- A global semi-empirical glacial isostatic adjustment (GIA) model based on Gravity Recovery and Climate Experiment (GRACE) data
- Statistically optimal estimation of degree-1 and C20 coefficients based on GRACE data and an ocean bottom pressure model
- A high resolution model of linear trend in mass variations from DMT-2: Added value of accounting for coloured noise in GRACE data
- Optimizing estimates of annual variations and trends in geocentermotion and J2 from a combination of GRACE data and geophysical models