Since few time‐variable gravity field models were developed before the Gravity Recovery
and Climate Experiment (GRACE) era, one normally estimates the global mean ocean mass …

Understanding global sea level variations and exploring their causes hold significant
importance for future climate change predictions and the sustainable development of …

Accurate estimates of global sea-level change from the observations of Altimetry, Argo and
Gravity Recovery and Climate Experiment (GRACE) and GRACE Follow-on (GRACE-FO) …

Abstract Space gravity measurements have been mainly used to study the temporal mass
variations at the Earth's surface and within the mantle. Nevertheless, mass variations due to …

Considering the nonlinear and non-stationary characteristics of sea-level-change time
series, this study focuses on enhancing the predictive accuracy of sea level change. The …

Removing stripe noise from the GRACE (Gravity Recovery and Climate Experiment) monthly
gravity field model is crucial for accurately interpreting temporal gravity variations. The …

Abstract The Antarctic Ice Sheet (AIS) has been losing ice mass and contributing to global
sea level rise (GSLR). Given its mass that is enough to cause∼ 58 m of GSLR, accurate …

The discrepancy in the observed global mean sea level budget increased significantly since
2016, but the budget discrepancy over basin‐scales is unclear. In this contribution, we …

利用重力卫星监测全球水储量变化, 有助于应对全球气候变化, 防灾减灾等挑战,
具有重要的科学意义. 国际上已发布了多个系列的重力恢复和气候实验(gravity recovery and …

Accurate error covariance is crucial for post-processing GRACE gravity field solutions in
terms of Spherical Harmonic Coefficients (SHCs). Unfortunately, most GRACE SHC products …