摘要
本文基于IRI模型、地面数字测高仪和GNSS TEC数据,提出了一种利用经验正交函数(Empirical Orthogonal Function,简称EOF)估算顶部电离层电子密度剖面的方法,并将其应用于美国Millstone Hill测高仪和GNSS数据以估算顶部电离层电子密度剖面.通过将估算的临界频率、峰值高度、400km以上电子密度分别与测高仪实测临界频率、测高仪实测峰值高度以及非相干散射雷达实测400km以上电子密度作对比以对方法的有效性进行验证.统计结果显示估算临界频率、峰值高度与测高仪实测数据基本一致,400km以上估算电子密度相较于非相干散射雷达实测的绝对误差平均值仅是测高仪推算400km以上电子密度绝对误差平均值的一半左右.所以本文提出的方法可以更加精确地估算顶部电离层电子密度.
Based on the international reference ionosphere(IRI)model,digital ionosonde and GNSS TEC data,we proposed a method which uses the empirical orthogonal function to estimate the topside ionospheric electron density profile and applied it to the Millstone Hill station.We then compared the estimated critical frequency and peak height with the digital ionosonde observations,and compared the estimated electron density above 400 km with density observed by incoherent scatter radar(ISR).Statistical results show that the estimated critical frequency and peak height are in consistent with the digital ionosonde data,the absolute error between modeled and ISR measured density above 400 km reduces 50%in comparison with that between digital ionosonde derivations and ISR.In summary,adding GNSS TEC in addition to digisonde could improve the topside ionospheric electron density estimation by our method accurately.
引文
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