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

The variability of the Antarctic and Greenland ice sheets occurs on various timescales and is
important for projections of sea level rise; however, there are substantial uncertainties …

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 …

The determination of the gravity model for the Gravity Recovery and Climate Experiment
(GRACE) is susceptible to modeling errors, measurement noise, and observability issues …

We discuss several classes of improvements to gravity solutions from the Gravity Recovery
and Climate Experiment (GRACE) mission. These include both improvements in …

Global mean sea level is an integral of changes occurring in the climate system in response
to unforced climate variability as well as natural and anthropogenic forcing factors. Its …

Abstract We use Gravity Recovery and Climate Experiment (GRACE) monthly gravity fields
to determine the regional acceleration in ice mass loss in Greenland and Antarctica for 2003 …

Glacial isostatic adjustment (GIA) describes the response of the solid Earth, the gravitational
field, and the oceans to the growth and decay of the global ice sheets. A commonly studied …

Climate-driven changes in land water storage and their contributions to sea level rise have
been absent from Intergovernmental Panel on Climate Change sea level budgets owing to …

Continuous observations of temporal variations in the Earth's gravity field have recently
become available at an unprecedented resolution of a few hundreds of kilometers. The …