The ICEMASS project will derive and analyse glacier thickness changes using satellite laser and radar altimetry, and satellite-derived and other digital elevation models, and convert these to a global glacier mass budget. Such data set will enable major steps forward in glacier and Earth science, in particular: constrain current sea-level contribution from glaciers; complete climate change patterns as reflected in glacier mass changes; quantify the contribution of glacier imbalance to river run-off; allow the separation of glacier mass loss from other components of gravity changes as detected through satellite gravimetry; and allow improved modelling of the isostatic uplift component due to current changes in glacier load.
These results will be connected to global-scale glacier dynamics, for which a global set of repeat optical and radar satellite images will be processed to measure displacements due to glacier flow and their annual to decadal-scale changes. The analysis of these data will enable several major steps forward in glacier and Earth science, in particular: progress the understanding of glacier response to climate and its changes; provide new insights in processes underlying spatio-temporal variability and instability of glacier flow on decadal scales; improve understanding of dynamic thickness change effects; allow the estimation of global calving fluxes; progress understanding of transport in glaciers and their role in landscape development; and help to better assess potentially hazardous glacier lakes.