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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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| I publikationen: | Proc Natl Acad Sci U S A |
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| Huvudupphovsmän: | , , |
| Materialtyp: | Artigo |
| Språk: | Inglês |
| Publicerad: |
National Academy of Sciences
2018
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| 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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