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Comment on "Long-term climate forcing by atmospheric oxygen concentrations"
1School of Earth and Ocean Sciences, University of Victoria, Victoria, British Columbia, Canada.
Abstract:
Poulsen et al (Reports, 12 June 2015, p. 1238) argued that lower atmospheric oxygen levels during the Phanerozoic would have given a warmer climate. However, radiative and atmospheric structure changes under lower pressure both cause cooling, making their result unusual in that a hierarchy of models gives opposing results. Scrutiny of how radiative and cloud processes were represented, and a mechanistic explanation of the results, are required.
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