Abstract

Abstract. An extensive validation of line-of-sight tropospheric slant total delays (STD) from Global Navigation Satellite Systems (GNSS), ray tracing in numerical weather prediction model (NWM) fields and microwave water vapour radiometer (WVR) is presented. Ten GNSS reference stations, including collocated sites, and almost 2 months of data from 2013, including severe weather events were used for comparison. Seven institutions delivered their STDs based on GNSS observations processed using 5 software programs and 11 strategies enabling to compare rather different solutions and to assess the impact of several aspects of the processing strategy. STDs from NWM ray tracing came from three institutions using three different NWMs and ray-tracing software. Inter-techniques evaluations demonstrated a good mutual agreement of various GNSS STD solutions compared to NWM and WVR STDs. The mean bias among GNSS solutions not considering post-fit residuals in STDs was −0.6 mm for STDs scaled in the zenith direction and the mean standard deviation was 3.7 mm. Standard deviations of comparisons between GNSS and NWM ray-tracing solutions were typically 10 mm ± 2 mm (scaled in the zenith direction), depending on the NWM model and the GNSS station. Comparing GNSS versus WVR STDs reached standard deviations of 12 mm ± 2 mm also scaled in the zenith direction. Impacts of raw GNSS post-fit residuals and cleaned residuals on optimal reconstructing of GNSS STDs were evaluated at inter-technique comparison and for GNSS at collocated sites. The use of raw post-fit residuals is not generally recommended as they might contain strong systematic effects, as demonstrated in the case of station LDB0. Simplified STDs reconstructed only from estimated GNSS tropospheric parameters, i.e. without applying post-fit residuals, performed the best in all the comparisons; however, it obviously missed part of tropospheric signals due to non-linear temporal and spatial variations in the troposphere. Although the post-fit residuals cleaned of visible systematic errors generally showed a slightly worse performance, they contained significant tropospheric signal on top of the simplified model. They are thus recommended for the reconstruction of STDs, particularly during high variability in the troposphere. Cleaned residuals also showed a stable performance during ordinary days while containing promising information about the troposphere at low-elevation angles.

Highlights

  • Tropospheric slant total delay (STD) represents the total delay that undergoes the Global Navigation Satellite Systems (GNSS) radio signal due to the neutral atmosphere along the path from a satellite to a ground receiver antenna

  • Statistical parameters became more stable above 25◦, with occasional disturbances similar to those observed in other numerical weather prediction model (NWM)-based solutions

  • We presented results of validating tropospheric slant total delays obtained from GNSS data processing with those obtained from NWM ray tracing, water vapour radiometer (WVR) measurements and collocated GNSS stations, in search of the optimal method for estimating GNSS STDs

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Summary

Introduction

Tropospheric slant total delay (STD) represents the total delay that undergoes the GNSS radio signal due to the neutral atmosphere along the path from a satellite to a ground receiver antenna. This total delay can be separated into the hydrostatic part, caused by the dry atmospheric constituents, and the wet part caused by water vapour. Slant tropospheric delays (STDs) can provide additional details about the horizontal asymmetry in the troposphere, in the directions from a receiver to all observed GNSS satellites. The quality of the tomography depends on both the accuracy of the STDs (Bender et al, 2009) and the observation geometry (Bender et al, 2011)

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