Usually, ionospheric Total Electron Conten (TEC) variation with time can be viewed as a stationary random process under quiet conditions.
平静状态下电离层总电子含量(TEC)随时间的变化通常可以视为平稳随机过程。
Applying the coupling methods, the author establishes the stability in total variation for the diffusion process corresponding to the mean-field model.
应用耦合方法，建立了相应于这个平均场模型的扩散过程的依全变差稳定性。
Applying the coupling methods, the author establishes the stability in total variation for the diffusion process corresponding to the mean-field model.
应用耦合方法，建立了相应于这个平均场模型的扩散过程的依全变差稳定性。
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