2019
DOI: 10.1049/iet-rsn.2018.5504
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Least‐squares collocation modelling of regional ionospheric TEC for accelerating real‐time single‐frequency PPP convergence

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Cited by 7 publications
(3 citation statements)
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References 35 publications
(46 reference statements)
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“…For single-frequency GNSS observations, the ionospheric delay error is a key factor to determine the positioning performance. In the MSDQ-PPP, the slant ionospheric delay is estimated as an unknown parameter, and simultaneously the GIM product is introduced as a virtual observation, which is assigned with a proper weight to strengthen the observation model (Gong et al., 2019; Wang et al., 2020). Since the satellite hardware delay biases cannot be eliminated, the satellite differential code bias (DCB) products provided by the Chinese Academy of Sciences (CAS) are used to correct the hardware delay biases (Guo et al., 2015).…”
Section: Methodology and Processing Strategymentioning
confidence: 99%
“…For single-frequency GNSS observations, the ionospheric delay error is a key factor to determine the positioning performance. In the MSDQ-PPP, the slant ionospheric delay is estimated as an unknown parameter, and simultaneously the GIM product is introduced as a virtual observation, which is assigned with a proper weight to strengthen the observation model (Gong et al., 2019; Wang et al., 2020). Since the satellite hardware delay biases cannot be eliminated, the satellite differential code bias (DCB) products provided by the Chinese Academy of Sciences (CAS) are used to correct the hardware delay biases (Guo et al., 2015).…”
Section: Methodology and Processing Strategymentioning
confidence: 99%
“…The commonly used fitting function models include the spherical harmonic function model [15], the trigonometric series model [16], and the polynomial fitting model (PFM). Among them, the PFM is more widely used due to its easy implementation [17]. It models the STEC on a single layer as a function of the longitude and latitude differences of the reference stations and the center point of the modeled area.…”
Section: Introductionmentioning
confidence: 99%
“…In the tsunami detection, the gravity waves generated by the tsunami can engender the ionospheric disturbances in the E and F regions. Meanwhile, ionospheric disturbances can be studied using the real‐time total electron content measurement which is estimated by the geometry‐free combination TDCP method [14, 15]. In the airborne gravimetry, the Kin‐VADASE method [16] is modified to measure the velocity of the aircraft.…”
Section: Introductionmentioning
confidence: 99%