The Antarctic Ice Sheet is losing mass at an accelerating pace, and ice loss will likely
continue over the coming decades and centuries. Some regions of the ice sheet may reach …

The release of new and updated sea‐level rise (SLR) information, such as from the
Intergovernmental Panel on Climate Change (IPCC) Assessment Reports, needs to be …

Abstract The Paris Agreement aims to limit global mean warming in the twenty-first century to
less than 2 degrees Celsius above preindustrial levels, and to promote further efforts to limit …

Abstract An IPCC Special Report on the impacts of global warming of 1.5 C above pre-
industrial levels and related global greenhouse gas emission pathways, in the context of …

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 …

Predictions for sea-level rise this century due to melt from Antarctica range from zero to more
than one metre. The highest predictions are driven by the controversial marine ice-cliff …

Robust appraisals of climate impacts at different levels of global-mean temperature increase
are vital to guide assessments of dangerous anthropogenic interference with the climate …

Coastal flood damage and adaptation costs under 21st century sea-level rise are assessed
on a global scale taking into account a wide range of uncertainties in continental topography …

Atmospheric warming is projected to increase global mean surface temperatures by 0.3 to
4.8 degrees Celsius above pre-industrial values by the end of this century. If anthropogenic …

Geological data indicate that global mean sea level has fluctuated on 10 3 to 10 6 yr time
scales during the last∼ 25 million years, at times reaching 20 m or more above modern. If …