ICESat has provided surface elevation measurements of the ice sheets since the launch in
January 2003, resulting in a unique dataset for monitoring the changes of the cryosphere …

We derive mass changes of the Greenland ice sheet (GIS) for 2003–07 from ICESat laser
altimetry and compare them with results for 1992–2002 from ERS radar and airborne laser …

Observed changes in the surface elevation of the Greenland Ice Sheet are caused by ice
dynamics, basal elevation change, basal melt, surface mass balance (SMB) variability, and …

The Greenland ice sheet is a major contributor to sea level rise, adding on average
0.47±0.23 mm year− 1 to global mean sea level between 1991 and 2015. The cryosphere …

Data from the ICESat/GLAS laser altimetry mission is used to obtain an estimate of the
volume change of Greenland's ice sheet over the time span of February 2003 to April 2007 …

Results from a regional climate simulation (1970–2006) over the Greenland ice sheet (GrIS)
reveals that more than 97% of the interannual variability of the modelled Surface Mass …

Four high-resolution regional climate models (RCMs) have been set up for the area of
Greenland, with the aim of providing future projections of Greenland ice sheet surface mass …

The shape of the large ice sheets responds rapidly to climate change, making the elevation
changes of these ice-covered regions an essential climate variable. Consistent, long time …

This study examines the recent evolution of the Greenland ice sheet and its six major
drainage basins. Based on laser altimetry data acquired by the Ice, Cloud and Land …

A new methodology for retrieval of glacier and ice sheet elevations and elevation changes
from CryoSat-2 data is presented. Surface elevations and elevation changes determined …