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Sparse DDK
Sparse DDK: A Data-Driven Decorrelation Filter for GRACE Level-2 Products
How to quantify the accuracy of mass anomaly time-series based on GRACE data in the absence of knowledge about true signal?
How to quantify the accuracy of mass anomaly time-series based on GRACE data in the absence of knowledge about true signal?
Analysis and Mitigation of Biases in Greenland Ice Sheet Mass Balance Trend Estimates From GRACE Mascon Products
Analysis and Mitigation of Biases in Greenland Ice Sheet Mass Balance Trend Estimates From GRACE Mascon Products
Improved recovery of temporal variations of the Earth’s gravity field from satellite kinematic orbits using an epoch-difference scheme
Improved recovery of temporal variations of the Earth’s gravity field from satellite kinematic orbits using an epoch-difference scheme
Using GRACE to Explain Variations in the Earth's Oblateness
Using GRACE to Explain Variations in the Earth's Oblateness
Evaluating GRACE Mass Change Time Series for the Antarctic and Greenland Ice Sheet—Methods and Results
Evaluating GRACE Mass Change Time Series for the Antarctic and Greenland Ice Sheet—Methods and Results
Conversion of time-varying Stokes coefficients into mass anomalies at the Earth’s surface considering the Earth’s oblateness
Conversion of time-varying Stokes coefficients into mass anomalies at the Earth’s surface considering the Earth’s oblateness
Estimation and reduction of random noise in mass anomaly time-series from satellite gravity data by minimization of month-to-month year-to-year double differences
Estimation and reduction of random noise in mass anomaly time-series from satellite gravity data by minimization of month-to-month year-to-year double differences
Optimal mascon geometry in estimating mass anomalies within Greenland from GRACE
Optimal mascon geometry in estimating mass anomalies within Greenland from GRACE
Regularization and analysis of GRACE mass anomaly time series by a minimization of month-to-month year-to-year double differences
Regularization and analysis of GRACE mass anomaly time series by a minimization of month-to-month year-to-year double differences
Geocentre motion and Earth's dynamic oblateness time-series derived from GRACE CSR RL06 solutions and geophysical models
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)
Assessment of GRACE monthly solutions by quantifying the noise level in mass anomaly time-series with the variance component estimation (PPT)
How to optimize the spatial resolution of GRACE data for studying mass anomaly trends of the Greenland and Antarctic Ice Sheets? (PPT)
How to optimize the spatial resolution of GRACE data for studying mass anomaly trends of the Greenland and Antarctic Ice Sheets? (PPT)
Seasonal mass variations show timing and magnitude of meltwater storage in the Greenland ice sheet
Seasonal mass variations show timing and magnitude of meltwater storage in the Greenland ice sheet
Improvements in the Monthly Gravity Field Solutions Through Modeling the Colored Noise in the GRACE Data
Improvements in the Monthly Gravity Field Solutions Through Modeling the Colored Noise in the GRACE Data
Statistically optimal estimation of degree-1 and C<sub>20</sub> coefficients based on GRACE data and an ocean bottom pressure model
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
Improving estimates of water resources in a semi-arid region by assimilating GRACE data into the PCR-GLOBWB hydrological model
Earth’s gravity field modelling based on satellite accelerations derived from onboard GPS phase measurements
Earth’s gravity field modelling based on satellite accelerations derived from onboard GPS phase measurements
A high resolution model of linear trend in mass variations from DMT-2
A high resolution model of linear trend in mass variations from DMT-2: Added value of accounting for coloured noise in GRACE data
Statistically optimal estimation of Greenland Ice Sheet mass variations from GRACE monthly solutions using an improved mascon approach
Statistically optimal estimation of Greenland Ice Sheet mass variations from GRACE monthly solutions using an improved mascon approach
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