Reference : Multi-GNSS Slant Wet Delay Retrieval Using Multipath Mitigation Maps
Scientific congresses, symposiums and conference proceedings : Unpublished conference
Physical, chemical, mathematical & earth Sciences : Earth sciences & physical geography
Physics and Materials Science
http://hdl.handle.net/10993/50647
Multi-GNSS Slant Wet Delay Retrieval Using Multipath Mitigation Maps
English
Hunegnaw, Addisu mailto [University of Luxembourg > Faculty of Science, Technology and Medicine (FSTM) > Department of Engineering (DoE) >]
Ejigu, Yohannes Getachew []
Teferle, Felix Norman mailto [University of Luxembourg > Faculty of Science, Technology and Medicine (FSTM) > Department of Engineering (DoE) >]
Elgered, Gunnar []
24-Apr-2021
EGU21-16243
https://doi.org/10.5194/egusphere-egu21-16243
EGU General Assembly 2021
No
EGU General Assembly Conference
09-04-2021 to 30-04-2021
online
Austria
[en] Multipath ; GNSS ; Slant total delay
[en] The conventional Global Navigation Satellite System (GNSS) processing is typically contaminated with errors due to atmospheric variabilities, such as those associated with the mesoscale phenomena. These errors are manifested in the parameter estimates, including station coordinates and atmospheric products. To enhance the accuracy of these GNSS products further, a better understanding of the local-scale atmospheric variability is necessary. As part of multi-GNSS processing, station coordinates, carrier phase ambiguities, orbits, zenith total delay (ZTD) and horizontal gradients are the main parameters of interest. Here, ZTD is estimated as the average zenith delay along the line-of-sight to every observed GNSS satellite mapped to the vertical while the horizontal gradients are estimated in NS and EW directions and provide a means to partly account for the azimuthally inhomogeneous atmosphere. However, a better atmospheric description is possible by evaluating the slant path delay (SPD) or slant wet delay (SWD) along GNSS ray paths, which are not resolved by ordinary ZTD and gradient analysis. SWD is expected to provide better information about the inhomogeneous distribution of water vapour that is disregarded when retrieving ZTD and horizontal gradients. Usually, SWD cannot be estimated directly from GNSS processing as the number of unknown parameters exceeds the number of observations. Thus, SWD is generally calculated from ZTD for each satellite and may be dominated by un-modelled atmospheric delays, clock errors, unresolved carrier-phase ambiguities and near-surface multipath scattering. In this work, we have computed multipath maps by stacking individual post-fit carrier residuals incorporating the signals from four GNSS constellations, i.e. BeiDou, Galileo, Glonass and GPS. We have selected a subset of global International GNSS Service (IGS) stations capable of multi-GNSS observables located in different climatic zones. The multipath effects are reduced by subtracting the stacked multipath maps from the raw post-fit carrier phase residuals. We demonstrate that the multipath stacking technique results in significantly reduced variations in the one-way post-fit carrier phase residuals. This is particularly evident for lower elevation angles, thus, producing a retrieval method for SWD that is less affected by site-specific multipath effects. We show a positive impact on SWD estimation using our multipath maps during increased atmospheric inhomogeneity as induced by severe weather events.
University of Luxembourg: The Faculty of Science, Technology and Medicine (FSTM)
Fonds National de la Recherche - FnR
VAPOUR
Researchers ; Professionals
http://hdl.handle.net/10993/50647
https://meetingorganizer.copernicus.org/EGU21/EGU21-16243.html
FnR ; FNR12909050 > Norman Teferle > VAPOUR > Advanced Asymmetry Tropospheric Products For Meteorology From Gnss And Sar Observations > 01/02/2019 > 31/01/2022 > 2018

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