Abstract
Successful implementation of integer ambiguity resolution enabled precise point positioning (aka PPP-RTK) algorithms is inextricably linked to the ability of a user to perform near real-time positioning by quickly and reliably resolving the integer carrier-phase ambiguities. In the PPP-RTK technique, a major barrier to successful ambiguity resolution is the unmodelled impact of the ionosphere. We present a 4D ionospheric tomographic model that computes in real time the ionospheric electron density as a linear combination of basis functions, namely B-splines. The results show that when the ionospheric estimates are provided as atmospheric corrections for a PPP-RTK end-user, the time to fix its horizontal position below 10 cm is around 20 epochs (the sample rate is 30 s) at the \(90\%\) of the cumulative distribution function (CDF), as opposed to the time it takes when no external corrections are provided, which is around 80 epochs at \(90\%\) of the CDF.
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Notes
\(1~\hbox {TECU} = 10^{16}\, e^-/m^2\); \(e^-= 1\) electron.
By real time we mean updating the estimates as the observations and corrections are provided, typically less than 1 min.
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This work has been supported by the Cooperative Research Centre for Spatial Information, whose activities are funded by the Business Cooperative Research Centres Programme.
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Appendix
Appendix
Equation (9) can be rearranged into one single equation as follows:
The optimal solution (in a LLS sense) for Eq. (16) corresponds to the argument \(\mathbf{x}_k\) that minimizes the error, i.e.
whose solution is as follows
where \(\mathbf{z}_k\,\equiv [\mathbf{y}_k^\mathrm{T}, \,\, \mathbf{f}^\mathrm{T}\left( {\hat{\mathbf{x}}}_{k-1}\right) ]^\mathrm{T}\); \({{\varvec{{\Omega }}}}_k\) is the matrix that maps the state-space estimates onto the observations and onto the a priori state-space estimates,
which is always full rank due to the presence of the identity matrix.
The covariance of the state-space estimates is
where \(\mathbf{E}_k\) is the covariance of the measurements \(\mathbf{y}_k\), and \(\mathbf{Q}_{\mathbf{f}\left( {\hat{\mathbf{x}}}_{k-1}\right) }\) is the covariance of the stochastic dynamic model \(\mathbf{f}\left( {\hat{\mathbf{x}}}_{k-1}\right) \).
The covariance of the estimates \({\hat{\mathbf{x}}}_k\) is as follows:
which, after developing the right-hand side, yields
The matrix inversion lemma, e.g. Stengel (1994), states that
thence, after replacing Eq. (23) in Eq. (22), it leads to the following expression
where \(\mathbf{K}_k\), the gain matrix, is defined as follows
Finally, by using Eq. (24) in Eq. (18), and noting that
the following expression is obtained:
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Olivares-Pulido, G., Terkildsen, M., Arsov, K. et al. A 4D tomographic ionospheric model to support PPP-RTK. J Geod 93, 1673–1683 (2019). https://doi.org/10.1007/s00190-019-01276-4
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DOI: https://doi.org/10.1007/s00190-019-01276-4