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Tree-ring δ~(18)O, a tool to crack the paleo-hydroclimatic code in subtropical China

机译:树环δ〜(18)o,一种破解亚热带古水蛭码的工具

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摘要

Tree ring plays an important role in deciphering the paleoclimatic signals. Although tree-ring width (TRW) has obvious advantages in studying the hydroclimatic history in the middle-high latitudes, it has certain limitation in hydroclimatic signal extraction in the tropical to subtropical areas, which greatly limits our fully understanding about the hydroclimatic history in these areas. In this work, tree-ring delta O-18 (delta O-18(tree)) records from five independent tree-ring cores were measured and a composite delta O-18(tree) record (1939-2014) was developed in Guilin, subtropical southwest China. No "juvenile effect" existed in this delta O-18(tree) record and no relationship was found between delta O-18(tree) and TRW. Correlation analysis with the climatic parameters demonstrated that the delta(18)O(tree )record significantly (p 0.01) and negatively correlated with all the hydroclimatic parameters during the growing season (e.g. April-October precipitation, August-October relative humidity and April-November standardized precipitation -evapotranspiration index), while it only positively correlated with the August-September mean temperature (p 0.05). At high frequency, the above relationships were greatly strengthened. Compared with the temperature-limited TRW in Guilin and other areas of subtropical China, delta(18)O(tree )was a better choice for hydroclimatic reconstruction. Moreover, the delta O-18(tree) record in Guilin showed high consistency with other moisture-sensitive delta(18)O(tree )records in a large area of central-southeastern China. Analysis revealed that both large-scale circulation system (e.g. Indian summer monsoon, ENSO, westerlies) and local weather system significantly influenced the growing-season hydroclimatic variation in the study area. This study provides great potential for extracting hydroclimatic information from longer-living trees in subtropical China. (C) 2017 Elsevier Ltd and INQUA. All rights reserved.
机译:树戒指在破译古跨线信号时起着重要作用。虽然树木宽度(TRW)在研究中高纬度的循环历史方面具有明显的优势,但它对热带地区的液压信号提取有一定的限制,亚热带地区大大限制了我们对这些循环史上的完全理解地区。在这项工作中,测量了来自五个独立树圈核的树木ΔO-18(Delta O-18(树))记录,并在桂林开发了复合ΔO-18(树)记录(1939-2014) ,亚热带西南中国。在该ΔO-18(树)记录中没有“少年效应”存在,并且在Delta O-18(树)和TRW之间没有任何关系。与气候参数的相关性分析表明,Δ(18)O(树)显着记录(P <0.01),与生长季节期间的所有循环参数呈负相关(例如,4月至10月 - 10月 - 10月的相对湿度和4月至11月标准化降水 - 臂散液指数),而它只与8月至9月的平均温度正相关(P <0.05)。在高频时,上述关系大大加强了。与桂林温度有限的TRW相比,亚热带中国的其他地区,Delta(18)O(树)是液压革动物重建的更好选择。此外,桂林中的Delta O-18(树)记录与中国东南部大面积的其他水分敏感的三角洲(18)o(树)记录显示出高一致性。分析表明,大型循环系统(例如印度夏季季风,ENSO,Westerlies)和局部天气系统的显着影响了研究区的生长季节性循环变异。本研究提供了从亚热带亚热带地区从长生动的树木中提取循环信息的巨大潜力。 (c)2017年Elsevier Ltd和诊断。版权所有。

著录项

  • 来源
    《Quaternary International》 |2018年第10期|3-11|共9页
  • 作者单位

    Chinese Acad Sci Inst Earth Environm State Key Lab Loess & Quatemary Geol Xian 710075 Shaanxi Peoples R China;

    Chinese Acad Sci Inst Earth Environm State Key Lab Loess & Quatemary Geol Xian 710075 Shaanxi Peoples R China|Beijing Normal Univ IRCESF Beijing 100875 Peoples R China|Beijing Normal Univ JCGCS Beijing 100875 Peoples R China|Nanjing Univ Sch Earth Sci & Engn Nanjing 210046 Jiangsu Peoples R China;

    Chinese Acad Sci Inst Earth Environm State Key Lab Loess & Quatemary Geol Xian 710075 Shaanxi Peoples R China|Univ Chinese Acad Sci Beijing 100049 Peoples R China;

    Chinese Acad Sci Inst Earth Environm State Key Lab Loess & Quatemary Geol Xian 710075 Shaanxi Peoples R China;

    Chinese Acad Sci Inst Earth Environm State Key Lab Loess & Quatemary Geol Xian 710075 Shaanxi Peoples R China;

    Chinese Acad Sci Inst Earth Environm State Key Lab Loess & Quatemary Geol Xian 710075 Shaanxi Peoples R China|Univ Chinese Acad Sci Beijing 100049 Peoples R China;

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

    Hydroclimatic proxy; ENSO; Asian summer monsoon; Growing season; Tree-ring delta O-18;

    机译:水加工代理;Enso;亚洲夏季季风;生长季节;树戒指达到O-18;

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