Abstract

Tropospheric delay is one of the main sources of measurement error in global navigation satellite systems. It is usually compensated by using an empirical correction model. In this paper, temporal and spatial variations of the global zenith tropospheric delay (ZTD) are further analyzed by ZTD time series from global International GNSS Service stations and annual ZTDs derived from global National Centers for Environmental Prediction reanalysis data, respectively. A new ZTD correction model, named IGGtrop, is developed based on the characteristics of ZTD. Experimental results show that this new 3D-grid-based model that accommodates longitudinal as well as latitudinal variations of ZTD performs better than latitude-only based models (such as UNB3, EGNOS, and UNB3m). The global average bias and RMS for IGGtrop are about −0.8 cm and 4.0 cm, respectively. Bias values for UNB3, EGNOS, and UNB3m are 2.0, 2.0, and 0.7 cm, respectively, and respective RMS values 5.4, 5.4, and 5.0 cm. IGGtrop shows much more consistent prediction errors for different areas than EGNOS and UNB3m. In China, the performance of IGGtrop (bias values from −2.0 to 0.4 cm and RMS from 2.1 to 6.4 cm) is clearly superior to those of EGNOS and UNB3m. It is also demonstrated that IGGtrop biases vary little with height, and its RMS values tend to decrease with increasing height. In addition, IGGtrop generally estimates ZTD with greater accuracy than EGNOS and UNB3m in the Southern Hemisphere.

Highlights

  • Tropospheric delay is one of the main sources of measurement error in global navigation satellite systems

  • Temporal and spatial characteristics of global zenith tropospheric delay (ZTD) were further studied by ZTD observations derived from Global Navigation Satellite System (GNSS) signals and National Centers for Environmental Prediction (NCEP) reanalysis data

  • IGGtrop was validated by comparing zenith delays predicted from model with those derived from 125 global International GNSS Service (IGS) sites

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Summary

ZTD characteristics analysis

Since comprehensive knowledge about the characteristics of ZTD is fundamental to its modeling, the temporal variation of ZTD is analyzed by a set of continuous GNSS measurements, and ZTD obtained from the NCEP reanalysis data is used to investigate its spatial distribution. The ZTD time series are analyzed with the Fast Fourier transform and the corresponding PSD (power spectral density) results are included in the figure This clearly reveals peaks for the annual and semiannual periods. According to the foregoing analysis, the ZTD time series for sites outside the equatorial region are fitted again with a simpler equation (2), which has no semiannual component. Our results indicate that unlike at mid and high latitudes, the semiannual component may be important in the temporal variation of equatorial ZTD, which has not been previously reported by other researchers. To achieve more realistic prediction and correction performance, zonal ZTD variation must be taken into account as much as possible in ZTD modeling

A new global ZTD model—IGGtrop
IGGtrop model validation
Findings
Conclusions
Full Text
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