1. What have the authors contributed in "Joint estimation of vertical total electron content (vtec) and satellite differential code biases (sdcbs) using low-cost receivers" ?
In this work, the authors present a 2 / 30 single-frequency ( SF ) approach, enabling the joint estimation of VTEC and SDCBs using low-cost receivers ; this approach is also based on two steps and it differs from the DF approach only in the first step, where they turn to the Precise Point Positioning ( PPP ) technique to retrieve from the single-frequency GNSS data the ionospheric observables, interpreted as the combination of the STEC, the SDCBs and the biased receiver clocks at the pivot epoch.. Their numerical analyses clarify how SF approach performs when being applied to GPS L1 data collected by a single receiver under both calm and disturbed ionospheric conditions.
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2. What is the way to process the L1 data?
When implementing the PPP, a least-square batch adjustment is used to process the GPS L1 data, corrected by IGS Final orbit and clock products, into ionospheric observables along with their covariance matrix.
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3. What is the role of the thin-layer ionosphere model?
The thin-layer ionosphere model fulfills the role of isolating the interested parameters (the VTEC and the SDCBs), along with the nuisance ones (the RDCBs), from the ionospheric observables.
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4. How does the thin-layer model exploit the first fact?
The thin-layer model exploits the first fact by approximating the whole ionosphere with a spherical shell located at a pre-specified height, say, 450 kilometers, above the Earth’s surface.
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