Status and Prospects for Combined GPS LOD and VLBI UT1 Measurements

Status and Prospects for Combined GPS LOD and VLBI UT1 Measurements A Kalman filter was developed to combine VLBI estimates of UT1-TAI with biased length of day (LOD) estimates from GPS. The VLBI results are the analyses of the NASA Goddard Space Flight Center group from 24-hr multi-station observing sessions several times per week and the nearly daily 1-hr single-baseline sessions. Daily GPS LOD estimates from the International GNSS Service (IGS) are combined with the VLBI UT1-TAI by modeling the natural excitation of LOD as the integral of a white noise process (i.e., as a random walk) and the UT1 variations as the integration of LOD, similar to the method described by Morabito et al. (1988). To account for GPS technique errors, which express themselves mostly as temporally correlated biases in the LOD measurements, a Gauss-Markov model has been added to assimilate the IGS data, together with a fortnightly sinusoidal term to capture errors in the IGS treatments of tidal effects. Evaluated against independent atmospheric and oceanic axial angular momentum (AAM + OAM) excitations and compared to other UT1/LOD combinations, ours performs best overall in terms of lowest RMS residual and highest correlation with (AAM + OAM) over sliding intervals down to 3 d. The IERS 05C04 and Bulletin A combinations show strong high-frequency smoothing and other problems. Until modified, the JPL SPACE series suffered in the high frequencies from not including any GPS-based LODs. We find, surprisingly, that further improvements are possible in the Kalman filter combination by selective rejection of some VLBI data. The best combined results are obtained by excluding all the 1-hr single-baseline UT1 data as well as those 24-hr UT1 measurements with formal errors greater than 5 μs (about 18% of the multi-baseline sessions). A rescaling of the VLBI formal errors, rather than rejection, was not an effective strategy. These results suggest that the UT1 errors of the 1-hr and weaker 24-hr VLBI sessions are non-Gaussian and more heterogeneous than expected, possibly due to the diversity of observing geometries used, other neglected systematic effects, or to the much shorter observational averaging interval of the single-baseline sessions. UT1 prediction services could benefit from better handling of VLBI inputs together with proper assimilation of IGS LOD products, including using the Ultra-rapid series that is updated four times daily with 15 hr delay.

[1]  David D. Morabito,et al.  Kalman Filtering of Earth Orientation Changes , 1988 .

[2]  J. Dickey,et al.  Earth's Variable Rotation , 1991, Science.

[3]  J. G. Williams,et al.  Tidal variations of earth rotation , 1981 .

[4]  Richard S. Gross,et al.  A Kalman-filter-based approach to combining independent Earth-orientation series , 1998 .

[5]  J. Ray,et al.  Measurements of length of day using the Global Positioning System , 1996 .

[6]  Jan Kouba Sub-Daily Earth Rotation Parameters and the International GPS Service Orbit/Clock Solution Products , 2002 .

[7]  Jan Kouba Testing of the IERS2000 Sub-Daily Earth Rotation Parameter Model , 2003 .

[8]  Jan Vondrák,et al.  Combined smoothing method and its use in combining Earth orientation parameters measured by space techniques , 2000 .

[9]  Dimitris Menemenlis,et al.  Atmospheric and oceanic excitation of decadal‐scale Earth orientation variations , 2005 .

[10]  Jan Kouba,et al.  Comparison of length of day with oceanic and atmospheric angular momentum series , 2005 .

[11]  Jim R. Ray,et al.  On the precision and accuracy of IGS orbits , 2009 .

[12]  A Quasi-Optimal, Consistent Approach for Combination of UT1 and LOD , 2009 .

[13]  J. Vondrák A contribution to the problem of smoothing observational data , 1969 .

[14]  Richard S. Gross,et al.  Combinations of Earth Orientation Measurements: SPACE2001, COMB2001, and POLE2001 , 2002 .

[15]  H. Schuh,et al.  Daily Earth rotation determinations from IRIS very long baseline interferometry , 1985, Nature.

[16]  Jim R. Ray,et al.  A Kalman Filter for Improved Multi-Technique Estimates of UT1 Variations , 2008 .

[17]  H. Schuh,et al.  Asymmetric tropospheric delays from numerical weather models for UT1 determination from VLBI Intensive sessions on the baseline Wettzell–Tsukuba , 2010 .

[18]  Z. Altamimi,et al.  ITRF2005 : A new release of the International Terrestrial Reference Frame based on time series of station positions and Earth Orientation Parameters , 2007 .

[19]  J. Vondrák,et al.  COMBINING GPS AND VLBI MEASUREMENTS OF CELESTIAL MOTION OF THE EARTH'S SPIN AXIS AND UNIVERSAL TIME , 2005 .

[20]  Jim R. Ray,et al.  Recent Improvements to IERS Bulletin A Combination and Prediction , 2001, GPS Solutions.

[21]  Zuheir Altamimi,et al.  Is there utility in rigorous combinations of VLBI and GPS Earth orientation parameters? , 2005 .

[22]  Jim R. Ray,et al.  IGS Earth Rotation Parameters , 1999, GPS Solutions.

[23]  Zinovy Malkin On comparison of the Earth orientation parameters obtained from different VLBI networks and observing programs , 2009 .

[24]  J. Scott Stewart,et al.  Long-period lunar fortnightly and monthly ocean tides , 1998 .

[25]  Markus Rothacher,et al.  Combined Earth orientation parameters based on homogeneous and continuous VLBI and GPS data , 2007 .