Greenland’s ice shelves have lost more than a third of their volume

Alert press CNRS
The Zachariæ Isstrøm glacier in 2016
The Zachariæ Isstrøm glacier in 2016, discharging several kilometre-long icebergs into the ocean. The melting of platforms in North Greenland could make a significant contribution to rising sea levels.
© Romain Millan
The largest floating ice shelves in the polar ice sheet have lost more than a third of their volume since 1978. In a study to be published on 7 November in Nature Communications, scientists from the Institut des géosciences de l’environnement (IGE) [1], alongside their Danish and American colleagues, have established that most of this thinning is due to the rise in surrounding ocean temperatures, which causes the glaciers’ floating extensions to melt. Until now, the glaciers in this region were considered to be stable, unlike more sensitive areas of the polar ice cap, which began to weaken in the mid-1980s.

Located in North Greenland, these ice shelves play an essential role in regulating the amount of ice discharged into the ocean by acting as huge frozen “dams”. Although Greenland is already responsible for 17% of the current rise in sea levels, any weakening of these barriers could lead to an increase in the amount of ice released, accelerating further rises in the water level.

These results were obtained using field observations, aerial photography and satellite data, combined with regional climate models.

En savoir +

► IGE Article Toward a complete extinction of the last ice shelves of the Greenland ice sheet


Reference

Rapid disintegration and weakening of ice shelves in North Greenland. R. Millan, et al. Nature Communications, le 7 novembre 2023. DOI: 10.1038/s41467-023-42198-2

Local scientifique contact

 Romain Millan, researcher CNRS at the Institut des géosciences de l’Environnement (IGE/OSUG)

This press alerte was initially published le CNRS.

Updated on 13 November 2023

[1CNRS Laboratory involve
Institut des géosciences de l’environnement ( IGE - OSUG)
Tutelles : CNRS / UGA / IRD / INRAE