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Statistical modeling of Southern Ocean marine diatom proxy and winter sea ice data: Model comparison and developments

机译:南大洋海洋硅藻代理和冬季海冰数据的统计建模:模型的比较和发展

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We compare the performance of the modern analog technique (MAT), the Imbrie and Kipp transfer function (IKTF), the generalized additive model (GAM) and weighted averaging partial least squares (WA PLS) on a southern hemisphere diatom relative abundance and winter sea ice concentration training data set. All relevant model assumptions are tested with a random 10-fold cross-validation, whilst a hold out cross-validation tested the explanatory power of each model on spatially independent validation data. We used auto correlograms on model residuals, variance partitioning, and principal coordinates analysis of neighbor matrices (PCNM) to investigate the importance of the spatial structure of our training database. A set of hierarchical logistic regression models (or Huisman-Olff-Fresco models) are used to infer the response of each diatom species along the winter sea ice gradient. Our analyses suggest that IKTF is an inappropriate sea ice estimation approach as its underlying statistical assumptions do not hold and the fit of IKTF to our data under cross-validation was poor. We conclude that MAT may be biased by spatial autocorrelation, and together with IKTF fails to provide unbiased estimates of winter sea ice. We find GAM and WA PLS are more appropriate than IKTF and MAT for the estimation of paleo winter sea ice cover throughout the Southern Ocean. However, as WA PLS is based on a unimodal species response, which is rarely exhibited by diatoms along the winter sea ice gradient, we ultimately advocate the application of GAM. GAM only uses diatoms with a statistically significant association, and ecologically based link, with sea ice. GAM outperformed all other models under cross-validation in terms of performance statistics, the fit of GAM to the training dataset and diagnostic tests for model assumptions. We also demonstrate that GAM provides a more detailed and potentially more accurate (based on a comparison with New Zealand and southeast Australian paleo climatic records) paleo winter sea ice record for the southwestern Pacific Ocean in comparison with IKTF, MAT and WA PLS. (C) 2014 Elsevier Ltd. All rights reserved.
机译:我们比较了南半球硅藻相对丰度和冬季海域上现代模拟技术(MAT),Imbrie和Kipp传递函数(IKTF),广义加性模型(GAM)和加权平均偏最小二乘(WA PLS)的性能。冰浓度训练数据集。所有相关的模型假设均通过随机10倍交叉验证进行了测试,而支持交叉验证则通过空间独立的验证数据测试了每个模型的解释能力。我们对模型残差,方差划分和邻居矩阵的主坐标分析(PCNM)使用自动相关图来研究训练数据库的空间结构的重要性。使用一组分层逻辑回归模型(或Huisman-Olff-Fresco模型)来推断每种硅藻物种沿冬季海冰梯度的响应。我们的分析表明,IKTF是不合适的海冰估算方法,因为其基本的统计假设不成立,并且在交叉验证下IKTF与我们数据的拟合性很差。我们得出的结论是,MAT可能会受到空间自相关的影响,并且与IKTF一起无法提供冬季海冰的无偏估计。我们发现GAM和WA PLS比IKTF和MAT更适合于估计整个南大洋的冬季冬季海冰覆盖。但是,由于WA PLS基于单峰物种响应,而硅藻沿冬季海冰梯度很少出现,因此我们最终提倡GAM的应用。 GAM仅使用硅藻与海冰具有统计学上的显着联系,并且具有生态学上的联系。在性能统计,GAM与训练数据集的拟合以及模型假设的诊断测试方面,GAM在交叉验证方面的表现优于所有其他模型。我们还证明,与IKTF,MAT和WA PLS相比,GAM为西南太平洋的古冬季海冰记录提供了更详细,更准确的信息(基于与新西兰和澳大利亚东南部的古气候记录的比较)。 (C)2014 Elsevier Ltd.保留所有权利。

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  • 来源
    《Progress in Oceanography》 |2015年第2期|100-112|共13页
  • 作者单位

    Macquarie Univ, Fac Sci & Engn, Dept Biol Sci, N Ryde, NSW 2109, Australia;

    Macquarie Univ, Fac Sci & Engn, Dept Stat, N Ryde, NSW 2109, Australia;

    Cal Poly Pomona, Deans Off, Coll Sci, Pomona, CA 91768 USA;

    Univ Bordeaux 1, DGO, UMR CNRS EPOC 5805, F-33405 Talence, France;

    Macquarie Univ, Fac Sci & Engn, Dept Biol Sci, N Ryde, NSW 2109, Australia;

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