Ionospheric tomography for SWARM satellite orbit determination using single-frequency GNSS data

被引:0
|
作者
Prol, Fabricio S. [1 ,2 ]
Pignalberi, Alessio [3 ]
Smirnov, Artem [4 ,5 ]
Pezzopane, Michael [3 ]
Christovam, Ana L. [6 ]
Selvan, Kannan [2 ]
Hoque, Mainul [7 ]
Kaasalainen, Sanna [1 ]
机构
[1] Finnish Geospatial Res Inst FGI, Dept Nav & Positioning, Espoo 02150, Finland
[2] Univ Vaasa, Sch Technol & Innovat, Wolffintie 32, Vaasa 65200, Finland
[3] Ist Nazl Geofis & Vulcanol INGV, Via Vigna Murata 605, I-00143 Rome, Italy
[4] Ludwig Maximilian Univ Munich LMU, Dept Earth & Environm Sci, Theresien str 41, D-80333 Munich, Germany
[5] Helmholtz Ctr Potsdam, GFZ German Res Ctr Geosci, Telegrafenberg, D-14473 Potsdam, Germany
[6] Sao Paulo State Univ UNESP, Dept Cartog, BR-19060900 Presidente Prudente, SP, Brazil
[7] German Aerosp Ctr DLR, Inst Solar Terr Phys, Kalkhorstweg 53, D-17235 Neustrelitz, Germany
关键词
Low earth orbit; Ionosphere; Swarm; GPS; Tomography; GRAPHIC; Geomagnetic storm; GPS RECEIVER;
D O I
10.1007/s10291-024-01779-4
中图分类号
TP7 [遥感技术];
学科分类号
081102 ; 0816 ; 081602 ; 083002 ; 1404 ;
摘要
Ionospheric tomography offers three-dimensional (3D) description of the electron density distribution, enabling the direct incorporation of electron density data into the slant total electron content (STEC) computation. As a result, STEC derived from tomography helps mitigate the ionospheric delay experienced in the line of sight between global navigation satellite systems (GNSS) and satellites positioned in low Earth orbits (LEO). Tomography can therefore be effectively employed to correct single-frequency GNSS observations and allow enhanced positioning of spaceborne platforms. We demonstrate the accuracy and performance of a global-scale ionospheric tomography method for determining satellite orbits, utilizing single-frequency GNSS measurements combined with a precise point positioning (PPP) algorithm. We compare the tomographic outcomes against orbit determination derived from the GRoup and PHase ionospheric correction (GRAPHIC) observable and based on an ionospheric climatological model. Near the peak of solar cycle 24, the overall accuracy achieved with tomography was around 3.8 m. notably, compared to the background climatological model, tomography demonstrated improvements ranging from 15 to 20%. The GRAPHIC method outperformed tomography, achieving an accuracy of 0.7 m, whereas we obtained around 7 m accuracy when no ionospheric model is employed. Although the developed ionospheric tomography has yet to match the precision of GRAPHIC, our results bring us relatively closer to this objective.
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页数:14
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