Time-resolved satellite gravimetry has revolutionized understanding of mass transport in the
Earth system. Since 2002, the Gravity Recovery and Climate Experiment (GRACE) has …

Sea-level variations spread over a very broad spectrum of spatial and temporal scales as a
result of complex processes occurring in the Earth System in response to natural variability …

The rate of global-mean sea-level rise since 1900 has varied over time, but the contributing
factors are still poorly understood. Previous assessments found that the summed …

Abstract The Antarctic Ice Sheet is an important indicator of climate change and driver of sea-
level rise. Here we combine satellite observations of its changing volume, flow and …

Glaciers outside of the ice sheets are known to be important contributors to sea level rise. In
this work, we provide an overview of changes in the mass of the world's glaciers, excluding …

While there is evidence for an acceleration in global mean sea level (MSL) since the 1960s,
its detection at local levels has been hampered by the considerable influence of natural …

Abstract The Greenland Ice Sheet (GIS) is losing mass at a high rate 1. Given the short-term
nature of the observational record, it is difficult to assess the historical importance of this …

The melting of ice sheets and global glaciers results in sea-level rise, a pole-to-equator
mass transport increasing Earth's oblateness and resulting in an increase in the length of …

We estimate the rates and patterns of vertical land motion (VLM) on all locations on Earth's
land surface using GPS Imaging. The solution is based on a large database of uniformly …

Earth's energy imbalance (EEI) is a fundamental metric of global Earth system change,
quantifying the cumulative impact of natural and anthropogenic radiative forcings and …