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 …

While there are numerous hypotheses concerning glacial–interglacial environmental and
climatic regime shifts in the Arctic Ocean, a holistic view on the Northern Hemisphere's late …

Recent observations show that the rate at which the Antarctic ice sheet (AIS) is contributing
to sea level rise is increasing. Increases in ice‐ocean heat exchange have the potential to …

Floating ice shelves, which fringe most of Antarctica's coastline, regulate ice flow into the
Southern Ocean,–. Their thinning,,–or disintegration, can cause upstream acceleration of …

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 growth and reduction of Northern Hemisphere ice sheets over the past million years is
dominated by an approximately 100,000-year periodicity and a sawtooth pattern,(gradual …

Global-scale 21st-century glacier mass change projections from six published global glacier
models are systematically compared as part of the Glacier Model Intercomparison Project. In …

Global mean sea level has been steadily rising over the last century, is projected to increase
by the end of this century, and will continue to rise beyond the year 2100 unless the current …

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 …

Over the past decade, ice loss from the Greenland Ice Sheet increased as a result of both
increased surface melting and ice discharge to the ocean,. The latter is controlled by the …