Supplementary material to "Overcoming model instability in tree-ring-based temperature reconstructions using a multi-species method: A case study from the Changbai Mountains, northeastern China"

Liangjun Zhu, Shuguang Liu, Haifeng Zhu, D. Cooper, D. Yuan, Yu Zhu, Zongshan Li, Yuandong Zhang, Hanxue Liang, Xu Zhang, Wenqi Song, Xiaochun Wang
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Abstract

Abstract. The unstable sensitivity of growth-climate relationships greatly restricts tree-ring-based paleoclimate reconstructions, especially in areas with frequent divergence problems, such as the temperate zone in northeast China. Here, we propose an original tree-species mixing method to overcome this obstacle and improve the stability and reliability of reconstruction models. We take the tree-ring based growing-season minimum temperature reconstruction for the northern Changbai Mountains in northeast China as an example to illustrate the method. Compared with previous temperature reconstruction models, our reconstruction model is more stable and reliable and explains up to 68 % of the variance. It is also highly consistent with historical records and tree-ring-based temperature reconstructions from the nearby Xiaoxing'an Mountains and from across the Northern Hemisphere. Our reconstruction uses two different tree species and is more accurate than temperature reconstructions developed from a single species. Over the past 259 years (AD 1757–2015), five significant cold periods and five warm periods were identified. The reconstruction indicates rapid warming since the 1980s, which is consistent with other instrumental and reconstructed records. We also found the Atlantic Multidecadal Oscillation plays a crucial role in driving the growing-season minimum temperature in the northern Changbai Mountains.
“利用多物种方法克服基于树木年轮的温度重建模式的不稳定性:以长白山为例”的补充材料
摘要生长-气候关系的不稳定敏感性极大地限制了基于树木年轮的古气候重建,特别是在东北温带等频繁出现辐散问题的地区。在此,我们提出了一种原始树种混合方法来克服这一障碍,提高重建模型的稳定性和可靠性。以长白山北部树木年轮的生长季节最低温度重建为例,对该方法进行了说明。与以往的温度重建模型相比,我们的重建模型更加稳定可靠,可以解释高达68%的方差。它也与历史记录和来自附近小兴安岭和整个北半球的基于树木年轮的温度重建高度一致。我们的重建使用了两种不同的树种,比单一树种的温度重建更准确。在过去的259年(公元1757年至2015年)中,确定了五个显著的冷期和五个显著的暖期。重建结果表明,自20世纪80年代以来气候迅速变暖,这与其他仪器和重建记录一致。大西洋多年代际振荡对长白山北部生长期最低气温的影响也非常显著。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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