Oceans cover over 70% of the Earth's surface and provide numerous services to humans
and the environment. Therefore, it is crucial to monitor these valuable assets using …

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 …

We combined an ensemble of satellite altimetry, interferometry, and gravimetry data sets
using common geographical regions, time intervals, and models of surface mass balance …

We have determined the ice mass evolution of the Antarctic and Greenland ice sheets (AIS
and GIS) and Gulf of Alaska (GOA) glaciers from a new GRACE global solution of equal …

The fifth edition of this textbook has been completely revised and significantly extended in
order to reflect the revolution of geodetic technologies, methods and applications during the …

Tide gauges show that global sea level has risen about 7 inches during the 20th century,
and recent satellite data show that the rate of sea-level rise is accelerating. As Earth warms …

Spatial leakage is a major limitation for quantitative interpretation of satellite gravity
measurements from the gravity recovery and climate experiment (GRACE). Using synthetic …

Within the last decade, the Greenland ice sheet (GrIS) and its surroundings have
experienced record high surface temperatures (Mote, 2007; Box et al., 2010), ice sheet melt …

Over the last two decades, the Greenland ice sheet (GrIS) has been losing mass at an
increasing rate, enhancing its contribution to sea-level rise (SLR). The recent increases in …