Ice Core Records of Atmospheric CO 2 Around the Last Three Glacial Terminations

Author:

Fischer Hubertus1,Wahlen Martin1,Smith Jesse1,Mastroianni Derek1,Deck Bruce1

Affiliation:

1. Scripps Institution of Oceanography, Geosciences Research Division, University of California San Diego, La Jolla, CA 92093–0220, USA.

Abstract

Air trapped in bubbles in polar ice cores constitutes an archive for the reconstruction of the global carbon cycle and the relation between greenhouse gases and climate in the past. High-resolution records from Antarctic ice cores show that carbon dioxide concentrations increased by 80 to 100 parts per million by volume 600 ± 400 years after the warming of the last three deglaciations. Despite strongly decreasing temperatures, high carbon dioxide concentrations can be sustained for thousands of years during glaciations; the size of this phase lag is probably connected to the duration of the preceding warm period, which controls the change in land ice coverage and the buildup of the terrestrial biosphere.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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4. . Recent investigations in central Greenland have reported an in situ production of CO 2 in the ice possibly related to carbonate or organic species reactions (or both) and have strongly compromised the validity of the determined CO 2 concentrations. However Antarctic ice cores are (if at all) much less affected by this effect because of the very low abundance of reactive carbon species dissolved in Antarctic ice.

5. Interannual extremes in the rate of rise of atmospheric carbon dioxide since 1980

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