Abstract
We carry out a comprehensive analysis and assessment of degree-2 gravitational changes ΔC21, and ΔS21, estimated using the Gravity Recovery and Climate Experiment (GRACE) and GRACE Follow-On (GFO), satellite laser ranging (SLR), Earth Orientation Parameters (EOP), and geophysical models over the period April 2002–February 2020. The four independent estimates of ΔC21 and ΔS21 variations agree well over a broad band of frequencies. The GRACE/GFO Release 6 (RL06) solutions show major improvements over the previous RL05 solutions at both seasonal and intra-seasonal time scales, when compared with EOP and SLR estimates. Among the four independent estimates, highest correlation coefficients and smallest RMS residuals are found between GRACE/GFO and EOP estimates of ΔC21 and ΔS21 variations. GRACE/GFO and EOP ΔC21 and ΔS21 estimates exhibit slightly different trends, which are related to the implementation and interpretation of the pole tide correction in GRACE/GFO data processing. This study provides an important early validation of GFO ΔC21 and ΔS21 solutions, especially the new pole tide correction applied in GRACE/GFO RL06 solutions using independent estimates.
Original language | English |
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Article number | 38 |
Journal | Journal of Geodesy |
Volume | 95 |
Issue number | 4 |
DOIs | |
Publication status | Published - Apr 2021 |
Externally published | Yes |
Keywords
- Earth rotation
- EOP
- Geophysical models
- GRACE
- GRACE Follow-on
- Gravity
- SLR
ASJC Scopus subject areas
- Geophysics
- Geochemistry and Petrology
- Computers in Earth Sciences