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 last decade witnessed an explosion in yearly number of publications on passive glacier
seismology. The seismic signals from a wide range of glacier‐related processes fill a broad …

Ocean-driven basal melting of Antarctica's floating ice shelves accounts for about half of
their mass loss in steady state, where gains in ice-shelf mass are balanced by losses. Ice …

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 …

The Greenland Ice Sheet holds 7.2 m of sea level equivalent and in recent decades, rising
temperatures have led to accelerated mass loss. Current ice margin recession is led by the …

Rates of ice mass loss at the calving margins of tidewater glaciers (frontal ablation rates) are
a key uncertainty in sea level rise projections. Measurements are difficult because mass lost …

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 …

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 …

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 …

Submarine melt can account for substantial mass loss at tidewater glacier termini. However,
the processes controlling submarine melt are poorly understood due to limited observations …