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Reconstructing terrestrial temperatures in the Australian sub-tropics and tropics: A chironomid based transfer function approach

机译:重建澳大利亚亚热带和热带地区的地面温度:基于天文学的传递函数方法

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摘要

This paper presents chironomid-based transfer functions for temperature reconstructions intended for use in the Australian tropics and sub-tropics. Temperature was the primary independent control of chironomid assemblages. Two transfer functions were created to infer mean annual (MAT) and mean summer temperature as represented by February temperatures (MFT) as it was not reasonable to automatically assume that chironomid populations in the tropics are controlled by summer temperatures. Weighted average partial least square (WA-PLS) models were the most robust. For MAT they produced a coefficient of determination (r(jack)(2)) of 0.83, a maximum bias of 1.74 degrees C and a root mean squared error of prediction (RMSEP) of 2.35 degrees C while for MFT an r(jack)(2) of 0.76, maximum bias of 2.43 degrees C, and RMSEP of 2.43 degrees C was achieved. Based on the statistics we recommend that the MAT model is used for chironomid work in tropical regions.
机译:本文介绍了打算用于澳大利亚热带地区和亚热带地区的温度重建中基于色氨酸的传递函数。温度是嵌合体组合的主要独立控制。创建两个传递函数来推断年平均温度(MAT)和以2月温度(MFT)表示的夏季平均温度,因为自动假设热带地区的尺虫种群受夏季温度控制是不合理的。加权平均偏最小二乘(WA-PLS)模型最为稳健。对于MAT,他们得出的确定系数(r(jack)(2))为0.83,最大偏差为1.74摄氏度,预测的均方根误差(RMSEP)为2.35摄氏度,而对于MFT,则为r(jack) (2)为0.76,最大偏置为2.43摄氏度,RMSEP为2.43摄氏度。根据统计数据,我们建议将MAT模型用于热带地区的手性工作。

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