An ice sheet model was constrained to reconstruct the evolution of the Greenland Ice Sheet
(GrIS) from the Last Glacial Maximum (LGM) to present to improve our understanding of its …

From the red grouse to the Ethiopian bush-crow, bird populations around the world can
provide us with vital insights into the effects of climate change on species and ecosystems …

The evolution of past global ice sheets is highly uncertain. One example is the missing ice
problem during the Last Glacial Maximum (LGM, 26 000-19 000 years before present)–an …

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 …

We have determined the ice mass evolution of the Antarctic and Greenland ice sheets (AIS
and GIS) and Gulf of Alaska (GOA) glaciers from a new GRACE global solution of equal …

Abstract Greenland Ice Sheet (GrIS) mass loss has accelerated since the turn of the twenty‐
first century. Several recent episodes of rapid GrIS ablation coincided with intense moisture …

As the planet cooled from peak warmth in the early Cenozoic, extensive Northern
Hemisphere ice sheets developed by 2.6 Ma ago, leading to changes in the circulation of …

Several decades of ice‐penetrating radar surveys of the Greenland and Antarctic ice sheets
have observed numerous widespread internal reflections. Analysis of this radiostratigraphy …

Abstract The Greenland Ice Sheet (GIS) contains the equivalent of 7.4 metres of global sea-
level rise. Its stability in our warming climate is therefore a pressing concern. However, the …

Reconstructing the growth and decay of palaeo-ice sheets is critical to understanding
mechanisms of global climate change and associated sea-level fluctuations in the past …