Global Eustatic Sea-Level Variations for the Approximation of Geocenter Motion from Grace
Global degree-1 coefficients are derived by means of the method by Swenson et al. (2008) from a model of ocean mass variability and RL05 GRACE monthly mean gravity fields. Since an ocean model consistent with the GRACE GSM fields is required to solely include eustatic sea-level variability which can...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
De Gruyter
2014-04-01
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| Series: | Journal of Geodetic Science |
| Online Access: | http://www.degruyter.com/view/j/jogs.2014.4.issue-1/jogs-2014-0006/jogs-2014-0006.xml?format=INT |