- Geocentre motion and Earth's dynamic oblateness time-series derived from GRACE CSR RL06 solutions and geophysical models
- Assessment of GRACE monthly solutions by quantifying the noise level in mass anomaly time-series with the variance component estimation (PPT)
- Improvements in the Monthly Gravity Field Solutions Through Modeling the Colored Noise in the GRACE Data
- Statistically optimal estimation of degree-1 and C20 coefficients based on GRACE data and an ocean bottom pressure model
- Improving estimates of water resources in a semi-arid region by assimilating GRACE data into the PCR-GLOBWB hydrological model
- A high resolution model of linear trend in mass variations from DMT-2: Added value of accounting for coloured noise in GRACE data