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A Combined Neural Network- and Physics-Based Approach for Modeling Plasmasphere Dynamics

机译:结合神经网络和基于物理等离子体层动力学建模方法

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In recent years, feedforward neural networks (NNs) have been successfully applied to reconstruct global plasmasphere dynamics in the equatorial plane. These neural network-based models capture the large-scale dynamics of the plasmasphere, such as plume formation and erosion of the plasmasphere on the nightside. However, their performance depends strongly on the availability of training data. When the data coverage is limited or non-existent, as occurs during geomagnetic storms, the performance of NNs significantly decreases, as networks inherently cannot learn from the limited number of examples. This limitation can be overcome by employing physics-based modeling during strong geomagnetic storms. Physics-based models show a stable performance during periods of disturbed geomagnetic activity if they are correctly initialized and configured. In this study, we illustrate how to combine the neural network- and physics-based models of the plasmasphere in an optimal way by using data assimilation. The proposed approach utilizes advantages of both neural network- and physics-based modeling and produces global plasma density reconstructions for both quiet and disturbed geomagnetic activity, including extreme geomagnetic storms. We validate the models quantitatively by comparing their output to the in-situ density measurements from RBSP-A for an 18-month out-of-sample period from June 30, 2016 to January 01, 2018 and computing performance metrics. To validate the global density reconstructions qualitatively, we compare them to the IMAGE EUV images of the He+ particle distribution in the Earth's plasmasphere for a number of events in the past, including the Halloween storm in 2003.
机译:近年来,前馈神经网络(NNs)已经成功地应用于重建在赤道全球等离子体层动态飞机。大型等离子体层的动力学,如羽流形成和侵蚀在阴面等离子体层。性能很大程度上取决于可用性的训练数据。有限的或不存在的,因为发生在地磁风暴,得到的性能大幅减少,网络本身不能从数量有限的例子。这种限制可以克服采用基于物理建模期间强烈地磁风暴。表演期间打扰地磁活动是否正确初始化和配置。说明如何结合神经网络和基于物理模型的等离子体层利用数据同化的最佳方式。建议的方法利用两者的优势神经网络和基于物理建模和产生全球等离子体密度重建地磁宁静和不安活动,包括极端的地磁风暴。我们定量的验证模型比较它们的输出到现场密度测量从RBSP-A 18个月样本外期从2016年6月30日2018年1月1日和计算性能指标。重建定性,我们进行比较他的形象EUV图像+粒子分布在地球的等离子体层过去的事件,包括在2003年万圣节风暴。

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