Suppressed basal melting in the eastern Thwaites Glacier grounding zone

Thwaites Glacier is one of the fastest-changing ice–ocean systems in Antarctica(1–3). Much of the ice sheet within the catchment of Thwaites Glacier is grounded below sea level on bedrock that deepens inland(4), making it susceptible to rapid and irreversible ice loss that could raise the global sea...

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Detalles Bibliográficos
Autores principales: Davis, Peter E. D., Nicholls, Keith W., Holland, David M., Schmidt, Britney E., Washam, Peter, Riverman, Kiya L., Arthern, Robert J., Vaňková, Irena, Eayrs, Clare, Smith, James A., Anker, Paul G. D., Mullen, Andrew D., Dichek, Daniel, Lawrence, Justin D., Meister, Matthew M., Clyne, Elisabeth, Basinski-Ferris, Aurora, Rignot, Eric, Queste, Bastien Y., Boehme, Lars, Heywood, Karen J., Anandakrishnan, Sridhar, Makinson, Keith
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/PMC9931584/
https://www.ncbi.nlm.nih.gov/pubmed/36792735
http://dx.doi.org/10.1038/s41586-022-05586-0

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9931584/
https://www.ncbi.nlm.nih.gov/pubmed/36792735
http://dx.doi.org/10.1038/s41586-022-05586-0

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