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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Detalles Bibliográficos
Autores principales: Willeit, M., Ganopolski, A., Calov, R., Brovkin, V.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2019
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6447376/
https://www.ncbi.nlm.nih.gov/pubmed/30949580
http://dx.doi.org/10.1126/sciadv.aav7337

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6447376/
https://www.ncbi.nlm.nih.gov/pubmed/30949580
http://dx.doi.org/10.1126/sciadv.aav7337

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