Onset and termination of Heinrich Stadial 4 and the underlying climate dynamics
Severe cooling at high northern latitudes, which marked the onset of Heinrich Stadial 4, was synchronous with changes in tropical monsoon systems and preceded Antarctic warming by around 300 years, according to a compilation of speleothem and ice core records.
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| Auteurs principaux: | , , , , , , , , , , , , , , , , , , , , , , , , |
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| Format: | article |
| Langue: | EN |
| Publié: |
Nature Portfolio
2021
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| Accès en ligne: | https://doaj.org/article/9bd939c9962f4a0dbe1b6386c48e4487 |
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