Probabilistic storyline attribution using machine learning
使用机器学习的概率性故事线归因
Frieder Loer, Maybritt Schillinger, Sebastian Sippel
AI总结 提出分布自编码器(DAE)方法,基于大气环流状态和全球变暖水平生成气候反事实,用于概率性故事线归因,并以2003年欧洲热浪为例展示了条件强度和概率比的变化。
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- main text: 19 pages and 4 figures
气候归因的一个基本目标是估计强迫气候变化如何影响观测到的极端天气事件。故事线归因方法将观测到的天气事件(以其大气动态状态即大气环流为条件)与当前“事实”气候中的事件进行比较,并与假设的“反事实”气候中具有非常相似环流条件的事件进行比较。然而,物理气候模型无法直接在不同气候强迫状态下转移这些故事线反事实。统计和机器学习技术可能克服这一限制;然而,在不同气候状态下模拟环流条件极端事件具有挑战性。在这里,我们展示了分布自编码器(DAE)作为一种生成气候反事实的通用方法。它们以大气环流状态和平均全球变暖水平为条件,对欧洲空间分辨温度场的完整分布进行建模。这些分布允许推导有意义的条件概率比,这是基于DAE的故事线方法的一个特殊优势。我们在完全耦合的气候模型模拟上训练DAE,并评估在不同事实和基于故事线的反事实气候模型模拟中的建模分布。在一个说明性案例研究中,我们重新审视了2003年欧洲热浪,并使用ERA5环流为假设的“类似2003年的欧洲热浪”生成反事实,我们假设该热浪发生在2003年后的四分之一世纪(2028年)和半个世纪(2053年)。条件强度将从2003年的29.3°C增加到2028年的30.3°C和2053年的32.1°C,与2003年相比,条件概率比分别为2.1和3.2。
A fundamental goal in climate attribution is to estimate how forced climate change contributes to observed extreme weather events. The storyline attribution method compares an observed weather event, conditional on its atmospheric dynamic state (i.e., atmospheric circulation), in the current, 'factual' climate to an event with very similar circulation conditions in a hypothetical, 'counterfactual' climate. However, physical climate models cannot directly transfer these storyline counterfactuals across different climate forcing states. Statistical and machine learning techniques may overcome this limitation; yet, emulating circulation-conditional extreme events under different climate states is challenging. Here, we demonstrate distributional autoencoders (DAEs) as a versatile method for generating climate counterfactuals. They model the full distribution of spatially resolved European temperature fields conditional on the atmospheric circulation state and the mean global warming level. These distributions allow for deriving meaningful conditional probability ratios, which is a particular advantage of the DAE-based storyline approach. We train DAEs on fully coupled climate model simulations and we evaluate the modelled distributions across different factual and storyline-based counterfactual climate model simulations. In an illustrative case study, we revisit the 2003 European heatwave and we generate counterfactuals for a hypothetical `2003-like European heatwave' using ERA5 circulation, which we hypothesize to occur a quarter century (2028) and a half century (2053) after 2003. The conditional intensity would increase from 29.3 °C in 2003, to 30.3 °C and 32.1 °C in 2028 and 2053, respectively and conditional probability ratios would be 2.1 and 3.2 when compared to 2003.