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Mid-Pleistocene transition in glacial cycles explained by declining CO(2) and regolith removal
Variations in Earth’s orbit pace the glacial-interglacial cycles of the Quaternary, but the mechanisms that transform regional and seasonal variations in solar insolation into glacial-interglacial cycles are still elusive. Here, we present transient simulations of coevolution of climate, ice sheets,...
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| Udgivet i: | Sci Adv |
|---|---|
| Main Authors: | , , , |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
American Association for the Advancement of Science
2019
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| Fag: | |
| Online adgang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6447376/ https://ncbi.nlm.nih.gov/pubmed/30949580 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.aav7337 |
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