Total isostatic response to the complete unloading of the Greenland and Antarctic Ice Sheets

The land surface beneath the Greenland and Antarctic Ice Sheets is isostatically suppressed by the mass of the overlying ice. Accurate computation of the land elevation in the absence of ice is important when considering, for example, regional geodynamics, geomorphology, and ice sheet behaviour. Her...

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Detalles Bibliográficos
Autores principales: Paxman, Guy J. G., Austermann, Jacqueline, Hollyday, Andrew
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/PMC9259639/
https://www.ncbi.nlm.nih.gov/pubmed/35794143
http://dx.doi.org/10.1038/s41598-022-15440-y

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9259639/
https://www.ncbi.nlm.nih.gov/pubmed/35794143
http://dx.doi.org/10.1038/s41598-022-15440-y

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