Letter | Published:

Detecting regional anthropogenic trends in ocean acidification against natural variability

Nature Climate Change volume 2, pages 167171 (2012) | Download Citation

Abstract

Since the beginning of the Industrial Revolution humans have released 500 billion metric tons of carbon to the atmosphere through fossil-fuel burning, cement production and land-use changes1,2. About 30% has been taken up by the oceans3. The oceanic uptake of carbon dioxide leads to changes in marine carbonate chemistry resulting in a decrease of seawater pH and carbonate ion concentration, commonly referred to as ocean acidification. Ocean acidification is considered a major threat to calcifying organisms4,5,6. Detecting its magnitude and impacts on regional scales requires accurate knowledge of the level of natural variability of surface ocean carbonate ion concentrations on seasonal to annual timescales and beyond. Ocean observations are severely limited with respect to providing reliable estimates of the signal-to-noise ratio of human-induced trends in carbonate chemistry against natural factors. Using three Earth system models we show that the current anthropogenic trend in ocean acidification already exceeds the level of natural variability by up to 30 times on regional scales. Furthermore, it is demonstrated that the current rates of ocean acidification at monitoring sites in the Atlantic and Pacific oceans exceed those experienced during the last glacial termination by two orders of magnitude.

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Acknowledgements

This study was funded by The Nature Conservancy (www.nature.org) and National Science Foundation (NSF) grant #0902133. AT is supported by the Japan Agency for Marine-Earth Science and Technology (JAMSTEC) through its sponsorship of the International Pacific Research Center and NSF grant #0902551. We thank S. Lorenz for conducting the MPI-ESM experiments. This is International Pacific Research Center contribution number 829.

Author information

Affiliations

  1. International Pacific Research Center (IPRC), SOEST, University of Hawai’i, Honolulu, Hawaii 96822, USA

    • T. Friedrich
    • , A. Timmermann
    •  & M. Heinemann
  2. Research Institute for Global Change, Japan Agency for Marine Science and Technology, Yokohama 236-0001, Japan

    • A. Abe-Ouchi
    •  & M. O. Chikamoto
  3. Bermuda Institute of Ocean Sciences, St George’s, GE 01, Bermuda

    • N. R. Bates
  4. Department of Oceanography, University of Hawai’i, Honolulu, Hawaii 96822, USA

    • M. J. Church
  5. Department of Land Resources and Environmental Sciences, Montana State University, Bozeman, Montana 59717, USA

    • J. E. Dore
  6. NOAA AOML, Cooperative Institute of Marine and Atmospheric Studies, Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida 33149, USA

    • D. K. Gledhill
  7. Departamento de Química, Facultad de Ciencias del Mar, Universidad de Las Palmas de Gran Canaria, Las Palmas de Gran Canaria 35.017, Spain

    • M. González-Dávila
    •  & J. M. Santana-Casiano
  8. Max Planck Institute for Meteorology, Hamburg 20146, Germany

    • T. Ilyina
    •  & J. H. Jungclaus
  9. The Nature Conservancy, Hawai’i Field Office, Honolulu, Hawaii 96817, USA

    • E. McLeod
  10. Département Astrophysique, Géophysique et Océanographie, Université de Liège, Liège B-4000, Belgium

    • A. Mouchet

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Contributions

The paper was written by T.F. and A.T. Data analysis and interpretation were carried out by T.F., A.T., M.H., D.K.G., N.R.B., M.J.C., J.E.D., M.G-D., J.M.S-C., T.I., J.H.J., M.O.C., E.M. and A.M. Observational data were provided by N.R.B., M.J.C., J.E.D., M.G-D. and J.M.S-C. Data for the Caribbean region were calculated by D.K.G. Last Glacial Maximum modelling data were provided by T.F., M.O.C., A.A-O. and A.M.

Competing interests

The authors declare no competing financial interests.

Corresponding authors

Correspondence to T. Friedrich or A. Timmermann.

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DOI

https://doi.org/10.1038/nclimate1372

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