The retreat and acceleration of Greenland glaciers since the mid-1990s have been
attributed to the enhanced intrusion of warm Atlantic Waters (AW) into fjords, but this …

In combination, the breakaway of icebergs (calving) and submarine melting at marine-
terminating glaciers account for between one third and one half of the mass annually …

Over the past two decades, mass loss from the Greenland Ice Sheet (GrIS) has accelerated
and contributed to global sea level rise. This has been partly attributed to dynamic changes …

The mass loss of the Greenland Ice Sheet is nearly equally partitioned between a decrease
in surface mass balance from enhanced surface melt and an increase in ice dynamics from …

This chapter assesses the state of physical, biological and social knowledge concerning the
Arctic and Antarctic ocean and cryosphere, how they are affected by climate change, and …

We present a 1986 through March 2020 estimate of Greenland Ice Sheet ice discharge. Our
data include all discharging ice that flows faster than 100 m yr-1 and are generated through …

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 …

In the past two decades, the data volume of remote sensing imagery in the polar regions has
increased dramatically. The calving fronts of many Greenland glaciers have been …

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 …

During the last glacial period, the Laurentide Ice Sheet sporadically discharged huge
numbers of icebergs through the Hudson Strait into the North Atlantic Ocean, leaving behind …