Intrinsic processes drive variability in basal melting of the Totten Glacier Ice Shelf
Low frequency intrinsic ocean variability has an unknown impact on Antarctic ice shelves, yet can arise even in the absence of varying climate forcing. Here, the authors show that this variability significantly affects modelled basal melting under the Totten Ice Shelf, with implications for the attr...
Guardado en:
Autores principales: | David E. Gwyther, Terence J. O’Kane, Benjamin K. Galton-Fenzi, Didier P. Monselesan, Jamin S. Greenbaum |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2018
|
Materias: | |
Acceso en línea: | https://doaj.org/article/05ca0dcd86b94cb6bff783cae8a54d57 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Poleward eddy-induced warm water transport across a shelf break off Totten Ice Shelf, East Antarctica
por: Daisuke Hirano, et al.
Publicado: (2021) -
Massive subsurface ice formed by refreezing of ice-shelf melt ponds
por: Bryn Hubbard, et al.
Publicado: (2016) -
Thermohaline structure and circulation beneath the Langhovde Glacier ice shelf in East Antarctica
por: Masahiro Minowa, et al.
Publicado: (2021) -
A first constraint on basal melt-water production of the Greenland ice sheet
por: Nanna B. Karlsson, et al.
Publicado: (2021) -
Interplay of grounding-line dynamics and sub-shelf melting during retreat of the Bjørnøyrenna Ice Stream
por: Michele Petrini, et al.
Publicado: (2018)