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 …

Glaciers distinct from the Greenland and Antarctic ice sheets are shrinking rapidly, altering
regional hydrology, raising global sea level and elevating natural hazards. Yet, owing to the …

This chapter assesses the state of physical, biological and social knowledge concerning the
Arctic and Antarctic ocean and cryosphere, how they are affected by climate change, and …

The precise positioning and long-term monitoring of the grounding line, forming the
boundary between grounded and floating ice of marine ice sheets and tidewater glaciers, is …

We use time series of time‐variable gravity from the Gravitational Recovery and Climate
Experiment (GRACE) and GRACE Follow‐On (GRACE‐FO) missions to evaluate the mass …

Since the first estimates of Svalbard-wide glacier mass balance were made in the early
2000s, there has been great progress in remote sensing and modeling of mass balance …

This chapter assesses the state of physical, biological and social knowledge concerning the
Arctic and Antarctic ocean and cryosphere, how they are affected by climate change, and …

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 …

We generate a high spatial and temporal record of ice loss across glaciers globally for the
first time from CryoSat‐2 swath interferometric radar altimetry. We show that between 2010 …

Compared to other Arctic ice masses, Svalbard glaciers are low-elevated with flat interior
accumulation areas, resulting in a marked peak in their current hypsometry (area-elevation …