基于一维残差卷积神经网络的Pi2脉动识别模型

    Identification Model of Pi2 Pulsation Based on One-dimensional Residual Convolutional Neural Network

    • Pi2脉动是一种不规则的超低频波(Ultra-Low Frequency, ULF), 是磁层与电离层耦合的重要瞬态响应, 其发生与亚暴爆发有密切的关系. Pi2脉动作为地球磁层中的一种扰动现象, 其发生信号隐藏在地磁场分量观测数据中. 面对持续增长的观测数据量, 如何有效地判断某段地磁场分量观测数据中是否有Pi2脉动发生, 是构建Pi2脉动识别模型的关键. 利用子午工程磁通门磁力仪观测的地磁场分量数据, 基于一维残差卷积神经网络(One-Dimensional Residual Convolutional Neural Network, 1D-ResCNN), 构建了一个端到端的Pi2脉动识别模型, 用于判别某段地磁场分量观测数据中是否有Pi2脉动发生. 实验结果表明, 该模型与现有公开发表的Pi2脉动机器学习识别模型相比, 具有更高的识别准确率和更低的虚报率、漏报率.

       

      Abstract: Pi2 pulsations are irregular ultra-low frequency waves, representing a significant transient response to the coupling between the magnetosphere and ionosphere. Their occurrence is associated with onset of substorms. As a disturbance phenomenon in the Earth’s magnetosphere, the occurrence signal of Pi2 pulsations is hidden within the observation data of geomagnetic field components. Addressing the increasing amount of observation data, how to efficiently determine whether Pi2 pulsation has occurred in a segment of geomagnetic field component observational data is the key to build a Pi2 pulsation identification model. Based on the time series observation data of the FGM from the Chinese Meridian Project and One-Dimensional Residual Convolutional Neural Network (1D-ResCNN), this paper establishes an end-to-end Pi2 pulsation identification model. This model can distinguish whether Pi2 pulsation occurs in the observation data of a certain geomagnetic field component. Experimental results show that this model has higher recognition accuracy and lower false positive rate and false negative rate than the existing Pi2 pulsation machine learning identification model.

       

    /

    返回文章
    返回