We construct long-term time series of Greenland and Antarctic ice sheet mass change from satellite gravity measurements. A statistical reconstruction approach is developed based on a Principal Component Analysis to combine high-resolution spatial modes from the Gravity Recovery and Climate Experiment (GRACE) mission with the gravity information from conventional satellite track-ing data. Uncertainties of this reconstruction are rigorously assessed; they include temporal limitations for short GRACE measurements, spatial limitations for the low-resolution conventional tracking data measurements, and limitations of the estimated statistical relationships between low and high degree potential coe�cients re ected in the PCA modes. Trend...
Redistribution of mass over the Earth and within the mantle changes the gravity field whose variatio...
A least squares inversion of satellite laser ranging (SLR) data over Greenland and Antarctica could ...
Abstract:The Antarctic ice sheet is the largest block of ice on Earth, a tiny change of its ice shee...
We construct long-term time series of Greenland and Antarctic ice sheet mass change from satellite ...
We construct long-term time series of Greenland and Antarctic ice sheet mass change from satellite g...
Satellite gravimetry data acquired by the Gravity Recovery and Climate Experiment (GRACE) allows to ...
We present regional-scale mass balances for 25 drainage basins of the Antarctic Ice Sheet (AIS) from...
Time-variable gravity data from the Gravity Recovery and Climate Experiment (GRACE) mission have bee...
We use monthly measurements of time‐variable gravity from the GRACE (Gravity Recovery and Climate Ex...
Measuring present day changes in the volume of the Antarctic ice sheet has traditionally been diffic...
The Greenland and Antarctic ice sheets have been reported to be losing mass at accelerating rates1, ...
Time-variable gravity measurements from the Gravity Recovery and Climate Experiment (GRACE) and GRAC...
Accurate estimation of ongoing Antarctic ice mass change is important to predict future ice mass los...
We use Gravity Recovery and Climate Experiment (GRACE) monthly gravity fields to determine the regio...
The dynamic stability of the Antarctic Ice Sheet is one of the largest uncertainties in projections ...
Redistribution of mass over the Earth and within the mantle changes the gravity field whose variatio...
A least squares inversion of satellite laser ranging (SLR) data over Greenland and Antarctica could ...
Abstract:The Antarctic ice sheet is the largest block of ice on Earth, a tiny change of its ice shee...
We construct long-term time series of Greenland and Antarctic ice sheet mass change from satellite ...
We construct long-term time series of Greenland and Antarctic ice sheet mass change from satellite g...
Satellite gravimetry data acquired by the Gravity Recovery and Climate Experiment (GRACE) allows to ...
We present regional-scale mass balances for 25 drainage basins of the Antarctic Ice Sheet (AIS) from...
Time-variable gravity data from the Gravity Recovery and Climate Experiment (GRACE) mission have bee...
We use monthly measurements of time‐variable gravity from the GRACE (Gravity Recovery and Climate Ex...
Measuring present day changes in the volume of the Antarctic ice sheet has traditionally been diffic...
The Greenland and Antarctic ice sheets have been reported to be losing mass at accelerating rates1, ...
Time-variable gravity measurements from the Gravity Recovery and Climate Experiment (GRACE) and GRAC...
Accurate estimation of ongoing Antarctic ice mass change is important to predict future ice mass los...
We use Gravity Recovery and Climate Experiment (GRACE) monthly gravity fields to determine the regio...
The dynamic stability of the Antarctic Ice Sheet is one of the largest uncertainties in projections ...
Redistribution of mass over the Earth and within the mantle changes the gravity field whose variatio...
A least squares inversion of satellite laser ranging (SLR) data over Greenland and Antarctica could ...
Abstract:The Antarctic ice sheet is the largest block of ice on Earth, a tiny change of its ice shee...