- Wood, Michael;
- Rignot, Eric;
- Fenty, Ian;
- An, Lu;
- Bjørk, Anders;
- van den Broeke, Michiel;
- Cai, Cilan;
- Kane, Emily;
- Menemenlis, Dimitris;
- Millan, Romain;
- Morlighem, Mathieu;
- Mouginot, Jeremie;
- Noël, Brice;
- Scheuchl, Bernd;
- Velicogna, Isabella;
- Willis, Josh K;
- Zhang, Hong
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 assertion has not been quantitatively tested on a Greenland-wide basis or included in models. Here, we investigate how AW influenced retreat at 226 marine-terminating glaciers using ocean modeling, remote sensing, and in situ observations. We identify 74 glaciers in deep fjords with AW controlling 49% of the mass loss that retreated when warming increased undercutting by 48%. Conversely, 27 glaciers calving on shallow ridges and 24 in cold, shallow waters retreated little, contributing 15% of the loss, while 10 glaciers retreated substantially following the collapse of several ice shelves. The retreat mechanisms remain undiagnosed at 87 glaciers without ocean and bathymetry data, which controlled 19% of the loss. Ice sheet projections that exclude ocean-induced undercutting may underestimate mass loss by at least a factor of 2.