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 construct the probability density function of global sea level at 2100, estimating that sea
level rises larger than 180 cm are less than 5% probable. An upper limit for global sea level …

Considerable progress has been made in understanding the present and future regional
and global sea level in the 2 years since the publication of the Fifth Assessment Report …

We use the BISICLES adaptive mesh ice sheet model to carry out one, two, and three
century simulations of the fast-flowing ice streams of the West Antarctic Ice Sheet, deploying …

Sea level rise poses a significant threat to coastal communities, infrastructure, and
ecosystems. Sea level rise is not uniform globally but is affected by a range of regional …

Abstract Totten Glacier, East Antarctica, a glacier that holds a 3.9 m sea level change
equivalent, has thinned and lost mass for decades. We map its grounding line positions in …

Simulations of the glacial–interglacial history of the Antarctic Ice Sheet provide insights into
dynamic threshold behavior and estimates of the ice sheet's contributions to global sea-level …

Present-day mass loss from the West Antarctic ice sheet is centred on the Amundsen Sea
Embayment (ASE), primarily through ice streams, including Pine Island, Thwaites and Smith …

Increasing ice flux from glaciers retreating over deepening (retrograde) bed topography has
been implicated in the recent acceleration of mass loss from the Greenland and Antarctic ice …

We produced a 6 year time series of differential tidal displacement for Pine Island Ice Shelf,
Antarctica, using speckle‐tracking methods applied to fine‐resolution TerraSAR‐X data …