The aims of this review are to:(a) describe and interpret structures in valley glaciers in
relation to strain history; and (b) to explore how these structures inform our understanding of …

Ice sheet response to forced changes—such as that from anthropogenic climate forcing—is
closely regulated by two‐way interactions with other components of the Earth system. These …

The floating ice shelves along the seaboard of the Antarctic ice sheet restrain the outflow of
upstream grounded ice,. Removal of these ice shelves, as shown by past ice-shelf recession …

The sudden propagation of a major preexisting rift (full-thickness crack) in late 2016 on the
Larsen C Ice Shelf, Antarctica led to the calving of tabular iceberg A68 in July 2017, one of …

Ice shelves control sea-level rise through frictional resistance, which slows the seaward flow
of grounded glacial ice. Evidence from around Antarctica indicates that ice shelves are …

The catastrophic collapses of Larsen A and B ice shelves on the eastern Antarctic Peninsula
have caused their tributary glaciers to accelerate, contributing to sea-level rise and …

Rapid retreat of the Larsen A and B ice shelves has provided important clues about the ice
shelf destabilization processes. The Larsen C Ice Shelf, the largest remaining ice shelf on …

Icebergs impact the physical and biological properties of the ocean where they drift,
depending on the degree of melting. We use satellite imagery and altimetry to quantify the …

We use model data from the Antarctic Mesoscale Prediction System (AMPS), measurements
from automatic weather stations and satellite observations to investigate the association …

The Antarctic Peninsula has seen rapid and widespread changes in the extent of its ice
shelves in recent decades, including the collapse of the Larsen A and B ice shelves in 1995 …