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Title:
Vostok ice core - Climatic response to CO2 and orbital forcing changes over the last climatic cycle
Authors:
Genthon, C.; Jouzel, J.; Barnola, J. M.; Raynaud, D.; Lorius, C.
Affiliation:
AA(CEA, Laboratoire de Geochimie Isotopique, Gif-sur-Yvette, France), AB(CEA, Laboratoire de Geochimie Isotopique, Gif-sur-Yvette, France), AC(CNRS, Laboratoire de Glaciologie et de Geophysique de l'Environnement, Saint-Martin-d'Heres, France), AD(CNRS, Laboratoire de Glaciologie et de Geophysique de l'Environnement, Saint-Martin-d'Heres, France), AE(CNRS, Laboratoire de Glaciologie et de Geophysique de l'Environnement, Saint-Martin-d'Heres, France)
Publication:
Nature (ISSN 0028-0836), vol. 329, Oct. 1, 1987, p. 414-418. Research supported by the Programme National d'Etudes de la Dynamique du Climat and CEC. (Nature Homepage)
Publication Date:
10/1987
Category:
Geophysics
Origin:
STI
NASA/STI Keywords:
Antarctic Regions, Carbon Dioxide, Core Sampling, Ice Environments, Paleoclimatology, Atmospheric Composition, Atmospheric Models, Atmospheric Temperature, Orbital Elements
DOI:
10.1038/329414a0
Bibliographic Code:
1987Natur.329..414G

Abstract

Vostok climate and CO2 records suggest that CO2 changes have had an important climatic role during the late Pleistocene in amplifying the relatively weak orbital forcing. The existence of the 100-kyr cycle and the synchronism between Northern and Southern Hemisphere climates may have their origin in the large glacial-interglacial CO2 changes.
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