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 …

Antarctica's ice shelves modulate the grounded ice flow, and weakening of ice shelves due
to climate forcing will decrease their 'buttressing'effect, causing a response in the grounded …

Abstract The National Aeronautics and Space Administration (NASA)'s Operation IceBridge
(OIB) was a 13‐year (2009–2021) airborne mission to survey land and sea ice across the …

Melting of the Greenland ice sheet (GrIS) in response to anthropogenic global warming
poses a severe threat in terms of global sea-level rise (SLR). Modelling and palaeoclimate …

Speedup of Pine Island Glacier over the past several decades has made it Antarctica's
largest contributor to sea-level rise. The past speedup is largely due to grounding-line …

Ice shelf basal melting is the primary mechanism driving mass loss from the Antarctic Ice
Sheet, yet it is unknown how the localized melt enhancement from subglacial discharge will …

Mass loss from the Greenland ice sheet (GrIS) has increased over the last two decades in
response to changes in global climate, motivating the scientific community to question how …

We present the result of the third Marine Ice Sheet Intercomparison project, MISMIP+.
MISMIP+ is intended to be a test of ice flow models which include fast sliding marine ice …

The Thwaites Eastern Ice Shelf continues to buttresses a significant portion of Thwaites
Glacier through contact with a pinning point 40 km offshore of the present grounding line …

Petermann Glacier is a major outlet glacier of northern Greenland that drains a marine‐
based basin vulnerable to destabilization from enhanced oceanic and atmospheric forcings …