a new chronology for CO2 is established and synchronized with Greenland ice core records to study how high latitude climate change and the carbon cycle were linked during the last glacial period. Atmospheric CO2 rose several thousand years before abrupt warming in Greenland associated with Dansgaard...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.474.9736 2023-05-15T14:03:51+02:00 Jinho Ahn Edward J. Brook The Pennsylvania State University CiteSeerX Archives 2007 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.474.9736 http://www.science.oregonstate.edu/~brooke/Recent_Publications_files/Ahn and Brook_2007_1.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.474.9736 http://www.science.oregonstate.edu/~brooke/Recent_Publications_files/Ahn and Brook_2007_1.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.science.oregonstate.edu/~brooke/Recent_Publications_files/Ahn and Brook_2007_1.pdf text 2007 ftciteseerx 2016-01-08T07:31:42Z a new chronology for CO2 is established and synchronized with Greenland ice core records to study how high latitude climate change and the carbon cycle were linked during the last glacial period. Atmospheric CO2 rose several thousand years before abrupt warming in Greenland associated with Dansgaard-Oeschger events, 8, 12, 14, 17, four large warm events that follow Heinrich events. The CO2 rise terminated at the onset of Greenland warming for each of these events. Atmospheric CO2 is strongly correlated with the Antarctic isotopic temperature proxy with an average time lag of 720 ± 370 yr (mean ± 1s) during the time interval studied. The new data and chronology should provide a better target for models attempting to explain CO2 variability and abrupt climate Text Antarc* Antarctic Dansgaard-Oeschger events Greenland Greenland ice core ice core Unknown Antarctic Greenland The Antarctic |
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English |
description |
a new chronology for CO2 is established and synchronized with Greenland ice core records to study how high latitude climate change and the carbon cycle were linked during the last glacial period. Atmospheric CO2 rose several thousand years before abrupt warming in Greenland associated with Dansgaard-Oeschger events, 8, 12, 14, 17, four large warm events that follow Heinrich events. The CO2 rise terminated at the onset of Greenland warming for each of these events. Atmospheric CO2 is strongly correlated with the Antarctic isotopic temperature proxy with an average time lag of 720 ± 370 yr (mean ± 1s) during the time interval studied. The new data and chronology should provide a better target for models attempting to explain CO2 variability and abrupt climate |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Jinho Ahn Edward J. Brook |
spellingShingle |
Jinho Ahn Edward J. Brook |
author_facet |
Jinho Ahn Edward J. Brook |
author_sort |
Jinho Ahn |
publishDate |
2007 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.474.9736 http://www.science.oregonstate.edu/~brooke/Recent_Publications_files/Ahn and Brook_2007_1.pdf |
geographic |
Antarctic Greenland The Antarctic |
geographic_facet |
Antarctic Greenland The Antarctic |
genre |
Antarc* Antarctic Dansgaard-Oeschger events Greenland Greenland ice core ice core |
genre_facet |
Antarc* Antarctic Dansgaard-Oeschger events Greenland Greenland ice core ice core |
op_source |
http://www.science.oregonstate.edu/~brooke/Recent_Publications_files/Ahn and Brook_2007_1.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.474.9736 http://www.science.oregonstate.edu/~brooke/Recent_Publications_files/Ahn and Brook_2007_1.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766274708016201728 |