Cargando…
Ocean warming drives rapid dynamic activation of marine-terminating glacier on the west Antarctic Peninsula
Ice dynamic change is the primary cause of mass loss from the Antarctic Ice Sheet, thus it is important to understand the processes driving ice-ocean interactions and the timescale on which major change can occur. Here we use satellite observations to measure a rapid increase in speed and collapse o...
Autores principales: | Wallis, Benjamin J., Hogg, Anna E., Meredith, Michael P., Close, Romilly, Hardy, Dominic, McMillan, Malcolm, Wuite, Jan, Nagler, Thomas, Moffat, Carlos |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2023
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10684579/ https://www.ncbi.nlm.nih.gov/pubmed/38016938 http://dx.doi.org/10.1038/s41467-023-42970-4 |
Ejemplares similares
-
Shelf–ocean exchange and hydrography west of the Antarctic Peninsula: a review
por: Moffat, C., et al.
Publicado: (2018) -
Impact of marine processes on flow dynamics of northern Antarctic Peninsula outlet glaciers
por: Rott, Helmut, et al.
Publicado: (2020) -
Volcanically Triggered Ocean Warming Near the Antarctic Peninsula
por: Verona, L. S., et al.
Publicado: (2019) -
Rapid accelerations of Antarctic Peninsula outlet glaciers driven by surface melt
por: Tuckett, Peter A., et al.
Publicado: (2019) -
Coastal Bacterial Community Response to Glacier Melting in the Western Antarctic Peninsula
por: Alcamán-Arias, María Estrella, et al.
Publicado: (2021)