Rapid ice loss from the Greenland ice sheet since 1992 is due in equal parts to increased
surface melting and accelerated ice flow. The latter is conventionally attributed to ocean …

Nearly every glacier in Greenland has thinned or retreated over the past few decades,,–,
leading to glacier acceleration, increased rates of sea-level rise and climate impacts around …

Mass loss from the Antarctic Ice Sheet is the main source of uncertainty in projections of
future sea-level rise, with important implications for coastal regions worldwide. Central to …

Sea-level rise may accelerate significantly if marine ice sheets become unstable. If such
instability occurs, there would be considerable uncertainty in future sea-level rise projections …

Abstract The Greenland Ice Sheet is the largest land ice contributor to sea level rise. This will
continue in the future but at an uncertain rate and observational estimates are limited to the …

The effect of the North Atlantic Ocean on the Greenland Ice Sheet through submarine
melting of Greenland's tidewater glacier calving fronts is thought to be a key driver of …

Geology and bed topography influence how ice sheets respond to climate change. Despite
the West Antarctic Ice Sheet's capacity to retreat and advance quickly over its over …

Many marine-terminating outlet glaciers have retreated rapidly in recent decades, but these
changes have not been formally attributed to anthropogenic climate change. A key …

Modeling and observations suggest that Thwaites Glacier, West Antarctica, has begun
unstable retreat. Concurrently, oceanographic observations have revealed substantial …

Traditionally, acoustic streaming is assumed to be a steady-state, relatively slow fluid
response to passing acoustic waves. This assumption, the so-called slow streaming …