Retrieval of glacier ice thickness is extremely important for monitoring water resources and
predicting glacier dynamics and changes. The inter-annual glacier ice thickness …

This study investigates rock glacier destabilization based on the results of a unique in situ
and remote-sensing-based monitoring network focused on the kinematics of the rock glacier …

The basal thermal state (frozen or thawed) of the Greenland Ice Sheet is under-constrained
due to few direct measurements, yet knowledge of this state is becoming increasingly …

The distribution of pressure on the vertical seaward front of an ice shelf has been shown to
cause downward bending of the shelf if the ice is assumed to have vertically uniform …

We investigate the mass changes of Antarctic glaciers from 2003 to 2020, partitioning them
into the contributions of surface mass balance (SMB) and ice discharge, using high …

The flow of glaciers is largely controlled by changes at the ice–bed interface, where basal
slip and sediment deformation drive basal glacier motion. Determining subglacial conditions …

Glacier flow modulates sea level and is governed largely by the viscous deformation of ice.
Multiple molecular-scale mechanisms facilitate viscous deformation, but it remains unclear …

Accurately modeling the deformation of temperate glacier ice, which is at its pressure-
melting temperature and contains liquid water at grain boundaries, is essential for predicting …

Forecasting hanging glacier instabilities remain challenging as sensing technology focusing
on the ice surface fails to detect englacial damage leading to large‐scale failure. Here, we …

Glacial reworking of large rock avalanche sediment significantly contributes to glacial
sediment transfer. This study presents two interaction models, derived from a …