Sea ice breakup and marine melt of a retreating tidewater outlet glacier in northeast Greenland (81°N)
Abstract Rising temperatures in the Arctic cause accelerated mass loss from the Greenland Ice Sheet and reduced sea ice cover. Tidewater outlet glaciers represent direct connections between glaciers and the ocean where melt rates at the ice-ocean interface are influenced by ocean temperature and cir...
Enregistré dans:
| Auteurs principaux: | Jørgen Bendtsen, John Mortensen, Kunuk Lennert, Jens K. Ehn, Wieter Boone, Virginie Galindo, Yu-bin Hu, Igor A. Dmitrenko, Sergei A. Kirillov, Kristian K. Kjeldsen, Yngve Kristoffersen, David G. Barber, Søren Rysgaard |
|---|---|
| Format: | article |
| Langue: | EN |
| Publié: |
Nature Portfolio
2017
|
| Sujets: | |
| Accès en ligne: | https://doaj.org/article/47590520a4bb40d7a576d60fe250c65a |
| Tags: |
Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
|
Documents similaires
-
Complex Greenland outlet glacier flow captured
par: Andy Aschwanden, et autres
Publié: (2016) -
Centennial response of Greenland’s three largest outlet glaciers
par: Shfaqat A. Khan, et autres
Publié: (2020) -
Iceberg melting substantially modifies oceanic heat flux towards a major Greenlandic tidewater glacier
par: B. J. Davison, et autres
Publié: (2020) -
The Holocene retreat dynamics and stability of Petermann Glacier in northwest Greenland
par: Martin Jakobsson, et autres
Publié: (2018) -
Dynamic ice loss from the Greenland Ice Sheet driven by sustained glacier retreat
par: Michalea D. King, et autres
Publié: (2020)