In recent decades, the land-ocean aquatic continuum, commonly defined as the interface, or
transition zone, between terrestrial ecosystems and the open ocean, has undergone …

The aims of this review are to:(a) describe and interpret structures in valley glaciers in
relation to strain history; and (b) to explore how these structures inform our understanding of …

Antarctic ice shelves moderate the contribution of the Antarctic Ice Sheet to global sea level
rise; however, ice shelf health remains poorly constrained. Here, we present the annual …

The largest uncertainty in future sea-level rise is loss of ice from the Greenland and Antarctic
Ice Sheets. Ice shelves, freely floating platforms of ice that fringe the ice sheets, play a …

Most lake-terminating glaciers in the Himalaya retreat rapidly due to periodic frontal ice loss
at their terminus, but long-term observations are still limited regarding their flow dynamics …

The role of icebergs in narrow fjords hosting marine-terminating glaciers in Greenland is
poorly understood, even though iceberg melt results in a substantial freshwater flux that can …

Uncertainty about sea-level rise is dominated by uncertainty about iceberg calving, mass
loss from glaciers or ice sheets by fracturing. Review of the rapidly growing calving literature …

Future projections of global mean sea level change are uncertain, partly because of our
limited understanding of the dynamics of Greenland's outlet glaciers. Here we study …

Areas of structural damage mechanically weaken Antarctic ice shelves. This potentially
preconditions ice shelves for disintegration and enhanced grounding line retreat. The …

Ice shelf instability is one of the main sources of uncertainty in Antarctica's contribution to
future sea level rise. Calving events play a crucial role in ice shelf weakening but remain …