Time-variable gravity fields and ocean mass change from 37 months of kinematic Swarm orbits
Measuring the spatiotemporal variation of ocean mass allows for partitioning of volumetric sea level change, sampled by radar altimeters, into mass-driven and steric parts. The latter is related to ocean heat change and the current Earth's energy imbalance. Since 2002, the Gravity Recovery a...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2018-03-01
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| Series: | Solid Earth |
| Online Access: | https://www.solid-earth.net/9/323/2018/se-9-323-2018.pdf |