Abstract The Greenland Ice Sheet is losing mass at accelerated rates in the 21st century,
making it the largest single contributor to rising sea levels. Faster flow of outlet glaciers has …

We reconstruct the mass balance of the Greenland Ice Sheet using a comprehensive survey
of thickness, surface elevation, velocity, and surface mass balance (SMB) of 260 glaciers …

Observations taken over the last few decades indicate that dramatic changes are occurring
in the Arctic‐Boreal Zone (ABZ), which are having significant impacts on ABZ inhabitants …

Glaciers distinct from the Greenland and Antarctic ice sheets cover an area of approximately
706,000 square kilometres globally, with an estimated total volume of 170,000 cubic …

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 …

Abstract In the Northern Hemisphere, an insolation driven Early to Middle Holocene Thermal
Maximum was followed by a Neoglacial cooling that culminated during the Little Ice Age …

Modern game engines like Unity allow users to create realistic 3D environments containing
terrains as well as natural and artificial objects easily and swiftly. In addition, recent …

Over the past two decades, ice loss from the Greenland ice sheet (GrIS) has increased
owing to enhanced surface melting and ice discharge to the ocean,,,–. Whether continuing …

Nearly every glacier in Greenland has thinned or retreated over the past few decades,,–,
leading to glacier acceleration, increased rates of sea-level rise and climate impacts around …

In recent decades, tidewater glaciers in Northwest Greenland contributed significantly to sea
level rise but exhibited a complex spatial pattern of retreat. Here we use novel observations …