2015
DOI: 10.1186/s40623-015-0293-0
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Tropospheric delay determination by Kalman filtering VLBI data

Abstract: The troposphere is one of the most important error sources for space geodetic techniques relying on radio signals. Since it is not possible to model the wet part of the tropospheric delay with sufficient accuracy, it needs to be estimated from the observational data. In the analysis of very long baseline interferometry (VLBI) data, the parameter estimation is routinely performed using a least squares adjustment. In this paper, we investigate the application of a Kalman filter for parameter estimation, specific… Show more

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Cited by 24 publications
(10 citation statements)
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“…A Kalman filter approach has been successfully used by the ITRS combination center at NASA Jet Propulsion Laboratory (JPL) for their JTRF2008 solution, providing station coordinates at weekly intervals together with secular velocities and seasonal signals . For the analysis of very long baseline interferometry (VLBI, Schuh and Behrend, 2012;Schuh and Böhm, 2013) observations, Kalman filtering was introduced by Herring et al (1990), and recently applied in studies by Nilsson et al (2015), Soja et al (2015), and Karbon et al (2015).…”
Section: Introductionmentioning
confidence: 99%
“…A Kalman filter approach has been successfully used by the ITRS combination center at NASA Jet Propulsion Laboratory (JPL) for their JTRF2008 solution, providing station coordinates at weekly intervals together with secular velocities and seasonal signals . For the analysis of very long baseline interferometry (VLBI, Schuh and Behrend, 2012;Schuh and Böhm, 2013) observations, Kalman filtering was introduced by Herring et al (1990), and recently applied in studies by Nilsson et al (2015), Soja et al (2015), and Karbon et al (2015).…”
Section: Introductionmentioning
confidence: 99%
“…Therefore, today the wet delays at all stations in an experiment are normally estimated from the VLBI data themselves, see e.g. Soja et al (2015). Stand-alone WVR observations at specific sites are mainly used to verify these estimates, see e.g.…”
Section: Introductionmentioning
confidence: 99%
“…The ZWD are modeled as random walk processes, and in this work, we assumed a PSD of 58 cm 2 /day for the process noise, as suggested (Herring et al 1990). For a description of how to estimate the PSD for the different parameters and the effect of using these values, see Soja et al (2015). The tropospheric gradients are modeled as first-order Gauss-Markov processes, and we assumed a time constant of 3 h and a process noise PSD of 0.025 cm 2 /day in the present study.…”
Section: Implementation In Vievs@gfzmentioning
confidence: 99%
“…For a more detailed study of the ZWD from the Kalman filter, see Soja et al (2015). A comparison of gradients from different techniques, including the Kalman filter and LSM VLBI solutions, is described by (Heinkelmann et al: Atmospheric delay gradients with high temporal resolution, submitted to J. Geodesy).…”
Section: Tropospheric Delaysmentioning
confidence: 99%
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