Evaluation of ocean mass variability derived from different GRACE solutions
The Gravity Recovery and Climate Experiment (GRACE) provides estimates of the earths static and time-variant gravity field. Solutions from various processing centres (GFZ, CSR, GRGS, JPL etc.) enable us to determine water mass redistributions on the globe. Given that land signals are generally large...
Main Authors: | , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2008
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/19522/ https://hdl.handle.net/10013/epic.31320 |