GRACE and GRACE Follow-On Gravity Observations of Intermediate-Depth Earthquakes Contrasted With Those of Shallow Events

Statistically optimal estimation of surface mass anomalies by directly using GRACE level-2 spherical harmonic coefficients as measurements

Dayside Upper-Thermospheric Density Fluctuations as Observed by GRACE and GRACE-FO at ∼500 km Height

Enhancing spatial resolution of GRACE-derived groundwater storage anomalies in Urmia catchment using machine learning downscaling methods

Adaptive DDK Filter for GRACE Time‐Variable Gravity Field with a Novel Anisotropic Filtering Strength Metric

How to quantify the accuracy of mass anomaly time-series based on GRACE data in the absence of knowledge about true signal?

Sparse DDK: A Data-Driven Decorrelation Filter for GRACE Level-2 Products

Analysis and Mitigation of Biases in Greenland Ice Sheet Mass Balance Trend Estimates From GRACE Mascon Products

On the performance of equiangular mascon solution in GRACE-like missions

Improving the Representation of Long-Term Storage Variations With Conceptual Hydrological Models in Data-Scarce Regions

Separating Long-Term and Short-Term Mass Changes of Antarctic Ice Drainage Basins: A Coupled State Space Analysis of Satellite Observations and Model Products

A simulation study for future satellite gravimetry missions

Sea Level Budgets Should Account for Ocean Bottom Deformation

Improved recovery of temporal variations of the Earth’s gravity field from satellite kinematic orbits using an epoch-difference scheme

Multivariate data assimilation of GRACE, SMOS, SMAP measurements for improved regional soil moisture and groundwater storage estimates

Estimation of regional mass balance changes of the Greenland ice sheet using GRACE data and the Input-output method

Global glacier mass loss during the GRACE satellite mission (2002-2016)

Evaluating GRACE Mass Change Time Series for the Antarctic and Greenland Ice Sheet—Methods and Results

Using GRACE to Explain Variations in the Earth's Oblateness

Conversion of time-varying Stokes coefficients into mass anomalies at the Earth’s surface considering the Earth’s oblateness