Global climate evolution during the last deglaciation

Deciphering the evolution of global climate from the end of the Last Glacial Maximum approximately 19 ka to the early Holocene 11 ka presents an outstanding opportunity for understanding the transient response of Earth’s climate system to external and internal forcings. During this interval of globa...

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Bibliografiske detaljer
Main Authors: Clark, Peter U., Shakun, Jeremy D., Baker, Paul A., Bartlein, Patrick J., Brewer, Simon, Brook, Ed, Carlson, Anders E., Cheng, Hai, Kaufman, Darrell S., Liu, Zhengyu, Marchitto, Thomas M., Mix, Alan C., Morrill, Carrie, Otto-Bliesner, Bette L., Pahnke, Katharina, Russell, James M., Whitlock, Cathy, Adkins, Jess F., Blois, Jessica L., Clark, Jorie, Colman, Steven M., Curry, William B., Flower, Ben P., He, Feng, Johnson, Thomas C., Lynch-Stieglitz, Jean, Markgraf, Vera, McManus, Jerry, Mitrovica, Jerry X., Moreno, Patricio I., Williams, John W.
Format: Artigo
Sprog:Inglês
Udgivet: National Academy of Sciences 2012
Fag:
PNAS Plus
Online adgang:https://ncbi.nlm.nih.gov/pmc/articles/PMC3358890/
https://ncbi.nlm.nih.gov/pubmed/22331892
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1116619109
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