In a warming climate, surface meltwater production on large ice sheets is expected to
increase. If this water is delivered to the ice sheet base it may have important consequences …

Detection, attribution and projection of mass loss from the Greenland Ice Sheet has been a
central focus of the glaciological community, with surface meltwater thought to play a key …

Accurate prediction of global sea-level rise requires that we understand the cause of recent,
widespread and intensifying, glacier acceleration along Antarctic ice-sheet coastal margins …

Enhanced submarine ice-shelf melting strongly controls ice loss in the Amundsen Sea
embayment (ASE) of West Antarctica, but its magnitude is not well known in the critical …

Polar temperatures over the last several million years have, at times, been slightly warmer
than today, yet global mean sea level has been 6–9 metres higher as recently as the Last …

Supraglacial lakes are known to influence ice melt and ice flow on the Greenland ice sheet
and potentially cause ice shelf disintegration on the Antarctic Peninsula. In East Antarctica …

As continental ice from Antarctica reaches the grounding line and begins to float, its
underside melts into the ocean. Results obtained with satellite radar interferometry reveal …

The observed acceleration of outlet glaciers and ice flows in Greenland and Antarctica is
closely linked to ocean warming, especially in the subsurface layer,,,,. Accurate projections …

Satellite‐based estimates of ice shelf melt rates reach 200 m close to the grounding line of
Pine Island Glacier, in West Antarctica. However, ocean simulations have not yet been able …

Ocean waters melt the margins of Antarctic and Greenland glaciers, and individual glaciers'
responses and the integrity of their ice shelves are expected to depend on the spatial …