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Partitioning Uncertainty Components of an Incomplete Ensemble of Climate Projections Using Data Augmentation

机译:使用数据增强分区气候投影的不完整集合的不确定性组件

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The quantification of uncertainty sources in ensembles of climate projections obtained from combinations of different scenarios and climate and impact models is a key issue in climate impact studies. The small size of the ensembles of simulation chains and their incomplete sampling of scenario and climate model combinations makes the analysis difficult. In the popular single-time ANOVA approach for instance, a precise estimate of internal variability requires multiple members for each simulation chain (e.g., each emission scenario-climate model combination), but multiple members are typically available for a few chains only. In most ensembles also, a precise partition of model uncertainty components is not possible because the matrix of available scenario/models combinations is incomplete (i.e., projections are missing for many scenario-model combinations). The method we present here, based on data augmentation and Bayesian techniques, overcomes such limitations and makes the statistical analysis possible for single-member and incomplete ensembles. It provides unbiased estimates of climate change responses of all simulation chains and of all uncertainty variables. It additionally propagates uncertainty due to missing information in the estimates. This approach is illustrated for projections of regional precipitation and temperature for four mountain massifs in France. It is applicable for any kind of ensemble of climate projections, including those produced from ad hoc impact models.
机译:从不同情景和气候和影响模型的组合获得的气候预测集中的不确定性来源是气候影响研究的关键问题。模拟链的尺寸的小尺寸及其情景和气候模型组合的不完整采样使得分析困难。例如,在流行的单时间Anova方法中,内部变异性的精确估计需要每个模拟链的多个成员(例如,每个发射场景 - 气候模型组合),但多个成员通常仅适用于几个链条。在大多数集合中,由于可用场景/型号组合的矩阵不完整的模型不确定性组件的精确分区是不可能的(即,对于许多场景模型组合缺少投影)。我们在此基于数据增强和贝叶斯技术的方法克服了这些限制,并使单个成员和不完整的合并成为可能的统计分析。它提供了对所有模拟链的气候变化响应和所有不确定性变量的无偏估计。它另外传播由于估计中缺少的信息而传播不确定性。示出了这种方法,用于法国四个山地暴力的区域降水和温度的预测。它适用于气候预测的任何类型的整体,包括由Ad Hoc Impact模型生产的集合。

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