Increased warm water intrusions could cause mass loss in East Antarctica during the next 200 years

The East Antarctic Ice Sheet (EAIS) is currently surrounded by relatively cool water, but climatic shifts have the potential to increase basal melting via intrusions of warm modified Circumpolar Deep Water (mCDW) onto the continental shelf. Here we use an ice sheet model to show that under the curre...

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Detalles Bibliográficos
Autores principales: Jordan, James R., Miles, B. W. J., Gudmundsson, G. H., Jamieson, S. S. R., Jenkins, A., Stokes, C. R.
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/PMC10067810/
https://www.ncbi.nlm.nih.gov/pubmed/37005432
http://dx.doi.org/10.1038/s41467-023-37553-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10067810/
https://www.ncbi.nlm.nih.gov/pubmed/37005432
http://dx.doi.org/10.1038/s41467-023-37553-2

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