Back to Search Start Over

JTRF2014, the JPL Kalman filter and smoother realization of the International Terrestrial Reference System.

Authors :
Abbondanza, Claudio
Chin, Toshio M.
Gross, Richard S.
Heflin, Michael B.
Parker, Jay W.
Soja, Benedikt S.
van Dam, Tonie
Wu, Xiaoping
Source :
Journal of Geophysical Research. Solid Earth; Oct2017, Vol. 122 Issue 10, p8474-8510, 37p
Publication Year :
2017

Abstract

We present and discuss JTRF2014, the Terrestrial Reference Frame (TRF) the Jet Propulsion Laboratory constructed by combining space-geodetic inputs from very long baseline interferometry (VLBI), satellite laser ranging (SLR), Global Navigation Satellite Systems (GNSS), and Doppler orbitography and radiopositioning integrated by satellite submitted for the realization of ITRF2014. Determined through a Kalman filter and Rauch-Tung-Striebel smoother assimilating position observations, Earth orientation parameters, and local ties, JTRF2014 is a subsecular, time series-based TRF whose origin is at the quasi-instantaneous center of mass (CM) as sensed by SLR and whose scale is determined by the quasi-instantaneous VLBI and SLR scales. The dynamical evolution of the positions accounts for a secular motion term, annual, and semiannual periodic modes. Site-dependent variances based on the analysis of loading displacements induced by mass redistributions of terrestrial fluids have been used to control the extent of random walk adopted in the combination. With differences in the amplitude of the annual signal within the range 0.5-0.8 mm, JTRF2014-derived center of network-to-center of mass (CM-CN) is in remarkable agreement with the geocenter motion obtained via spectral inversion of GNSS, Gravity Recovery and Climate Experiment (GRACE) observations and modeled ocean bottom pressure from Estimating the Circulation and Climate of the Ocean (ECCO). Comparisons of JTRF2014 to ITRF2014 suggest high-level consistency with time derivatives of the Helmert transformation parameters connecting the two frames below 0.18 mm/yr and weighted root-mean-square differences of the polar motion (polar motion rate) in the order of 30 μas (17 μas/d). [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
21699313
Volume :
122
Issue :
10
Database :
Complementary Index
Journal :
Journal of Geophysical Research. Solid Earth
Publication Type :
Academic Journal
Accession number :
126419420
Full Text :
https://doi.org/10.1002/2017JB014360