Low degree gravitational changes from GRACE: Validation and interpretation

Author
Keywords
Abstract
We examine low degree gravitational variations ΔC21, ΔS21, and ΔC20 observed by the Gravity Recovery and Climate Experiment (GRACE) satellites during the first 2 years of this gravity mission. The GRACE observations are compared with independent estimates from accurately measured Earth rotational changes and predictions from atmospheric, oceanic, and hydrological models. The 18 GRACE monthly gravity solutions, covering the period April 2002 to March 2004, show strong seasonal variability in the ΔC21, ΔS21, and ΔC20 time series, and generally agree with Earth rotation-derived changes and geophysical model estimates, in particular for ΔS21 and ΔC20. The reason for the poorer agreement between the GRACE results and the Earth rotation-derived estimates for ΔC21 is unclear. We demonstrate that the omission of the ocean pole tide in the GRACE data processing does have significant effects on the estimated ΔC21 and ΔS21.
Year of Publication
2004
Journal
Geophysical Research Letters
Volume
31
Number of Pages
22607
Date Published
11/2004
URL
http://adsabs.harvard.edu/abs/2004GeoRL..3122607C
DOI
10.1029/2004GL021670