Fast and slow components of interstadial warming in the North Atlantic during the last glacial
Interstadial North Atlantic warming during the last glacial period involved the operation of both fast and slow components of the coupled atmosphere–ocean–sea-ice system, according to analyses from the Portuguese Margin and climate model simulations.
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| Autores principales: | , , , , , , , , , , |
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| Formato: | article |
| Lenguaje: | EN |
| Publicado: |
Nature Portfolio
2020
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| Materias: | |
| Acceso en línea: | https://doaj.org/article/9bf04e66bc204733b65255d4e3dc8bcc |
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