Reference : Effect of unmodelled tidal displacements in GPS and GLONASS coordinate time series |
Scientific journals : Article | |||
Physical, chemical, mathematical & earth Sciences : Earth sciences & physical geography | |||
http://hdl.handle.net/10993/35060 | |||
Effect of unmodelled tidal displacements in GPS and GLONASS coordinate time series | |
English | |
Abraha, Kibrom Ebuy ![]() | |
Teferle, Felix Norman ![]() | |
Hunegnaw, Addisu [University of Luxembourg > Faculty of Science, Technology and Communication (FSTC) > Engineering Research Unit >] | |
Dach, Rolf [Astronomical Institute, University of Bern] | |
23-Jun-2018 | |
Geophysical Journal International | |
Blackwell Publishing | |
214 | |
3 | |
2195-2206 | |
Yes | |
International | |
0956-540X | |
[en] Time-series Analysis ; satellite geodesy ; space-geodetic surveys ; Global Navigation Satellite System ; Galileo | |
[en] This study demonstrates the different effects of unmodelled (sub-)daily tidal displacement in
Global Positioning System (GPS) and GLObalnaya NAvigatsionnaya Sputnikovaya Sistema (GLONASS) coordinate time-series. The results show that more than two propagated periodic signals appear in GPS and GLONASS Precise Point Positioning (PPP) coordinate time-series in the presence of an unmodelled M2 /O1 tidal displacements as a result of a non-overlapping 24-hr data sampling. To summarize the propagated periodic signals at the fortnightly period, an unmodelled M2 tidal displacement propagates predominately into two long-period signals at 13.6x (x is a positive integer) and 14.76 d for GPS, while only one significant propagated periodic signal at 14.76 d is discernible for GLONASS. Similarly, significant propagated periodic signals at 13.6x and 14.19 d for GPS and only at 14.19 d for GLONASS are evident as a result of an unmodelled O1 tidal displacement. However, an unmodelled M f (long- period) signal results in a strong power of similar magnitude at 13.6x d (∼13.66 d) for both GPS and GLONASS solutions. The appearance of different periodic signals as a result of the same unmodelled tidal displacement is attributed to the different ground repeat periods of the constellations. The latter is likely to explain the reason why the 13.6x-d fortnightly signal is present only in GPS solutions. Comparing the powers of the M2 propagated periodic signals at 13.6x and 14.76 d on average from 32 globally distributed stations, the amplitude of the former is larger than for the latter by an order of magnitude. The results of this study demonstrate that the 13.6x-d periodic signal in GPS/GNSS (Global Navigation Satellite System) derived products is a joint contribution of the propagation of unmodelled (sub-)daily tidal displacements and errors at longer periods with the former appearing to contribute more. Significant reduction of the propagated periodic signals is achieved from combined-system solutions where including Galileo (the European GNSS) to the combined solution already shows benefits by reducing the effect even before the system has reached its full constellation. Combined GNSS solutions will benefit the applications of GNSS time-series for retrieving tidal harmonic signals such as Mf as they reduce constellation specific propagation effects. | |
University of Luxembourg: High Performance Computing - ULHPC | |
Fonds National de la Recherche - FnR (6835562) ; University of Luxembourg - UL; SGSL IRP | |
MGLTM | |
Researchers ; Professionals ; Students | |
http://hdl.handle.net/10993/35060 | |
10.1093/gji/ggy254 | |
https://doi.org/10.1093/gji/ggy254 | |
The original publication is available at https://academic.oup.com/gji/article-abstract/214/3/2195/5043226 | |
FnR ; FNR6835562 > Kibrom Ebuy Abraha > MGLTM > Multi-GNSS Benefits to Long-Term Monitoring Applications in the Geosciences > 01/05/2014 > 30/04/2018 > 2013 |
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