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Filtering by: Publisher Mongolian Academy of Science Creator Carlson, Anders E.

Global climate evolution during the last deglaciation

Creator:

Clark, Peter U., Shakun, Jeremy D., Baker, Paul A., Bartlein, Patrick J., Brewer, Simon, Brook, Edward J., 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., and Williams, John W.

Abstract:

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 global warming, the decay of...

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Article

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; vCollege of Marine Science, University of South Florida, St. Petersburg, FL 33701; wSchool of Earth and
Geochemical proxies of North American freshwater routing during the Younger Dryas cold event

Creator:

Carlson, Anders E., Clark, Peter U., Haley, Brian A., Klinkhammer, Gary P., Simmons, Kathleen, Brook, Edward J., and Meissner, Katrin J.

Abstract:

The Younger Dryas cold interval represents a time when much of the Northern Hemisphere cooled from ≈12.9 to 11.5 kiloyears B.P. The cause of this event, which has long been viewed as the canonical example of abrupt climate change, was initially attributed to the routing of freshwater to the St....

Resource Type:

Article

Full Text:

/ 0611313104/DC1. © 2007 by The National Academy of Sciences of the USA 6556–6561 � PNAS � April 17, 2007

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Global climate evolution during the last deglaciation

Geochemical proxies of North American freshwater routing during the Younger Dryas cold event

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