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首页> 外文期刊>The holocene >Potential bias in 'updating' tree-ring chronologies using regional curve standardisation: Re-processing 1500 years of Tornetraesk density and ring-width data
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Potential bias in 'updating' tree-ring chronologies using regional curve standardisation: Re-processing 1500 years of Tornetraesk density and ring-width data

机译:使用区域曲线标准化在“更新”树年轮年代中的潜在偏差:重新处理1500年的Tornetraesk密度和年轮宽度数据

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摘要

We describe the analysis of existing and new maximum-latewood-density (MXD) and tree-ring width (TRW) data from the Tornetrask region of northern Sweden and the construction of 1500 year chronologies. Some previous work found that MXD and TRW chronologies from Tornetrask were inconsistent over the most recent 200 years, even though they both reflect predominantly summer temperature influences on tree growth. We show that this was partly a result of systematic bias in MXD data measurements and partly a result of inhomogeneous sample selection from living trees (modern sample bias). We use refinements of the simple Regional Curve Standardisation (RCS) method of chronology construction to identify and mitigate these biases. The new MXD and TRW chronologies now present a largely consistent picture of long-timescale changes in past summer temperature in this region over their full length, indicating similar levels of summer warmth in the medieval period (MWP, c. CE 900-1100) and the latter half of the 20th century. Future work involving the updating of MXD chronologies using differently sourced measurements may require similar analysis and appropriate adjustment to that described here to make the data suitable for the production of un-biased RCS chronologies. The use of 'growth-rate' based multiple RCS curves is recommended to identify and mitigate the problem of 'modern sample bias'.
机译:我们描述了对来自瑞典北部Tornetrask地区的现有和新的最大latewood密度(MXD)和树年轮宽度(TRW)数据的分析,以及1500年时间序列的构建。以前的一些工作发现,Tornetrask的MXD和TRW时间顺序在最近200年中不一致,即使它们都主要反映了夏季温度对树木生长的影响。我们表明,这部分是由于MXD数据测量中的系统性偏见的结果,而部分是由于从活树中选择不均匀的样本(现代样本偏见)的结果。我们使用按时间顺序构造的简单区域曲线标准化(RCS)方法的改进方法来识别和缓解这些偏差。现在,新的MXD和TRW年表在很大程度上反映了该地区过去夏季温度在整个长度上的长期尺度变化,表明中世纪时期的夏季温暖水平相似(MWP,c。CE 900-1100)和20世纪下半叶。涉及使用不同来源的测量值更新MXD时序的未来工作可能需要进行类似的分析,并对此处所述内容进行适当的调整,以使数据适合于产生无偏的RCS时序。建议使用基于“增长率”的多个RCS曲线来识别和缓解“现代样本偏差”的问题。

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