Over the modern satellite era, substantial climatic changes have been observed in the
Antarctic, including atmospheric and oceanic warming, ice sheet thinning and a general …

Abstract The Antarctic Ice Sheet (AIS) is out of equilibrium with the current anthropogenic‐
enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …

We evaluate modelled Antarctic ice sheet (AIS) near-surface climate, surface mass balance
(SMB) and surface energy balance (SEB) from the updated polar version of the regional …

Antarctic terrestrial biodiversity occurs almost exclusively in ice-free areas that cover less
than 1% of the continent. Climate change will alter the extent and configuration of ice-free …

Abstract The Southern Annular Mode (SAM) is the primary pattern of climate variability in the
Southern Hemisphere,, influencing latitudinal rainfall distribution and temperatures from the …

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 …

Warming of the Antarctic Peninsula in the latter half of the twentieth century was greater than
any other terrestrial environment in the Southern Hemisphere, and clear cryospheric and …

Ice shelves modulate Antarctic contributions to sea-level rise and thereby represent a
critical, climate-sensitive interface between the Antarctic ice sheet and the global ocean …

Mass loss from the Antarctic Ice Sheet is dominated by ice dynamics, where ocean-driven
melt leads to un-buttressing and ice flow acceleration. Long-term ice speed change has …

In the 2019/2020 austral summer, the surface melt duration and extent on the northern
George VI Ice Shelf (GVIIS) was exceptional compared to the 31 previous summers of …