用于区域气候模型预测的深度学习模拟器的可转移性和可解释性:未来应用前景

Jorge Baño-Medina, M. Iturbide, Jesús Fernández, José Manuel Gutiérrez
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摘要

区域气候模式(RCMs)是模拟和研究区域气候变异性和变化的重要工具。然而,其高昂的计算成本限制了涵盖多种情景和跨区域驱动全球气候模型(GCMs)的区域气候预测综合集合的制作。最近推出了基于深度学习模型的 RCM 仿真器,作为一种具有成本效益且前景广阔的替代方法,它只需要短期的 RCM 模拟来训练模型。因此,评估它们对不同时期、情景和 GCM 的可移植性成为一项关键而复杂的任务,其中 GCM 和 RCM 的固有偏差发挥着重要作用。在此,我们将重点放在这个问题上,考虑文献中介绍的完美和不完美两种不同的仿真方法,按照成熟的降尺度术语,我们在此将其分别称为完美预报(PP)和模型输出统计(MOS)。除了标准评估技术外,我们还采用了可解释人工智能(XAI)领域的方法来扩展分析,以评估模型所学经验联系的物理一致性。我们发现,这两种方法都能模拟不同时期和情景下区域气候变化模型的某些气候学特性(软转移性),但模拟功能的一致性因方法而异。PP学习到的是稳健且有物理意义的模式,而MOS的结果则依赖于GCM,在某些情况下缺乏物理一致性。由于存在依赖于 GCM 的偏差,这两种方法在将模拟功能转移到其他 GCM 时都会遇到问题(硬转移性)。这就限制了它们在构建 RCM 集合时的适用性。最后,我们展望了未来的应用前景。
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Transferability and explainability of deep learning emulators for regional climate model projections: Perspectives for future applications
Regional climate models (RCMs) are essential tools for simulating and studying regional climate variability and change. However, their high computational cost limits the production of comprehensive ensembles of regional climate projections covering multiple scenarios and driving Global Climate Models (GCMs) across regions. RCM emulators based on deep learning models have recently been introduced as a cost-effective and promising alternative that requires only short RCM simulations to train the models. Therefore, evaluating their transferability to different periods, scenarios, and GCMs becomes a pivotal and complex task in which the inherent biases of both GCMs and RCMs play a significant role. Here we focus on this problem by considering the two different emulation approaches introduced in the literature as perfect and imperfect, that we here refer to as Perfect Prognosis (PP) and Model Output Statistics (MOS), respectively, following the well-established downscaling terminology. In addition to standard evaluation techniques, we expand the analysis with methods from the field of eXplainable Artificial Intelligence (XAI), to assess the physical consistency of the empirical links learnt by the models. We find that both approaches are able to emulate certain climatological properties of RCMs for different periods and scenarios (soft transferability), but the consistency of the emulation functions differ between approaches. Whereas PP learns robust and physically meaningful patterns, MOS results are GCM-dependent and lack physical consistency in some cases. Both approaches face problems when transferring the emulation function to other GCMs (hard transferability), due to the existence of GCM-dependent biases. This limits their applicability to build RCM ensembles. We conclude by giving prospects for future applications.
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