A global overview of glacier advances and retreats (grouped by regions and by millennia)
for the Holocene is compiled from previous studies. The reconstructions of glacier …

Mass loss from the Greenland ice sheet quadrupled over the past two decades, contributing
a quarter of the observed global sea-level rise. Increased submarine melting is thought 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 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 …

Ocean tides are the main source of high‐frequency variability in the vertical and horizontal
motion of ice sheets near their marine margins. Floating ice shelves, which occupy about …

Mountain glaciers comprise a small and widely distributed fraction of the world's terrestrial
ice, yet their rapid losses presently drive a large percentage of the cryosphere's contribution …

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 …

The recent retreat and speedup of outlet glaciers, as well as enhanced surface melting
around the ice sheet margin, have increased Greenland's contribution to sea level rise to …

Rates of glacier mass loss in the northern Pacific coastal temperate rainforest (PCTR) are
among the highest on Earth, and changes in glacier volume and extent will affect the flow …

We show that subglacial freshwater discharge is the principal process driving high rates of
submarine melting at tidewater glaciers. This buoyant discharge draws in warm seawater …