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Solid Earth An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 2
Volume 9, issue 2
Solid Earth, 9, 323–339, 2018
https://doi.org/10.5194/se-9-323-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: Dynamics and interaction of processes in the Earth and its...

Solid Earth, 9, 323–339, 2018
https://doi.org/10.5194/se-9-323-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Volume 9, issue 2

Research article 23 Mar 2018

Research article | 23 Mar 2018

Time-variable gravity fields and ocean mass change from 37 months of kinematic Swarm orbits

Christina Lück et al.

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Christina Lück on behalf of the Authors (06 Feb 2018)  Author's response    Manuscript
ED: Publish as is (06 Feb 2018) by Simon McClusky
ED: Publish as is (07 Feb 2018) by J. Huw Davies(Executive Editor)
Publications Copernicus
Special issue
Dynamics and interaction of processes in the Earth and its...
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Short summary
Since 2002, the GRACE mission provides estimates of the Earth's time-variable gravity field, from which one can derive ocean mass variability. Now that the GRACE mission has come to an end, it is especially important to find alternative ways for deriving ocean mass changes. For the first time, we use kinematic orbits of Swarm for computing ocean mass time series. We compute monthly solutions, but also show an alternative way of directly estimating time-variable spherical harmonic coefficients.
Since 2002, the GRACE mission provides estimates of the Earth's time-variable gravity field,...
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Solid Earth

An interactive open-access journal of the European Geosciences Union

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