The calving of Antarctic ice shelves remains unpredictable to date due to a lack of
understanding of the role of the different climatic components in such events. In this study …

Ice shelf instability is one of the main sources of uncertainty in Antarctica's contribution to
future 17 sea level rise. Calving events play crucial role in ice shelf weakening but remain …

Ice shelf instability is one of the main sources of uncertainty in Antarctica's contribution to
future sea level rise. Calving events play a crucial role in ice shelf weakening but remain …

The disintegration of the eastern Antarctic Peninsula's Larsen A and B ice shelves has been
attributed to atmosphere and ocean warming, and increased mass losses from the glaciers …

The Ross Ice Shelf (RIS) buttresses ice streams from the Antarctic continent and restrains
the grounded ice sheet from flowing into the ocean, which is important for the stability of the …

Iceberg calving is the main process that facilitates the dynamic mass loss of ice sheets into
the ocean, which accounts for approximately half of the mass loss of the Antarctic ice sheet …

The volume of Arctic sea ice is in decline but exhibits high interannual variability, which is
driven primarily by atmospheric circulation. Through analysis of satellite-derived ice …

In austral spring 2016 the Antarctic region experienced anomalous sea ice retreat in all
sectors, with sea ice extent in October and November 2016 being the lowest in the Southern …

The calving of A‐68, the 5,800‐km2, 1‐trillion‐ton iceberg shed from the Larsen C Ice Shelf
in July 2017, is one of over 10 significant ice‐shelf loss events in the past few decades …

Ice shelves in the Southern Weddell Sea have large areas and volumes, and have
previously been stable due to their setting in a region of cold near-surface and sub-surface …