Even if anthropogenic warming were constrained to less than 2° C above pre-industrial, the
Greenland and Antarctic ice sheets will continue to lose mass this century, with rates similar …

Global sea level provides an important indicator of the state of the warming climate, but
changes in regional sea level are most relevant for coastal communities around the world …

The land ice contribution to global mean sea level rise has not yet been predicted using ice
sheet and glacier models for the latest set of socio-economic scenarios, nor using …

Working Group I (WGI) of the Intergovernmental Panel on Climate Change (IPCC) assesses
the current evidence on the physical science of climate change, evaluating knowledge …

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 …

Sea-level rise projections and knowledge of their uncertainties are vital to make informed
mitigation and adaptation decisions. To elicit projections from members of the scientific …

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 …

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 …

Projection of the contribution of ice sheets to sea-level change as part of the Coupled Model
Intercomparison Project–phase 6 (CMIP6) takes the form of simulations from coupled ice …