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Global ionospheric modeling based on multi-GNSS, satellite altimetry, and Formosat-3/COSMIC data

机译:基于多GNSS,卫星Altimetry和Formosat-3 / Cosmic数据的全局电离层建模

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摘要

Ionosphere total electron content (TEC) from global ionospheric maps (GIM) is widely applied in both ionospheric delay correction and research on space weather monitoring. Global ionospheric modeling based on multisource data is an effective method to improve conventional GIM accuracy and reliability. In this study, a global ionospheric model is constructed from multi-GNSS (here, GPS/GLONASS/BDS), satellite altimetry and Formosat-3/COSMIC (F3/C) observations using a spherical harmonic (SH) function. The results show that compared to the conventional GIM derived from GPS/GLONASS data, the combined GIM performance from multisource data improves significantly; the RMS versus external data decreases from [2, 5] to [2, 3] TECU, and the BIAS decreases from [- 3, 1] to [- 1, 1] TECU. Specifically, BDS observations improve the IPP distributions, especially over the region of Australia; compared with GPS-based ionospheric TEC. Our calculated GIM with BDS data has better performance than that without BDS data. By combining JASON 2 and GPS/GLONASS data, the residual distribution is more concentrated, and the RMS is improved effectively in mid-high latitudes of the southern hemisphere and in the equatorial region. F3/C TEC also exhibits relatively minor improvements on GIM; the standard deviation reduces from 2.89 to 1.92 TECU, and the BIAS regarding extra F3/C data decreases from - 2.02 to - 1.71 TECU.
机译:来自全局电离层图(GIM)的电离层总电子含量(TEC)广泛应用于电离层延迟校正和太空天气监测研究。基于多源数据的全局电离层建模是提高传统GIM精度和可靠性的有效方法。在本研究中,使用球形谐波(SH)功能,从多GNSS(这里,GPS / GLONASS / BDS),卫星高度测定和Formosat-3 / Cosmic(F3 / C)观察构成全局电离层模型。结果表明,与来自GPS / GLONASS数据的传统GIM相比,来自多源数据的组合GIM性能显着提高; RMS与外部数据从[2,5]降低到[2,3] TECU,并且偏置从[ - 3,1]到[ - 1,1] TECU。具体而言,BDS观察改善了IPP分布,特别是在澳大利亚地区;与基于GPS的电离层TEC相比。我们的计算GDS数据具有比没有BDS数据的更好的性能。通过组合Jason 2和GPS / GLONASS数据,剩余分布更集中,并且RMS在南半球的中高纬度和赤道区域中有效地提高。 F3 / C TEC也表现出对GIM的相对较小的改进;标准偏差从2.89降至1.92 TECU,关于额外的F3 / C数据的偏差从-2.02到-1.71 TECU减少。

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