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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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Bibliografiska uppgifter
I publikationen:Proc Natl Acad Sci U S A
Huvudupphovsmän: Boers, Niklas, Ghil, Michael, Rousseau, Denis-Didier
Materialtyp: Artigo
Språk:Inglês
Publicerad: National Academy of Sciences 2018
Ämnen:
Länkar: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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