Articles | Volume 18, issue 5
https://doi.org/10.5194/essd-18-3481-2026
https://doi.org/10.5194/essd-18-3481-2026
Data description article
 | 
22 May 2026
Data description article |  | 22 May 2026

GRACE and GRACE-FO mascons for ocean dynamic applications

Jennifer Bonin, Nadège Pie, Mark E. Tamisiea, Don Chambers, and Himanshu Save

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Cited articles

Bergmann, I. and Dobslaw, H.: Short-term transport variability of the Antarctic Circumpolar Current from satellite gravity observations, J. Geophys. Res.-Oceans, 117, https://doi.org/10.1029/2012JC007872, 2012. 
Bingham, R. J. and Hughes, C. W.: Observing seasonal bottom pressure variability in the North Pacific with GRACE, Geophys. Res. Lett., 33, https://doi.org/10.1029/2005GL025489, 2006. 
Boening, C., Willis, J. K., Landerer, F. W., Nerem, R. S., and Fasullo, J.: The 2011 la Nia: So strong, the oceans fell, Geophys. Res. Lett., 39, https://doi.org/10.1029/2012GL053055, 2012. 
Bonin, J. A., Pie, N., Chambers, D., Tamisiea, M. E., and Save, H.: Detection and modeling of the effect of large earthquakes in GRACE/GRACE-FO mascons, Earth Space Sci., 13, https://doi.org/10.1029/2025EA004219, 2026. 
Cambiotti, G. and Sabadini, R.: A source model for the great 2011 Tohoku earthquake (Mw= 9.1) from inversion of GRACE gravity data, Earth Planet Sc. Lett., 335–336, 72–79, https://doi.org/10.1016/j.epsl.2012.05.002, 2012. 
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A GRACE (Gravity Recovery and Climate Experiment)/GRACE-FO (Follow-On) mascon series is designed for studying ocean mass transport and circulation variations.  Mass distribution changes caused by major oceanic earthquakes and barystatic gravity, rotation, and deformation (GRD) have been removed. Errors were reduced via processing and regularization changes, particularly in the Arctic and near the removed earthquakes. This data set is designed for off-the-shelf oceanographic use.
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