Most of the Greenland and Antarctic ice sheets are covered with firn—the transitional
material between snow and glacial ice. Firn is vital for understanding ice-sheet mass …

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 …

An accurate in-field estimate of soil moisture content (SMC) is critical for precision irrigation
management. Current ground methods to measure SMC were limited by the disadvantages …

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 …

An accurate regional estimate of soil moisture content (SMC) is important for water
management and drought monitoring. Traditional ground measurement methods of SMC are …

Surface topography across the marginal zone of the Greenland Ice Sheet is constantly
evolving in response to changing weather, season, climate, and ice dynamics. However …

Arctic warming has accelerated surface melting even in the highland areas of the Greenland
ice sheet (GrIS). Understanding the relationship between climate and surface melting is …

Icebergs account for half of all ice loss from Antarctica and, once released, present a hazard
to maritime operations. Their melting leads to a redistribution of cold fresh water around the …

Although fluctuations in ice sheet surface mass balance lead to seasonal and interannual
elevation changes, it is unclear if they are resolved differently by radar and laser satellite …

Surface topography across the marginal zone of the Greenland Ice Sheet is constantly
evolving in response to changes in weather, season, climate and ice dynamics. Yet current …