Global Warming Amplified by Reduced Sulphur Fluxes as a Result of Ocean Acidification

TitleGlobal Warming Amplified by Reduced Sulphur Fluxes as a Result of Ocean Acidification
Publication TypeJournal Article
Year of Publication2013
JournalNature Climate Change
Date Published08/2013
Abstract / Summary

Climate change and decreasing seawater pH (ocean acidification)1 have widely been considered as uncoupled consequences of the anthropogenic CO2 perturbation. Recently, experiments in seawater enclosures (mesocosms) showed that concentrations of dimethylsulphide (DMS), a biogenic sulphur compound, were markedly lower in a low-pH environment. Marine DMS emissions are the largest natural source of atmospheric sulphur and changes in their strength have the potential to alter the Earth’s radiation budget. Here we establish observational-based relationships between pH changes and DMS concentrations to estimate changes in future DMS emissions with Earth system model climate simulations. Global DMS emissions decrease by about 18(±3)% in 2100 compared with pre-industrial times as a result of the combined effects of ocean acidification and climate change. The reduced DMS emissions induce a significant additional radiative forcing, of which 83% is attributed to the impact of ocean acidification, tantamount to an equilibrium temperature response between 0.23 and 0.48 K. Our results indicate that ocean acidification has the potential to exacerbate anthropogenic warming through a mechanism that is not considered at present in projections of future climate change.

URLhttp://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1981.html#ref4
DOI10.1038/nclimate1981
Journal: Nature Climate Change
Year of Publication: 2013
Date Published: 08/2013

Climate change and decreasing seawater pH (ocean acidification)1 have widely been considered as uncoupled consequences of the anthropogenic CO2 perturbation. Recently, experiments in seawater enclosures (mesocosms) showed that concentrations of dimethylsulphide (DMS), a biogenic sulphur compound, were markedly lower in a low-pH environment. Marine DMS emissions are the largest natural source of atmospheric sulphur and changes in their strength have the potential to alter the Earth’s radiation budget. Here we establish observational-based relationships between pH changes and DMS concentrations to estimate changes in future DMS emissions with Earth system model climate simulations. Global DMS emissions decrease by about 18(±3)% in 2100 compared with pre-industrial times as a result of the combined effects of ocean acidification and climate change. The reduced DMS emissions induce a significant additional radiative forcing, of which 83% is attributed to the impact of ocean acidification, tantamount to an equilibrium temperature response between 0.23 and 0.48 K. Our results indicate that ocean acidification has the potential to exacerbate anthropogenic warming through a mechanism that is not considered at present in projections of future climate change.

DOI: 10.1038/nclimate1981
Citation:
Six, KD, S Kloster, T Ilyina, SD Archer, K Zhang, and E Maier-Reimer.  2013.  "Global Warming Amplified by Reduced Sulphur Fluxes as a Result of Ocean Acidification."  Nature Climate Change.  https://doi.org/10.1038/nclimate1981.