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The Barcelona ionospheric mapping function (BIMF) and its application to northern mid-latitudes

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A Correction to this article was published on 20 July 2020

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Abstract

A simple way of improving the Global Navigation Satellite Systems (GNSS) slant ionospheric correction from Vertical Total Electron Content (VTEC) models is presented. In many GNSS applications, a mapping function is required to convert from VTEC, which may be provided in Global Ionospheric Maps (GIMs), to Slant TEC (STEC). Typical approaches assume a single ionospheric shell with constant height, which is unrealistic, especially for low-elevation signals. To reduce the associated conversion error, we propose the Barcelona Ionospheric Mapping Function and its first implementation at northern mid-latitudes (BIMF-nml). BIMF is based on a climatic prediction of the distribution of the topside vertical electron content fraction of VTEC (hereinafter µ2). BIMF is convenient to be applied since no external data are required in practice. To evaluate its performance, we use as independent reference the STEC difference (so-called dSTEC) values directly measured from mid-latitude dual-frequency Global Positioning System (GPS) receivers that have not been used in the computation of the VTEC GIMs under assessment. It is shown that the use of BIMF improves the GIM STEC estimation compared to the single-layer assumptions. This is the case for the mapping functions used by the International GNSS Service (IGS) and Satellite-Based Augmentation Systems (SBAS). This improvement is valid not only for the UPC GIMs, up to 15% for the year 2014, but especially for the GIMs of other analysis centers, such as those produced by CODE and JPL, up to 32 and 29%, respectively.

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  • 20 July 2020

    In the original article, some typos regarding Eq. (3) and Table��9 are introduced.

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Acknowledgements

This research has been generated within the context of the AUDITOR project (Advanced Multi­Constellation EGNSS Augmentation and Monitoring Network and its Application in Precision Agriculture), funded by the European Union’s H2020 Programme, under grant agreement number 687367. The first author is grateful to the financial support of the China Scholarship Council. The authors are also grateful to the International GNSS Service. The open-data open-product scientific organizations always provide a professional and friendly framework for collaboration. The authors would like to thank anonymous reviewers for their valuable comments and suggestions that improved the quality of the paper. The second author is indebted to Dr. Raül Orús-Pérez for his suggestions for improving the previous version of the manuscript.

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Correspondence to Manuel Hernández-Pajares.

Appendices

Appendix A

See Tables 3, 4, 5, 6 and 7.

Table 3 Coefficients of a0
Table 4 Coefficients of a1
Table 5 Coefficients of a2
Table 6 Coefficients of a3
Table 7 Coefficients of a4

Appendix B

See Tables 8 and 9.

Table 8 Statistical results for different stations using CODG in 2014
Table 9 Statistical results for different stations using JPLG in 2014

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Lyu, H., Hernández-Pajares, M., Nohutcu, M. et al. The Barcelona ionospheric mapping function (BIMF) and its application to northern mid-latitudes. GPS Solut 22, 67 (2018). https://doi.org/10.1007/s10291-018-0731-0

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