Changes in ice mass are estimated from elevation changes derived from 10.5 years
(Greenland) and 9 years (Antarctica) of satellite radar altimetry data from the European …

Ice sheet mass balance estimates have improved substantially in recent years using a
variety of techniques, over different time periods, and at various levels of spatial detail …

A high-resolution GCM is found to simulate precipitation and surface energy balance of high
latitudes with high accuracy. This opens new possibilities to investigate the future mass …

The sum of winter accumulation and summer losses of mass from glaciers and ice sheets
(net surface mass balance) varies with changing climate. In the Arctic, glaciers and ice caps …

Mass changes of the Antarctic ice sheet impact sea-level rise as climate changes, but recent
rates have been uncertain. Ice, Cloud and land Elevation Satellite (ICESat) data (2003–08) …

In total, Icelandic ice caps contain∼ 3600 km3 of ice, which if melted would raise sea level
by∼ 1 cm. Here, we present an overview of mass changes of Icelandic ice masses since the …

Glaciers and ice caps are known to contribute significantly to present‐day sea level rise, but
there are still glaciated regions where little is known about modern changes in glacier mass …

We analyzed Antarctic ice-sheet elevation change (dH/dt) from 1995 to 2000 using 123
million elevation change measurements from European Remote Sensing 2 ice-mode …

New experiments were performed with three-dimensional thermomechanical models of the
Greenland and Antarctic ice sheets to simulate their behaviour during the glacial cycles, to …

The Antarctic contribution to sea-level rise has long been uncertain. While regional
variability in ice dynamics has been revealed, a picture of mass changes throughout the …