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 …

Abstract The Greenland Ice Sheet has been a major contributor to global sea-level rise in
recent decades,, and it is expected to continue to be so. Although increases in glacier flow …

We evaluate modelled Antarctic ice sheet (AIS) near-surface climate, surface mass balance
(SMB) and surface energy balance (SEB) from the updated polar version of the regional …

We evaluate modelled Greenland ice sheet (GrIS) near-surface climate, surface energy
balance (SEB) and surface mass balance (SMB) from the updated regional climate model …

Observations and models agree that the Greenland Ice Sheet (GrIS) surface mass balance
(SMB) has decreased since the end of the 1990s due to an increase in meltwater runoff and …

Mass loss from the West Antarctic Ice Sheet is dominated by glaciers draining into the
Amundsen Sea Embayment (ASE), yet the impact of anomalous precipitation on the mass …

The Greenland Ice Sheet holds 7.2 m of sea level equivalent and in recent decades, rising
temperatures have led to accelerated mass loss. Current ice margin recession is led by the …

We compare the performance of five different regional climate models (RCMs)(COSMO-CLM
2, HIRHAM5, MAR3. 10, MetUM, and RACMO2. 3p2), forced by ERA-Interim reanalysis, in …

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 …

Rapid mass loss from the Greenland Ice Sheet (GrIS) is affecting sea level and, through
increased freshwater and sediment discharge, ocean circulation, sea-ice, biogeochemistry …