首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Three-dimensional ionospheric tomography using observation data of GPS ground receivers and ionosonde by neural network
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Three-dimensional ionospheric tomography using observation data of GPS ground receivers and ionosonde by neural network

机译:利用神经网络利用GPS地面接收器和离子探空仪的观测数据进行三维电离层层析成像

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In this paper we present a new method based on a Residual Minimization Training Neural Network (RMTNN) to reconstruct the three-dimensional electron density distribution of the local ionosphere with high spatial resolution (about 50 km × 50 km in east/west and 30 km in altitude) using GPS and ionosonde observation data. In this method we reconstruct an approximate three-dimensional electron density distribution as a computer tomographic image by making use of the excellent capability of a multilayer neural network to approximate an arbitrary function. For this application the network training is carried out by minimizing the squared residuals of an integral equation. We combine several additional techniques with the new method, i.e., input space discretization, use of ionosonde observation data to improve the vertical resolution, automatic estimation of the biases of the satellite and the ground receivers by using the parameter estimation method, and estimation of plasmasphere contributions to the total electron content on the basis of an assumption of diffusive equilibrium with constant scale height. Numerical experiments for the actual positions of the GPS satellites and the ground receivers are used to validate the reliability of the method. We also applied the method to the analysis of real observation data and compared the results with ionosonde observations which were not used for the network training.
机译:在本文中,我们提出了一种基于残差最小化训练神经网络(RMTNN)的新方法,该方法可重建具有高空间分辨率(东西向约为50 km×50 km,而东西向约为30 km)的电离层的三维电子密度分布使用GPS和离子探空仪观测数据。在这种方法中,我们利用多层神经网络的出色功能来近似任意函数,从而将近似三维电子密度分布重建为计算机断层扫描图像。对于此应用,网络训练是通过最小化积分方程的平方残差来进行的。我们将几种其他技术与新方法相结合,例如输入空间离散化,使用电离探空仪观测数据来提高垂直分辨率,通过使用参数估计方法自动估计卫星和地面接收器的偏置以及估计等离子层在恒定标尺高度的扩散平衡假设的基础上,对总电子含量的贡献。 GPS卫星和地面接收器的实际位置的数值实验用于验证该方法的可靠性。我们还将该方法应用于实际观测数据的分析,并将结果与​​未用于网络训练的离子探空仪观测结果进行了比较。

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