Synchronous Change of Atmospheric CO 2 and Antarctic Temperature During the Last Deglacial Warming-Reference-Cited by-同舟云学术

Synchronous Change of Atmospheric CO 2 and Antarctic Temperature During the Last Deglacial Warming

Published:2013-03 Issue:6123 Volume:339 Page:1060-1063
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Parrenin F.¹,Masson-Delmotte V.²,Köhler P.³,Raynaud D.¹,Paillard D.²,Schwander J.⁴,Barbante C.⁵⁶,Landais A.²,Wegner A.³,Jouzel J.²

Affiliation:

1. Laboratoire de Glaciologie et Géophysique de l'Environnement (CNRS/UJF), Grenoble, France.

2. Laboratoire des Sciences du Climat et de l'Environnement (CEA/CNRS/UVSQ-IPSL), Gif-sur-Yvette, France.

3. Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany.

4. Physics Institute, University of Bern, Bern, Switzerland.

5. Department of Environmental Sciences, University of Venice, Venice, Italy.

6. Institute for the Dynamics of Environmental Processes–CNR, University of Venice, Venice, Italy.

Abstract

No Leader to Follow Changes in the concentration of atmospheric CO 2 and surface air temperature are closely related. However, temperature can influence atmospheric CO 2 as well as be influenced by it. Studies of polar ice cores have concluded that temperature increases during periods of rapid warming have preceded increases in CO 2 by hundreds of years. Parrenin et al. (p. 1060 ; see the Perspective by

Brook

) present a revised age scale for the atmospheric component of Antarctic ice cores, based on the isotopic composition of the N 2 that they contain, and suggest that temperature and CO 2 changed synchronously over four intervals of rapid warming during the last deglaciation.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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