论文标题
通过各种编码器解码器降低非线性维度,以了解气候模型中的对流过程
Non-Linear Dimensionality Reduction with a Variational Encoder Decoder to Understand Convective Processes in Climate Models
论文作者
论文摘要
深度学习可以准确地代表气候模型中的子网格尺度对流过程,并从高分辨率模拟中学习。但是,深度学习方法通常由于内部维度较大而缺乏可解释性,从而导致这些方法的可信度降低。在这里,我们使用一种非线性降低降低技术的变量编码器解码器结构(VED)来学习和理解Aquaplanet超级参数气候模型模型中的对流过程,其中深层对流过程被明确模拟。我们表明,与以前的深度学习研究相似,基于馈送神经网络,VED能够学习并准确地再现对流过程。与过去的工作相反,我们表明可以通过将原始信息压入仅五个潜在节点来实现。结果,VED可用于通过探索其潜在维度来理解对流过程和对流模式。对潜在空间的密切研究可以鉴定出不同的对流方案:a)稳定条件明显与深度对流区分开,其外向发动的长波辐射低和强大的降水; b)高光学薄的卷曲样云与低光的浓云云分开; c)浅对流过程与大规模的水分含量和表面绝热加热有关。我们的结果表明,VED可以准确地代表气候模型中的对流过程,同时可以更好地理解亚网格尺度的物理过程,为具有有希望的生成属性的日益解释的机器学习参数铺平了道路
Deep learning can accurately represent sub-grid-scale convective processes in climate models, learning from high resolution simulations. However, deep learning methods usually lack interpretability due to large internal dimensionality, resulting in reduced trustworthiness in these methods. Here, we use Variational Encoder Decoder structures (VED), a non-linear dimensionality reduction technique, to learn and understand convective processes in an aquaplanet superparameterized climate model simulation, where deep convective processes are simulated explicitly. We show that similar to previous deep learning studies based on feed-forward neural nets, the VED is capable of learning and accurately reproducing convective processes. In contrast to past work, we show this can be achieved by compressing the original information into only five latent nodes. As a result, the VED can be used to understand convective processes and delineate modes of convection through the exploration of its latent dimensions. A close investigation of the latent space enables the identification of different convective regimes: a) stable conditions are clearly distinguished from deep convection with low outgoing longwave radiation and strong precipitation; b) high optically thin cirrus-like clouds are separated from low optically thick cumulus clouds; and c) shallow convective processes are associated with large-scale moisture content and surface diabatic heating. Our results demonstrate that VEDs can accurately represent convective processes in climate models, while enabling interpretability and better understanding of sub-grid-scale physical processes, paving the way to increasingly interpretable machine learning parameterizations with promising generative properties