During the last glacial the ice sheet that subsumed most of Britain, Ireland and the North Sea
attained its maximum extent by 27 ka BP and with an ice volume sufficient to raise global …

Constraining how much and how fast the West Antarctic Ice Sheet (WAIS) will change in the
coming decades has recently been identified as the highest priority in Antarctic research …

Thwaites Glacier is one of the fastest-changing ice–ocean systems in Antarctica,–. Much of
the ice sheet within the catchment of Thwaites Glacier is grounded below sea level on …

Since 1992, there has been a revolution in our ability to quantify the land ice contribution to
sea level rise using a variety of satellite missions and technologies. Each mission has …

We present Bedmap2, a new suite of gridded products describing surface elevation, ice-
thickness and the seafloor and subglacial bed elevation of the Antarctic south of 60° S. We …

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 …

“Climate Shock could have reasonably been called But Will the People Notice? It'sa
layperson's survey of climate economics, a field that includes cost-benefit analysis and other …

This chapter considers changes in global mean sea level, regional sea level, sea level
extremes, and waves. Confidence in projections of global mean sea level rise has increased …

We present regional sea-level projections and associated uncertainty estimates for the end
of the 21 st century. We show regional projections of sea-level change resulting from …

During the last interglacial (LIG) period, global mean sea level (GMSL) was higher than at
present, likely driven by greater high-latitude insolation. Past sea-level estimates require …