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...

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Detalles Bibliográficos
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:
Article
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

Internet

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

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