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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 36, issue 6 | Copyright
Ann. Geophys., 36, 1507-1519, 2018
https://doi.org/10.5194/angeo-36-1507-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Regular paper 06 Nov 2018

Regular paper | 06 Nov 2018

An empirical zenith wet delay correction model using piecewise height functions

YiBin Yao1,2,3 and YuFeng Hu1,4 YiBin Yao and YuFeng Hu
  • 1School of Geodesy and Geomatics, Wuhan University, 129 Luoyu Road, Wuhan 430079, China
  • 2Key Laboratory of Geospace Environment and Geodesy, Ministry of Education, Wuhan University, 129 Luoyu Road, Wuhan 430079, China
  • 3Collaborative Innovation Center for Geospatial Technology, 129 Luoyu Road, Wuhan 430079, China
  • 4College of Geology Engineering and Geomatics, Chang'an University, Xi'an 710054, Shanxi, China

Abstract. Tropospheric delay is an important error source in space geodetic techniques. The temporal and spatial variations of the zenith wet delay (ZWD) are very large and thus limit the accuracy of tropospheric delay modelling. Thus, it is worthwhile undertaking research aimed at constructing a precise ZWD model. Based on the analysis of vertical variations of ZWD, we divided the troposphere into three height intervals (below 2km, 2 to 5km, and 5 to 10km) and determined the fitting functions for the ZWD within these height intervals. The global empirical ZWD model HZWD, which considers the periodic variations of ZWD with a spatial resolution of 5° × 5°, is established using the ECMWF ZWD profiles from 2001 to 2010. Validated by the ECMWF ZWD data in 2015, the precision of the ZWD estimation in the HZWD model over the three height intervals are improved by 1.4, 0.9, and 1.2mm, respectively, compared to that of the currently best GPT2w model (23.8, 13.1, and 2.6mm). The test results from ZWD data from 318 radiosonde stations show that the root mean square error (RMSE) in the HZWD model over the three height intervals was reduced by 2% (0.6mm), 5% (0.9mm), and 33% (1.7mm), respectively, compared to the GPT2w model (30.1, 15.8, and 3.5mm) over the three height intervals. In addition, the spatial and temporal stabilities of the HZWD model are higher than those of GPT2w and UNB3m.

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