VMF3/GPT3: refined discrete and empirical troposphere mapping functions

• Published in: Journal of geodesy Vol. 92; no. 4; pp. 349 - 360
• Main Authors: Landskron, Daniel, Böhm, Johannes
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 01.04.2018; Springer Nature B.V
• Subjects: Coefficients; Earth and Environmental Science; Earth Sciences; Empirical models; Geodetics; Geophysics/Geodesy; Global pressure; Global temperatures; Interferometry; Mapping; Modelling; Navigation; Navigation satellites; Navigation systems; Original; Original Article; Radio waves; Satellites; Temperature; Tracers; Troposphere; VLBI; GNSS; Mapping functions; Horizontal gradients; Troposphere
• ISSN: 0949-7714; 1432-1394
• DOI: 10.1007/s00190-017-1066-2

Incorrect modeling of troposphere delays is one of the major error sources for space geodetic techniques such as Global Navigation Satellite Systems (GNSS) or Very Long Baseline Interferometry (VLBI). Over the years, many approaches have been devised which aim at mapping the delay of radio waves from zenith direction down to the observed elevation angle, so-called mapping functions. This paper contains a new approach intended to refine the currently most important discrete mapping function, the Vienna Mapping Functions 1 (VMF1), which is successively referred to as Vienna Mapping Functions 3 (VMF3). It is designed in such a way as to eliminate shortcomings in the empirical coefficients b and c and in the tuning for the specific elevation angle of 3 ∘ . Ray-traced delays of the ray-tracer RADIATE serve as the basis for the calculation of new mapping function coefficients. Comparisons of modeled slant delays demonstrate the ability of VMF3 to approximate the underlying ray-traced delays more accurately than VMF1 does, in particular at low elevation angles. In other words, when requiring highest precision, VMF3 is to be preferable to VMF1. Aside from revising the discrete form of mapping functions, we also present a new empirical model named Global Pressure and Temperature 3 (GPT3) on a 5 ∘ × 5 ∘ as well as a 1 ∘ × 1 ∘ global grid, which is generally based on the same data. Its main components are hydrostatic and wet empirical mapping function coefficients derived from special averaging techniques of the respective (discrete) VMF3 data. In addition, GPT3 also contains a set of meteorological quantities which are adopted as they stand from their predecessor, Global Pressure and Temperature 2 wet. Thus, GPT3 represents a very comprehensive troposphere model which can be used for a series of geodetic as well as meteorological and climatological purposes and is fully consistent with VMF3.