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 …

Abstract The Greenland Ice Sheet is losing mass at accelerated rates in the 21st century,
making it the largest single contributor to rising sea levels. Faster flow of outlet glaciers has …

Glacier terminus changes are one of the hallmarks of worldwide glacier change, and thus,
there is significant focus on the controls and limits to retreat in the literature. Here we use the …

In recent decades, tidewater glaciers in Northwest Greenland contributed significantly to sea
level rise but exhibited a complex spatial pattern of retreat. Here we use novel observations …

Accurate projections of the mass loss from the Greenland Ice Sheet (GrIS) require a
complete understanding of the ice‐dynamic response to climate forcings on seasonal and …

Greenland's outlet glaciers have been a leading source of mass loss and accompanying sea‐
level rise from the Greenland Ice Sheet (GrIS) over the last 25 years. The dynamic …

Abstract The Greenland Ice Sheet has lost mass at an accelerating rate over the last two
decades, but limits of early remote sensing restricted examination of localized change at an …

Recent observations indicate that many marine‐terminating glaciers in Greenland and
Antarctica are currently retreating and thinning, potentially due to long‐term trends in climate …

Characterizing sea ice changes over the Arctic can give proper insight into its extent in the
current context of climate change. Sea ice motion's effect on ice area is influenced by …

Over recent decades, the number of outlet glaciers terminating in lakes in Iceland has
increased in line with climate warming. The mass-balance changes of these lake …