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 …

Supraglacial lakes (SGLs) enhance surface melting and can flex and fracture ice shelves
when they grow and subsequently drain, potentially leading to ice shelf disintegration …

Core 2011804‐0010 from easternmost Lancaster Sound provides important insights into
deglacial timing and style at the marine margin of the NE Laurentide Ice Sheet (LIS) …

We derive the surface density and brine infiltration depth/extent at McMurdo Ice Shelf,
Antarctica, from combined analysis of radar profiles and radar statistical reconnaissance of …

We collected~ 1300 km of ground-penetrating radar profiles over McMurdo Ice Shelf,
Antarctica, using frequencies between 40 and 400 MHz to determine extent, continuity and …

We use borehole optical televiewing (OPTV) to explore the internal structure of Larsen C Ice
Shelf (LCIS). We report a suite of five~ 90 m long OPTV logs, recording a light‐emitting …

Abstract During the Last Glacial Maximum (LGM), a grounded ice sheet filled the Ross Sea
Embayment in Antarctica and deposited glacial sediments on volcanic islands and …

Surface debris covers much of the western portion of the McMurdo Ice Shelf and has a
strong influence on the local surface albedo and energy balance. Differential ablation …

Ice shelves are an important component of the Antarctic Ice Sheet as they indirectly control
sea level rise by regulating mass flux into the ocean. The coupling of ice shelves with the …

Ponds that form on sea ice can cause it to thin or break-up, which can promote calving from
an adjacent ice shelf. Studies of sea ice ponds have predominantly focused on Arctic ponds …