Cargando…
A continuous pathway for fresh water along the East Greenland shelf
Export from the Arctic and meltwater from the Greenland Ice Sheet together form a southward-flowing coastal current along the East Greenland shelf. This current transports enough fresh water to substantially alter the large-scale circulation of the North Atlantic, yet the coastal current’s origin an...
Autores principales: | Foukal, Nicholas P., Gelderloos, Renske, Pickart, Robert S. |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
American Association for the Advancement of Science
2020
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7577721/ https://www.ncbi.nlm.nih.gov/pubmed/33087349 http://dx.doi.org/10.1126/sciadv.abc4254 |
Ejemplares similares
-
Vertical redistribution of principle water masses on the Northeast Greenland Shelf
por: Gjelstrup, Caroline V. B., et al.
Publicado: (2022) -
Ocean convection linked to the recent ice edge retreat along east Greenland
por: Våge, Kjetil, et al.
Publicado: (2018) -
Vegetation phenology gradients along the west and east coasts of Greenland from 2001 to 2015
por: Karami, Mojtaba, et al.
Publicado: (2017) -
On-shelf circulation of warm water toward the Totten Ice Shelf in East Antarctica
por: Hirano, Daisuke, et al.
Publicado: (2023) -
Only 5 southern Greenland shelf edge glaciations since the early Pliocene
por: Nielsen, Tove, et al.
Publicado: (2013)