It is argued that Larsen Ice Shelf contains marine ice formed by oceanic freezing and other
mechanisms. Missing basal returns in airborne radar soundings and observations of a …

In May 2000 the US Antarctic Research Vessel Nathaniel B. Palmer braved extensive ice
and the frigid temperatures of the Northwest Weddell Sea to penetrate the coastal leads …

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 …

Because ice shelves respond to climatic forcing over a range of time scales, from years to
millennia, an understanding of their long-term history is critically needed for predicting their …

Marine ice is mainly formed by the accumulation and consolidation of ice platelets beneath
anice shelf. Layers of marine ice beneath ice shelves provide strong evidence of a vigorous …

During the austral summer of 2001/02, melting at the surface of Larsen Ice Shelf in the
Antarctic Peninsula was three times greater than the average of five previous summers. This …

On August 13, 2005, almost the entire Ayles Ice Shelf (87.1 km2) calved off within an hour
and created a new 66.4 km2 ice island in the Arctic Ocean. This loss of one of the six …

The collapses of the Larsen A and B ice shelves on the Antarctic Peninsula in 1995 and
2002 confirm the impact of southward-propagating climate warming in this region. Recent …

We modelled the flow of the Larsen C and northernmost Larsen D ice shelves, Antarctic
Peninsula, using a model of continuum mechanics of ice flow, and applied a fracture …

Sea‐ice ice shelves, at the apex of North America (> 80° N), constitute the oldest sea ice in
the Northern Hemisphere. We document the establishment and subsequent stability of the …