Abstract
Up to now, state-of-the-art empirical slant delay modeling for processing observations from radio space geodetic techniques has been provided by a combination of two empirical models. These are GPT (Global Pressure and Temperature) and GMF (Global Mapping Function), both operating on the basis of long-term averages of surface values from numerical weather models. Weaknesses in GPT/GMF, specifically their limited spatial and temporal variability, are largely eradicated by a new, combined model GPT2, which provides pressure, temperature, lapse rate, water vapor pressure, and mapping function coefficients at any site, resting upon a global 5° grid of mean values, annual, and semi-annual variations in all parameters. Built on ERA-Interim data, GPT2 brings forth improved empirical slant delays for geophysical studies. Compared to GPT/GMF, GPT2 yields a 40% reduction of annual and semi-annual amplitude differences in station heights with respect to a solution based on instantaneous local pressure values and the Vienna mapping functions 1, as shown with a series of global VLBI (Very Long Baseline Interferometry) solutions. Key Points Refined tropospheric delay model based on ERA-Interim Excellent match of empirical model pressure to in-situ pressure values Improved station height estimates deduced from VLBI observations. ©2013 American Geophysical Union. All Rights Reserved.
Author supplied keywords
Cite
CITATION STYLE
Lagler, K., Schindelegger, M., Böhm, J., Krásná, H., & Nilsson, T. (2013). GPT2: Empirical slant delay model for radio space geodetic techniques. Geophysical Research Letters, 40(6), 1069–1073. https://doi.org/10.1002/grl.50288
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.