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Sea level and global ice volumes from the Last Glacial Maximum to the Holocene
The major cause of sea-level change during ice ages is the exchange of water between ice and ocean and the planet’s dynamic response to the changing surface load. Inversion of ∼1,000 observations for the past 35,000 y from localities far from former ice margins has provided new constraints on the fl...
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| Autores principales: | , , , , |
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| Formato: | Artigo |
| Lenguaje: | Inglês |
| Publicado: |
National Academy of Sciences
2014
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| Materias: | |
| Acceso en línea: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4217469/ https://ncbi.nlm.nih.gov/pubmed/25313072 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1411762111 |
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