With the increased availability of very high-resolution satellite imagery, terrain based
imaging and participatory sensing, inexpensive platforms, and advanced information and …

This paper compiles and reviews marine and terrestrial data constraining the dimensions
and configuration of the Antarctic Peninsula Ice Sheet (APIS) from the Last Glacial Maximum …

In recent decades, hundreds of glaciers draining the Antarctic Peninsula (63° to 70° S) have
undergone systematic and progressive change. These changes are widely attributed to …

Glaciers and their changes through time are increasingly obtained from a wide range of
satellite sensors. Due to the often remote location of glaciers in inaccessible and high …

Since 1995 several ice shelves in the Northern Antarctic Peninsula have collapsed and
triggered ice-mass unloading, invoking a solid Earth response that has been recorded at …

Over the past 50 years, warming of the Antarctic Peninsula has been accompanied by
accelerating glacier mass loss and the retreat and collapse of ice shelves. A key driver of ice …

Surface meltwater ponding has been implicated as a major driver for recent ice shelf
collapse as well as the speedup of tributary glaciers in the northeast Antarctic Peninsula …

During the last few decades, several sectors in Antarctica have transitioned from glacial
mass balance equilibrium to mass loss. In order to determine if recent trends exceed the …

Glaciers on the Antarctic Peninsula have recently shown changes in extent, velocity and
thickness, yet there is little quantification of change in the mass balance of individual …

Abstract The northern Antarctic Peninsula is one of the fastest changing regions on Earth.
The disintegration of the Larsen-A Ice Shelf in 1995 caused tributary glaciers to adjust by …