The variability of the Antarctic and Greenland ice sheets occurs on various timescales and is
important for projections of sea level rise; however, there are substantial uncertainties …

Ice flow models of the Antarctic ice sheet are commonly used to simulate its future evolution
in response to different climate scenarios and inform on the mass loss that would contribute …

The Greenland ice sheet is one of the largest contributors to global mean sea-level rise
today and is expected to continue to lose mass as the Arctic continues to warm. The two …

Observations and models agree that the Greenland Ice Sheet (GrIS) surface mass balance
(SMB) has decreased since the end of the 1990s due to an increase in meltwater runoff and …

The future surface mass balance (SMB) will influence the ice dynamics and the contribution
of the Antarctic ice sheet (AIS) to the sea-level rise. Most of recent Antarctic SMB projections …

We provide an updated analysis of instrumental Greenland monthly temperature data to
2019, focusing mainly on coastal stations but also analysing ice‐sheet records from Swiss …

The sea level contribution of the Antarctic ice sheet constitutes a large uncertainty in future
sea level projections. Here we apply a linear response theory approach to 16 state-of-the-art …

Future climate projections show a marked increase in Greenland Ice Sheet (GrIS) runoff
during the 21st century, a direct consequence of the Polar Amplification signal. Regional …

Under future climate change scenarios it is virtually certain that global mean sea level will
continue to rise. But the rate at which this occurs, and the height and time at which it might …

Sea level rise (SLR) is a long‐lasting consequence of climate change because global
anthropogenic warming takes centuries to millennia to equilibrate for the deep ocean and …