Younger Dryas cooling and the Greenland climate response to CO(2)

Greenland ice-core δ(18)O-temperature reconstructions suggest a dramatic cooling during the Younger Dryas (YD; 12.9–11.7 ka), with temperatures being as cold as the earlier Oldest Dryas (OD; 18.0–14.6 ka) despite an approximately 50 ppm rise in atmospheric CO(2). Such YD cooling implies a muted Gree...

Disgrifiad llawn

Wedi'i Gadw mewn:
Manylion Llyfryddiaeth
Prif Awduron: Liu, Zhengyu, Carlson, Anders E., He, Feng, Brady, Esther C., Otto-Bliesner, Bette L., Briegleb, Bruce P., Wehrenberg, Mark, Clark, Peter U., Wu, Shu, Cheng, Jun, Zhang, Jiaxu, Noone, David, Zhu, Jiang
Fformat: Artigo
Iaith:Inglês
Cyhoeddwyd: National Academy of Sciences 2012
Pynciau:
Physical Sciences
Mynediad Ar-lein:https://ncbi.nlm.nih.gov/pmc/articles/PMC3396542/
https://ncbi.nlm.nih.gov/pubmed/22733733
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1202183109
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