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Investigating temporal and spatial patterns in the stochastic component of ZTD time series over Europe

Authors

Klos,  Anna
External Organizations;

Bogusz,  Janusz
External Organizations;

Pacione,  Rosa
External Organizations;

Humphrey,  Vincent
External Organizations;

/persons/resource/dobslaw

Dobslaw,  H.
1.3 Earth System Modelling, 1.0 Geodesy, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

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5014167.pdf
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Citation

Klos, A., Bogusz, J., Pacione, R., Humphrey, V., Dobslaw, H. (2023): Investigating temporal and spatial patterns in the stochastic component of ZTD time series over Europe. - GPS Solutions, 27, 19.
https://doi.org/10.1007/s10291-022-01351-y


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5014167
Abstract
The EUREF Permanent GNSS Network (EPN) provides a unique atmospheric dataset over Europe in the form of Zenith Total Delay (ZTD) time series. These ZTD time series are estimated independently by different analysis centers, but a combined solution is also provided. Previous studies showed that changes in the processing strategy do not affect trends and seasonal amplitudes. However, its effect on the temporal and spatial variations of the stochastic component of ZTD time series has not yet been investigated. This study analyses the temporal and spatial correlations of the ZTD residuals obtained from four different datasets: one solution provided by ASI (Agenzia Spaziale Italiana Centro di Geodesia Spaziale, Italy), two solutions provided by GOP (Geodetic Observatory Pecny, Czech Republic), and one combined solution resulting from the EPN’s second reprocessing campaign. We find that the ZTD residuals obtained from the three individual solutions can be modeled using a first-order autoregressive stochastic process, which is less significant and must be completed by an additional white noise process in the combined solution. Although the combination procedure changes the temporal correlation in the ZTD residuals, it neither affects its spatial correlation structure nor its time-variability, for which an annual modulation is observed for stations up to 1,000 km apart. The main spatial patterns in the ZTD residuals also remain identical. Finally, we compare two GOP solutions, one of which only differs in the modeling of non-tidal atmospheric loading at the observation level, and conclude that its modeling has a negligible effect on ZTD values.