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ESurf | Articles | Volume 6, issue 4
Earth Surf. Dynam., 6, 1203-1218, 2018
https://doi.org/10.5194/esurf-6-1203-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Earth Surf. Dynam., 6, 1203-1218, 2018
https://doi.org/10.5194/esurf-6-1203-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 07 Dec 2018

Research article | 07 Dec 2018

Earth's surface mass transport derived from GRACE, evaluated by GPS, ICESat, hydrological modeling and altimetry satellite orbits

Christian Gruber et al.
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Cited articles  
Bettadpur, S. and CSR Level-2 Team: Insights into the Earth System mass variability from CSR-RL05 GRACE gravity fields, EGU General Assembly, Vienna, Austria, 22–27 April 2012, EGU2012-6409, 2012. 
Cheng, M., Tapley, B. D., and Ries, J. C.: Deceleration in the Earth's oblateness, J. Geophys. Res.-Sol. Ea., 118, 740–747, https://doi.org/10.1002/jgrb.50058, 2013. 
Dahle, Ch., Flechtner, F., Gruber, Ch., König, D., König, R., Michalak, G., and Neumayer, K.-H.: GFZ GRACE Level-2 Processing Standards Document for Level-2 Product Release 0005, Scientific Technical Report STR12/02 – Data, Revised Edition, January 2013, Potsdam, 21 pp., https://doi.org/10.2312/GFZ.b103-1202-25, 2012. 
Dobslaw, H., Flechtner, F., Bergmann-Wolf, I., Dahle, C., Dill, R., Esselborn, S., Sasgen, I., and Thomas, M.: Simulating high-frequency atmosphere-ocean mass variability for de-aliasing of satellite gravity observations: AOD1B RL05, J. Geophys. Res., 118, 3704–3711, 2013. 
Döll, P., Kaspar, F., and Lehner, B.: A global hydrological model for deriving water availability indicators: model tuning and validation, J. Hydrol., 270, 105–134, 2003. 
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By using a set of evaluation methods involving GPS, ICESat, hydrological modelling and altimetry satellite orbits, we show that the novel radial basis function (RBF) processing technique can be used for processing the Gravity Recovery and Climate Experiment (GRACE) data yielding global gravity field models which fit independent reference values at the same level as commonly accepted global geopotential models based on spherical harmonics.
By using a set of evaluation methods involving GPS, ICESat, hydrological modelling and altimetry...
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