Pathways and modification of warm water flowing beneath Thwaites Ice Shelf, West Antarctica

Thwaites Glacier is the most rapidly changing outlet of the West Antarctic Ice Sheet and adds large uncertainty to 21st century sea-level rise predictions. Here, we present the first direct observations of ocean temperature, salinity, and oxygen beneath Thwaites Ice Shelf front, collected by an auto...

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Detalles Bibliográficos
Autores principales: Wåhlin, A. K., Graham, A. G. C., Hogan, K. A., Queste, B. Y., Boehme, L., Larter, R. D, Pettit, E. C., Wellner, J., Heywood, K. J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2021
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8034858/
https://www.ncbi.nlm.nih.gov/pubmed/33837074
http://dx.doi.org/10.1126/sciadv.abd7254

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8034858/
https://www.ncbi.nlm.nih.gov/pubmed/33837074
http://dx.doi.org/10.1126/sciadv.abd7254

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