TY - JOUR
T1 - Low-degree gravity change from GPS data of COSMIC and GRACE satellite missions
AU - Lin, Tingjung
AU - Hwang, Cheinway
AU - Tseng, Tzu Pang
AU - Chao, B. F.
N1 - Funding Information:
This research is supported by the National Space Organization of Taiwan , under grant No. NSPO-S-099010(P) . We thank the reviewer for his constructive reviews to improve the paper.
PY - 2012/1
Y1 - 2012/1
N2 - This paper demonstrates estimation of time-varying gravity harmonic coefficients from GPS data of COSMIC and GRACE satellite missions. The kinematic orbits of COSMIC and GRACE are determined to the cm-level accuracy. The NASA Goddard's GEODYN II software is used to model the orbit dynamics of COSMIC and GRACE, including the effect of a static gravity field. The surface forces are estimated per one orbital period. Residual orbits generated from kinematic and reference orbits serve as observables to determine the harmonic coefficients in the weighted-constraint least-squares. The monthly COSMIC and GRACE GPS data from September 2006 to December 2007 (16 months) are processed to estimate harmonic coefficients to degree 5. The geoid variations from the GPS and CSR RL04 (GRACE) solutions show consistent patterns over space and time, especially in regions of active hydrological changes. The monthly GPS-derived second zonal coefficient closely resembles the SLR-derived and CSR RL04 values, and third and fourth zonal coefficients resemble the CSR RL04 values.
AB - This paper demonstrates estimation of time-varying gravity harmonic coefficients from GPS data of COSMIC and GRACE satellite missions. The kinematic orbits of COSMIC and GRACE are determined to the cm-level accuracy. The NASA Goddard's GEODYN II software is used to model the orbit dynamics of COSMIC and GRACE, including the effect of a static gravity field. The surface forces are estimated per one orbital period. Residual orbits generated from kinematic and reference orbits serve as observables to determine the harmonic coefficients in the weighted-constraint least-squares. The monthly COSMIC and GRACE GPS data from September 2006 to December 2007 (16 months) are processed to estimate harmonic coefficients to degree 5. The geoid variations from the GPS and CSR RL04 (GRACE) solutions show consistent patterns over space and time, especially in regions of active hydrological changes. The monthly GPS-derived second zonal coefficient closely resembles the SLR-derived and CSR RL04 values, and third and fourth zonal coefficients resemble the CSR RL04 values.
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U2 - 10.1016/j.jog.2011.08.004
DO - 10.1016/j.jog.2011.08.004
M3 - Article
AN - SCOPUS:80052530025
SN - 0264-3707
VL - 53
SP - 34
EP - 42
JO - Journal of Geodynamics
JF - Journal of Geodynamics
IS - 1
ER -