Abstract Totten Glacier, East Antarctica, a glacier that holds a 3.9 m sea level change
equivalent, has thinned and lost mass for decades. We map its grounding line positions in …

Abstract Denman Glacier, East Antarctica, holds an ice volume equivalent to a 1.5 m rise in
global sea level. Using satellite radar interferometry from the COSMO‐SkyMed constellation …

We employ Sentinel‐1a C band satellite radar interferometry data in Terrain Observation
with Progressive Scans mode to map the grounding line and ice velocity of Pope, Smith, and …

We measure the grounding line retreat of glaciers draining the Amundsen Sea sector of
West Antarctica using Earth Remote Sensing (ERS‐1/2) satellite radar interferometry from …

Abstract The Pope, Smith and Kohler glaciers, in the Amundsen Sea Embayment of West
Antarctica, have experienced enhanced ocean-induced ice-shelf melt, glacier acceleration …

Thwaites Glacier, the second largest ice stream in West Antarctica, drains an area of 166
500±2000 km2 which accumulates 55±5 Gt a− 1 (or 60±6 km3 ice a− 1) into the Amundsen …

Recent satellite investigations revealed that in the 1990s the grounding line of Pine Island
and Thwaites Glaciers, West Antarctica, retreated several km, the ice surface on the interior …

Abstract Changes to the grounding line, where grounded ice starts to float, can be used as a
remotely sensed measure of ice‐sheet susceptibility to ocean‐forced dynamic thinning …

Grounding lines are a key indicator of ice-sheet instability, because changes in their position
reflect imbalance with the surrounding ocean and affect the flow of inland ice. Although the …

Abstract The Totten and Moscow University glaciers, located in East Antarctica, contain 5.1
m sea-level equivalent of ice and have been losing mass over recent decades. Using …