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 …

Glacier change is ubiquitous, but the fastest and largest magnitude changes occur in
glaciers that terminate in water. This includes the most rapidly retreating glaciers, and also …

Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and
accessible, it has established a reputation as a comprehensive and essential resource. In …

The recent marked retreat, thinning and acceleration of most of Greenland's outlet glaciers
south of 70∘ N has increased concerns over Greenland's contribution to future sea level …

We used time‐lapse imagery, seismic and audio recordings, iceberg and glacier velocities,
ocean wave measurements, and simple theoretical considerations to investigate the …

Tide gauges show that global sea level has risen about 7 inches during the 20th century,
and recent satellite data show that the rate of sea-level rise is accelerating. As Earth warms …

Mass loss from the Greenland ice sheet (GrIS) has increased over the last two decades in
response to changes in global climate, motivating the scientific community to question how …

Over the past quarter of a century the Arctic has warmed more than any other region on
Earth, causing a profound impact on the Greenland ice sheet (GrIS) and its contribution to …

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 …

Glacier ice discharge, which depends on ice velocity and terminus fluctuations, is a primary
component of Greenland Ice Sheet mass loss. Some research suggests that ice mélange …