The Transient Sea Level Response to External Forcing in CMIP6 Models

Earth is warming and sea levels are rising as land‐based ice is lost to melt, and oceans expand due to accumulation of heat. The pace of ice loss and steric expansion is linked to the intensity of warming. How much faster sea level will rise as climate warms is, however, highly uncertain and difficu...

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Detalles Bibliográficos
Autores principales: Grinsted, Aslak, Bamber, Jonathan, Bingham, Rory, Buzzard, Sammie, Nias, Isabel, Ng, Kelvin, Weeks, Jennifer
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2022
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9786795/
https://www.ncbi.nlm.nih.gov/pubmed/36582516
http://dx.doi.org/10.1029/2022EF002696

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9786795/
https://www.ncbi.nlm.nih.gov/pubmed/36582516
http://dx.doi.org/10.1029/2022EF002696

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