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Ocean circulation, ice shelf, and sea ice interactions explain Dansgaard–Oeschger cycles

The last glacial interval experienced abrupt climatic changes called Dansgaard–Oeschger (DO) events. These events manifest themselves as rapid increases followed by slow decreases of oxygen isotope ratios in Greenland ice core records. Despite promising advances, a comprehensive theory of the DO cyc...

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Detalhes bibliográficos
Publicado no:Proc Natl Acad Sci U S A
Main Authors: Boers, Niklas, Ghil, Michael, Rousseau, Denis-Didier
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2018
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC6255200/
https://ncbi.nlm.nih.gov/pubmed/30385629
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1802573115
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