Ocean variability beneath Thwaites Eastern Ice Shelf driven by the Pine Island Bay Gyre strength

West Antarctic ice-shelf thinning is primarily caused by ocean-driven basal melting. Here we assess ocean variability below Thwaites Eastern Ice Shelf (TEIS) and reveal the importance of local ocean circulation and sea-ice. Measurements obtained from two sub-ice-shelf moorings, spanning January 2020...

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Detalles Bibliográficos
Autores principales: Dotto, Tiago S., Heywood, Karen J., Hall, Rob A., Scambos, Ted A., Zheng, Yixi, Nakayama, Yoshihiro, Hyogo, Shuntaro, Snow, Tasha, Wåhlin, Anna K., Wild, Christian, Truffer, Martin, Muto, Atsuhiro, Alley, Karen E., Boehme, Lars, Bortolotto, Guilherme A., Tyler, Scott W., Pettit, Erin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9772408/
https://www.ncbi.nlm.nih.gov/pubmed/36543787
http://dx.doi.org/10.1038/s41467-022-35499-5

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9772408/
https://www.ncbi.nlm.nih.gov/pubmed/36543787
http://dx.doi.org/10.1038/s41467-022-35499-5

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