Comment on "Long-term climate forcing by atmospheric oxygen concentrations".

Science

School of Earth and Ocean Sciences, University of Victoria, Victoria, British Columbia, Canada.

Published: July 2016

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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http://dx.doi.org/10.1126/science.aad6976DOI Listing

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