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 …

The Greenland ice sheet is one of the largest contributors to global mean sea-level rise
today and is expected to continue to lose mass as the Arctic continues to warm. The two …

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 …

Greenland runoff, from ice mass loss and increasing rainfall, is increasing. That runoff, as
discharge, impacts the physical, chemical, and biological properties of the adjacent fjords …

Abstract Changes in ocean temperature and salinity are expected to be an important
determinant of the Greenland ice sheet's future sea level contribution. Yet, simulating the …

The effect of the North Atlantic Ocean on the Greenland Ice Sheet through submarine
melting of Greenland's tidewater glacier calving fronts is thought to be a key driver of …

The Greenland ice sheet has been one of the largest sources of sea-level rise since the
early 2000s. However, basal melt has not been included explicitly in assessments of ice …

Abstract The Greenland Ice Sheet (GrIS) faces accelerated melting under a warming climate.
This also affects the largest marine‐terminating outlet glacier of the Northeast Greenland Ice …

Over the past decade, Greenland has experienced several extreme melt events, the most
pronounced ones in the years 2010, 2012 and 2019. With progressing climate change, such …

Mass loss at the Greenland Ice Sheet is influenced by atmospheric processes controlling its
surface mass balance, and by submarine melt and calving where glaciers terminate in …