Modeling and empirical orthogonal function analysis of plasmaspheric electron content based on MetOp satellites

Tao, Xiangwu; Li, Shuhui; Zhou, Wu; Ji, Ming; Mao, Pengrui; Xiong, Shao-Jie

doi:10.1007/s10509-023-04177-3

Cited by 1 publication

(1 citation statement)

References 34 publications

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“…Chen et al proposed a mapping technique for generating gridded PEC maps using topside measurements of the COSMIC and MetOp-A constellations at an orbital altitude of around 800 km [23]. Tao et al analyzed the seasonal variations in the global PEC at LT 9:30 and 21:30 in 2020 using the EOF analysis method and dense PEC measurements from the MetOp-A, -B, and -C, and they further compared the differences of the major EOF modes between PEC and GNSS-TEC [24].…”

Section: Introductionmentioning

confidence: 99%

An EOF-Based Global Plasmaspheric Electron Content Model and Its Potential Role in Vertical-Slant TEC Conversion

Long,

Gao,

Dong

et al. 2024

Remote Sensing

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Topside total electron content (TEC) data measured by COSMIC/FORMAT-3 during 2008 and 2016 were used to analyze and model the global plasmaspheric electron content (PEC) above 800 km with the help of the empirical orthogonal function (EOF) analysis method, and the potential role of the proposed PEC model in helping Global Navigation Satellite System (GNSS) users derive accurate slant TEC (STEC) from existing high-precision vertical TEC (VTEC) products was validated. A uniform gridded PEC dataset was first obtained using the spherical harmonic regression method, and then, it was decomposed into EOF basis modes. The first four major EOF modes contributed more than 99% of the total variance. They captured the pronounced latitudinal gradient, longitudinal differences, hemispherical differences, diurnal and seasonal variations, and the solar activity dependency of global PEC. A second-layer EOF decomposition was conducted for the spatial pattern and amplitude coefficients of the first-layer EOF modes, and an empirical PEC model was constructed by fitting the second-layer basis functions related to latitude, longitude, local time, season, and solar flux. The PEC model was designed to be driven by whether solar proxy or parameters derived from the Klobuchar model meet the real-time requirements. The validation of the results demonstrated that the proposed PEC model could accurately simulate the major spatiotemporal patterns of global PEC, with a root-mean-square (RMS) error of 1.53 and 2.24 TECU, improvements of 40.70% and 51.74% compared with NeQuick2 model in 2009 and 2014, respectively. Finally, the proposed PEC model was applied to conduct a vertical-slant TEC conversion experiment with high-precision Global Ionospheric Maps (GIMs) and dual-frequency carrier phase observables of more than 400 globally distributed GNSS sites. The results of the differential STEC (dSTEC) analysis demonstrated the effectiveness of the proposed PEC model in aiding precise vertical-slant TEC conversion. It improved by 18.52% in dSTEC RMS on a global scale and performed better in 90.20% of the testing days compared with the commonly used single-layer mapping function.

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Section: Introductionmentioning

confidence: 99%