Abstract Predicting Greenland Ice Sheet mass loss due to ice dynamics requires a complete
understanding of spatiotemporal velocity fluctuations and related control mechanisms. We …

The freshwater budget of the Arctic and sub‐polar North Atlantic Oceans has been changing
due, primarily, to increased river runoff, declining sea ice and enhanced melting of Arctic …

Although the global environmental impact of Laurentide Ice-Sheet destabilizations on glacial
climate during Heinrich Events is well-documented, the mechanism driving these ice-sheet …

For decades oceanographers have understood the Atlantic meridional overturning
circulation (AMOC) to be primarily driven by changes in the production of deep-water …

Abstract The Northeast Greenland shelf (NEGS) is a recipient of Polar Water (PW) from the
Arctic Ocean, Greenland Ice Sheet melt, and Atlantic Water (AW). Here, we compile …

Jakobshavn Isbrae has been the single largest source of mass loss from the Greenland Ice
Sheet over the last 20 years. During that time, it has been retreating, accelerating and …

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 ocean plays an important role in modulating the mass balance of the polar ice sheets by
interacting with the ice shelves in Antarctica and with the marine-terminating outlet glaciers …

The following graphics are supplemental to Chapter 2 (Global Climate). In most cases, a
particular graphic is analagous to one provided in the chapter, but employs an alternate …

Rapid mass loss from the Greenland Ice Sheet has sparked interest in its glacial fjords for
two main reasons: Increased submarine melting of glaciers terminating in fjords is a …