Cargando…
Massive subsurface ice formed by refreezing of ice-shelf melt ponds
Surface melt ponds form intermittently on several Antarctic ice shelves. Although implicated in ice-shelf break up, the consequences of such ponding for ice formation and ice-shelf structure have not been evaluated. Here we report the discovery of a massive subsurface ice layer, at least 16 km acros...
Autores principales: | Hubbard, Bryn, Luckman, Adrian, Ashmore, David W., Bevan, Suzanne, Kulessa, Bernd, Kuipers Munneke, Peter, Philippe, Morgane, Jansen, Daniela, Booth, Adam, Sevestre, Heidi, Tison, Jean-Louis, O'Leary, Martin, Rutt, Ian |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group
2016
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4906384/ https://www.ncbi.nlm.nih.gov/pubmed/27283778 http://dx.doi.org/10.1038/ncomms11897 |
Ejemplares similares
-
Marine ice regulates the future stability of a large Antarctic ice shelf
por: Kulessa, Bernd, et al.
Publicado: (2014) -
Seawater softening of suture zones inhibits fracture propagation in Antarctic ice shelves
por: Kulessa, Bernd, et al.
Publicado: (2019) -
Crevasse refreezing and signatures of retreat observed at Kamb Ice Stream grounding zone
por: Lawrence, J. D., et al.
Publicado: (2023) -
A tipping point in refreezing accelerates mass loss of Greenland's glaciers and ice caps
por: Noël, B., et al.
Publicado: (2017) -
Benthic microbial communities of coastal terrestrial and ice shelf Antarctic meltwater ponds
por: Archer, Stephen D. J., et al.
Publicado: (2015)