Global warming amplified by reduced sulphur fluxes as a result of ocean acidification

Katharina D. Six (), Silvia Kloster, Tatiana Ilyina, Stephen D. Archer, Kai Zhang and Ernst Maier-Reimer ()
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Katharina D. Six: Max Planck Institute for Meteorology
Silvia Kloster: Max Planck Institute for Meteorology
Tatiana Ilyina: Max Planck Institute for Meteorology
Stephen D. Archer: Plymouth Marine Laboratory, The Hoe
Kai Zhang: Pacific Northwest National Laboratory
Ernst Maier-Reimer: Max Planck Institute for Meteorology

Nature Climate Change, 2013, vol. 3, issue 11, 975-978

Abstract: Using computer simulations, this study quantifies the potential effect of ocean acidification on marine biogenic sulphur emissions and the resulting feedback mechanisms on future climate. It emphasizes that a reduction of anthropogenic carbon dioxide emissions is not only necessary to limit the negative effects of ocean acidification on marine life, but also to avoid amplified climate warming due to changes in biogenic sulphur production.

Date: 2013
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DOI: 10.1038/nclimate1981

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