Cargando…
Rapid Holocene thinning of an East Antarctic outlet glacier driven by marine ice sheet instability
Outlet glaciers grounded on a bed that deepens inland and extends below sea level are potentially vulnerable to ‘marine ice sheet instability'. This instability, which may lead to runaway ice loss, has been simulated in models, but its consequences have not been directly observed in geological...
Autores principales: | Jones, R. S., Mackintosh, A. N., Norton, K. P., Golledge, N. R., Fogwill, C. J., Kubik, P. W., Christl, M., Greenwood, S. L. |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Pub. Group
2015
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4674764/ https://www.ncbi.nlm.nih.gov/pubmed/26608558 http://dx.doi.org/10.1038/ncomms9910 |
Ejemplares similares
-
Holocene reconfiguration and readvance of the East Antarctic Ice Sheet
por: Greenwood, Sarah L., et al.
Publicado: (2018) -
Mid-Holocene pulse of thinning in the Weddell Sea sector of the West Antarctic ice sheet
por: Hein, Andrew S., et al.
Publicado: (2016) -
Complex motion of Greenland Ice Sheet outlet glaciers with basal temperate ice
por: Law, Robert, et al.
Publicado: (2023) -
West Antarctic Ice Sheet retreat driven by Holocene warm water incursions
por: Hillenbrand, Claus-Dieter, et al.
Publicado: (2017) -
Holocene melting of the West Antarctic Ice Sheet driven by tropical Pacific warming
por: Sproson, Adam D., et al.
Publicado: (2022)