Assessing the Impact of the SCIGN Radome on
Geodetic Parameter Estimates
John J. Braun
UCAR/COSMIC Program
P.O. Box 3000, Boulder, CO
Introduction
The SCIGN radome is widely used within the geodetic community to protect GPS
antennas at permanent sites from snow, debris accumulation, and vandalism. It was
designed to have uniform thickness, minimizing its impact on the electrical phase center
of the associated antenna. Dragert and Schmidt in their paper “The Effect of SCIGN
Domes on the Vertical Phase Centre Position in Routine Processing of GPS Data” found
that the radome altered the vertical coordinate solutions by 1.5 cm when used with a
Dorne-Margolin(DM)/JPL Chokering antenna. This report suggested that this coordinate
change was induced by a misalignment of the radome center of curvature with the mean
L1/L2 electrical phase center. Ken Hudnut (the designer of the radome) confirmed this
misalignment noting that the radome was designed to have a radius of curvature centered
at the physical center of the DM element. There is a 3.5 cm difference between the
physical position of the element and the electrical phase center; the electrical phase center
is higher. Gerry Mader at the National Geodetic Survey (NGS) suggested that the NGS
phase center variations (PCV) for the antenna and radome configuration should properly
model this misaligment, and the radome should have no impact on geodetic parameter
estimates. Dragert argues, that the empirical PCV determination technique used by the
NGS does not estimate tropospheric delay parameters, inducing an error when these
parameters are included in the data analysis. This report summarizes a detailed analysis
of data collected at the Piñon Flat Observatory specifically collected to quantify what
impact the SCIGN radomes have on geodetic parameter estimates.
[See attached .pdf file for more.]
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