An Jiao Tong Univ, Sch Human Settlements & Civil Engn, Dept Earth & Environm Sci, Xian 710049, Shaanxi, Peoples R China;

    Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Shaanxi, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;

    Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Shaanxi, Peoples R China|Xi An Jiao Tong Univ, Sch Human Settlements & Civil Engn, Dept Earth & Environm Sci, Xian 710049, Shaanxi, Peoples R China;

    Xingtai Univ, Dept Geog, Xingtai 054001, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Subtropical southeast China; Tree ring; Growing season; Precipitation reconstruction; Spatial hydrological signal; East Asian summer monsoon;

    机译:中国亚热带东南;树木年轮;生长季节;降水重建;空间水文信号;东亚夏季风;

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