Surface mass balance (SMB) provides mass input to the surface of the Antarctic and
Greenland Ice Sheets and therefore comprises an important control on ice sheet mass …

Glaciers distinct from the Greenland and Antarctic ice sheets are currently losing mass
rapidly with direct and severe impacts on the habitability of some regions on Earth as glacier …

Since 1992, there has been a revolution in our ability to quantify the land ice contribution to
sea level rise using a variety of satellite missions and technologies. Each mission has …

Abstract Greenland Ice Sheet (GrIS) mass loss has accelerated since the turn of the twenty‐
first century. Several recent episodes of rapid GrIS ablation coincided with intense moisture …

Abstract We map recent Greenland Ice Sheet elevation change at high spatial (5 km) and
temporal (monthly) resolution using CryoSat‐2 altimetry. After correcting for the impact of …

Abstract Runoff from the Greenland Ice Sheet has increased over recent decades affecting
global sea level, regional ocean circulation, and coastal marine ecosystems, and it now …

The mass of the Greenland ice sheet is declining as mass gain from snow accumulation is
exceeded by mass loss from surface meltwater runoff, marine-terminating glacier calving …

Studies of the global sea-level budget (SLB) and the global ocean-mass budget (OMB) are
essential to assess the reliability of our knowledge of sea-level change and its contributors …

Satellite data have revealed that the Greenland and Antarctic Ice Sheets are changing
rapidly due to warming air and ocean temperatures. Crucially, Earth Observations can now …

Thirteen years of GRACE data provide an excellent picture of the current mass changes of
Greenland and Antarctica, with mass loss in the GRACE period 2002–2015 amounting to …