Skip to main content

Thank you for visiting nature.com. You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in Internet Explorer). In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript.

Isotopic evidence of multiple controls on atmospheric oxidants over climate transitions

Nature volume 546, pages 133–136 (2017)Cite this article

Subjects

Abstract

The abundance of tropospheric oxidants, such as ozone (O3) and hydroxyl (OH) and peroxy radicals (HO2 + RO2), determines the lifetimes of reduced trace gases such as methane and the production of particulate matter important for climate and human health. The response of tropospheric oxidants to climate change is poorly constrained owing to large uncertainties in the degree to which processes that influence oxidants may change with climate1 and owing to a lack of palaeo-records with which to constrain levels of atmospheric oxidants during past climate transitions2. At present, it is thought that temperature-dependent emissions of tropospheric O3 precursors and water vapour abundance determine the climate response of oxidants, resulting in lower tropospheric O3 in cold climates while HOx (= OH + HO2 + RO2) remains relatively buffered3. Here we report observations of oxygen-17 excess of nitrate (a proxy for the relative abundance of atmospheric O3 and HOx) from a Greenland ice core over the most recent glacial–interglacial cycle and for two Dansgaard–Oeschger events. We find that tropospheric oxidants are sensitive to climate change with an increase in the O3/HOx ratio in cold climates, the opposite of current expectations. We hypothesize that the observed increase in O3/HOx in cold climates is driven by enhanced stratosphere-to-troposphere transport of O3, and that reactive halogen chemistry is also enhanced in cold climates. Reactive halogens influence the oxidative capacity of the troposphere directly as oxidants themselves and indirectly4 via their influence on O3 and HOx. The strength of stratosphere-to-troposphere transport is largely controlled by the Brewer–Dobson circulation5, which may be enhanced in colder climates owing to a stronger meridional gradient of sea surface temperatures6, with implications for the response of tropospheric oxidants7 and stratospheric thermal and mass balance8. These two processes may represent important, yet relatively unexplored, climate feedback mechanisms during major climate transitions.

This is a preview of subscription content, access via your institution

Access options

Rent or buy this article

Get just this article for as long as you need it

$39.95

Learn more

Prices may be subject to local taxes which are calculated during checkout

Figure 1: GISP2 ice-core record of Δ17O(NO3−).
Figure 2: Relationship between measured δ18O(H2O) and Δ17O(NO3−).
Figure 3: ICECAP model results of zonal mean tropospheric oxidants in the Holocene and glacial climates.

References

  1. Naik, V. et al. Preindustrial to present-day changes in tropospheric hydroxyl radical and methane lifetime from the Atmospheric Chemistry and Climate Model Intercomparison Project (ACCMIP). Atmos. Chem. Phys. 13, 5277–5298 (2013)

    Article  ADS  Google Scholar 

  2. Alexander, B. & Mickley, L. Paleo-perspectives on potential future changes in the oxidative capacity of the atmosphere due to climate change and anthropogenic emissions. Curr. Pollution Rep. 1, 57–69 (2015)

    Article  CAS  Google Scholar 

  3. Murray, L. T. et al. Factors controlling variability in the oxidative capacity of the troposphere since the Last Glacial Maximum. Atmos. Chem. Phys. 14, 3589–3622 (2014)

    Article  ADS  Google Scholar 

  4. Schmidt, J. A. et al. Modeling the observed tropospheric BrO background: importance of multiphase chemistry and implications for ozone, OH, and mercury. J. Geophys. Res. 121, 11819–11835 (2016)

    CAS  Google Scholar 

  5. Holton, J. R. et al. Stratosphere-troposphere exchange. Rev. Geophys. 33, 403–439 (1995)

    Article  ADS  Google Scholar 

  6. Rind, D., Lerner, J., McLinden, C. & Perlwitz, J. Stratospheric ozone during the Last Glacial Maximum. Geophys. Res. Lett. 36, L09712 (2009)

    ADS  Google Scholar 

  7. Hegglin, M. I. & Shepherd, T. G. Large climate-induced changes in ultraviolet index and stratosphere-to-troposphere ozone flux. Nat. Geosci. 2, 687–691 (2009)

    Article  ADS  CAS  Google Scholar 

  8. Butchart, N. The Brewer-Dobson circulation. Rev. Geophys. 52, 157–184 (2014)

    Article  ADS  Google Scholar 

  9. Alexander, B. et al. Quantifying atmospheric nitrate formation pathways based on a global model of the oxygen isotopic composition (Δ17O) of atmospheric nitrate. Atmos. Chem. Phys. 9, 5043–5056 (2009)

    Article  ADS  CAS  Google Scholar 

  10. Savarino, J. et al. Isotopic composition of atmospheric nitrate in a tropical marine boundary layer. Proc. Natl Acad. Sci. USA 110, 17668–17673 (2013)

    Article  ADS  CAS  Google Scholar 

  11. Morin, S., Savarino, J., Bekki, S., Gong, S. & Bottenheim, J. W. Signature of Arctic surface ozone depletion events in the isotope anomaly (Δ17O) of atmospheric nitrate. Atmos. Chem. Phys. 7, 1451–1469 (2007)

    Article  ADS  CAS  Google Scholar 

  12. Alley, R. B. Wally was right: predictive ability of the North Atlantic “Conveyor Belt” hypothesis for abrupt climate change. Annu. Rev. Earth Planet. Sci. 35, 241–272 (2007)

    Article  ADS  CAS  Google Scholar 

  13. Barrie, L. A., Bottenheim, J. W., Schnell, R. C., Crutzen, P. J. & Rasmussen, R. A. Ozone destruction and photochemical reactions at polar sunrise in the lower Arctic atmosphere. Nature 334, 138–141 (1988)

    Article  ADS  CAS  Google Scholar 

  14. Rind, D., Chandler, M., Lonergan, P. & Lerner, J. Climate change and the middle atmosphere. 5. Paleostratosphere in cold and warm climates. J. Geophys. Res. 106, 20195–20212 (2001)

    Article  ADS  Google Scholar 

  15. Lin, P. & Fu, Q. Changes in various branches of the Brewer–Dobson circulation from an ensemble of chemistry climate models. J. Geophys. Res. 118, 73–84 (2013)

    CAS  Google Scholar 

  16. Olsen, M. A., Schoeberl, M. R. & Nielsen, J. E. Response of stratospheric circulation and stratosphere-troposphere exchange to changing sea surface temperatures. J. Geophys. Res. 112, (2007)

  17. Sherwen, T., Evans, M. J., Carpenter, L. J., Schmidt, J. A. & Mickley, L. J. Halogen chemistry reduces tropospheric O3 radiative forcing. Atmos. Chem. Phys. 17, 1557–1569 (2017)

    Article  ADS  CAS  Google Scholar 

  18. Sprenger, M., Wernli, H. & Bourqui, M. Stratosphere–troposphere exchange and its relation to potential vorticity streamers and cutoffs near the extratropical tropopause. J. Atmos. Sci. 64, 1587–1602 (2007)

    Article  ADS  Google Scholar 

  19. Xie, B., Zhang, H., Wang, Z., Zhao, S. & Fu, Q. A modeling study of effective radiative forcing and climate response due to tropospheric ozone. Adv. Atmos. Sci. 33, 819–828 (2016)

    Article  CAS  Google Scholar 

  20. Knutti, R., Fluckiger, J., Stocker, T. F. & Timmermann, A. Strong hemispheric coupling of glacial climate through freshwater discharge and ocean circulation. Nature 430, 851–856 (2004)

    Article  ADS  CAS  Google Scholar 

  21. McManus, J. F., Francois, R., Gherardi, J. M., Keigwin, L. D. & Brown-Leger, S. Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes. Nature 428, 834–837 (2004)

    Article  ADS  CAS  Google Scholar 

  22. Persechino, A. et al. Decadal-timescale changes of the Atlantic overturning circulation and climate in a coupled climate model with a hybrid-coordinate ocean component. Clim. Dyn. 39, 1021–1042 (2012)

    Article  Google Scholar 

  23. Shepherd, T. G. & McLandress, C. A robust mechanism for strengthening of the Brewer–Dobson circulation in response to climate change: critical-layer control of subtropical wave breaking. J. Atmos. Sci. 68, 784–797 (2011)

    Article  ADS  Google Scholar 

  24. Miller, G. H. et al. Arctic amplification: can the past constrain the future? Quat. Sci. Rev. 29, 1779–1790 (2010)

    Article  ADS  Google Scholar 

  25. Butchart, N. et al. Simulations of anthropogenic change in the strength of the Brewer-Dobson circulation. Clim. Dyn. 27, 727–741 (2006)

    Article  Google Scholar 

  26. Holmes, C. D., Prather, M. J., Sovde, O. A. & Myhre, G. Future methane, hydroxyl, and their uncertainties: key climate and emission parameters for future predictions. Atmos. Chem. Phys. 13, 285–302 (2013)

    Article  ADS  Google Scholar 

  27. Allan, W., Struthers, H. & Lowe, D. C. Methane carbon isotope effects caused by atomic chlorine in the marine boundary layer: global model results compared with Southern Hemisphere measurements. J. Geophys. Res. 112, D04306 (2007)

    Article  ADS  Google Scholar 

  28. Brook, E. J., Sowers, T. & Orchardo, J. Rapid variations in atmospheric methane concentration during the past 110,000 years. Science 273, 1087–1091 (1996)

    Article  ADS  CAS  Google Scholar 

  29. Grootes, P. M. & Stuiver, M. Oxygen 18/16 variability in Greenland snow and ice with 10−3- to 105-year time resolution. J. Geophys. Res. 102, 26455–26470 (1997)

    Article  ADS  CAS  Google Scholar 

  30. CLIMAP. The surface of the ice-age Earth. Science 191, 1131–1137 (1976)

  31. Webb, R. S., Rind, D. H., Lehman, S. J., Healy, R. J. & Sigman, D. Influence of ocean heat transport on the climate of the Last Glacial Maximum. Nature 385, 695–699 (1997)

    Article  ADS  CAS  Google Scholar 

  32. Cuffey, K. M. & Clow, G. D. Temperature, accumulation, and ice sheet elevation in central Greenland through the last deglacial transition. J. Geophys. Res. 102, 26383–26396 (1997)

    Article  ADS  Google Scholar 

  33. Geng, L. et al. Analysis of oxygen-17 excess of nitrate and sulfate at sub-micromole levels using the pyrolysis method. Rapid Commun. Mass Spectrom. 27, 2411–2419 (2013)

    Article  CAS  Google Scholar 

  34. Geng, L. et al. On the origin of the occasional spring nitrate peak in Greenland snow. Atmos. Chem. Phys. 14, 13361–13376 (2014)

    Article  ADS  Google Scholar 

  35. Kaiser, J., Hastings, M. G., Houlton, B. Z., Rockmann, T. & Sigman, D. M. Triple oxygen isotope analysis of nitrate using the denitrifier method and thermal decomposition of N2O. Anal. Chem. 79, 599–607 (2007)

    Article  CAS  Google Scholar 

  36. Gupta, P., Noone, D., Galewsky, J., Sweeney, C. & Vaughn, B. H. Demonstration of high-precision continuous measurements of water vapor isotopologues in laboratory and remote field deployments using wavelength-scanned cavity ring-down spectroscopy (WS-CRDS) technology. Rapid Commun. Mass Spectrom. 23, 2534–2542 (2009)

    Article  ADS  CAS  Google Scholar 

  37. Kaplan, J. O., Folberth, G. & Hauglustaine, D. A. Role of methane and biogenic volatile organic compound sources in late glacial and Holocene fluctuations of atmospheric methane concentrations. Glob. Biogeochem. Cycles 20, GB2016 (2006)

    Article  ADS  Google Scholar 

  38. Pfeiffer, M., Spessa, A. & Kaplan, J. O. A model for global biomass burning in preindustrial time: LPJ-LMfire (v1.0). Geosci. Model Dev. 6, 643–685 (2013)

    Article  ADS  Google Scholar 

  39. Alexander, M. J. et al. Recent developments in gravity-wave effects in climate models and the global distribution of gravity-wave momentum flux from observations and models. Q. J. R. Meteorol. Soc. 136, 1103–1124 (2010)

    Google Scholar 

Download references

Acknowledgements

We acknowledge financial support from NSF awards AGS 1103163, PLR 1106317 and PLR 1244817 (to B.A.) and AGS 1102880 (to L.J.M. and L.T.M.). L.T.M. was also supported by the NASA Postdoctoral Program Fellowship administered by Oak Ridge Associated Universities (NNH06CC03B). Q.F. is supported by NASA Grant NNX13AN49G. P.L. is supported by NA14OAR4320106 from the National Oceanic and Atmospheric Administration, the US Department of Commerce. The statements, findings, conclusions, and recommendations are those of the author(s) and do not necessarily reflect the views of the National Oceanic and Atmospheric Administration, or the US Department of Commerce. We thank the National Ice Core Laboratory for providing the GISP2 ice-core samples, and the GISP2 team for ice-core drilling. We also thank our laboratory technician B. Vanden Heuvel for measurements of δ18O(H2O).

Author information

Authors and Affiliations

  1. Department of Atmospheric Sciences, University of Washington, Seattle, 98195, Washington, USA

    Lei Geng, Qiang Fu & Becky Alexander

  2. Institut des Géosciences de l’Environnement, Université Grenoble Alpes, Grenoble, 38508, France

    Lei Geng

  3. School of Earth and Space Sciences, University of Science and Technology of China, Hefei, 230026, Anhui, China

    Lei Geng

  4. Department of Earth and Environmental Sciences, University of Rochester, Rochester, New York, USA

    Lee T. Murray

  5. School of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts, USA

    Loretta J. Mickley

  6. Program in Atmospheric and Oceanic Sciences, Princeton University, Princeton, New Jersey, USA

    Pu Lin

  7. Department of Earth and Space Sciences, University of Washington, Seattle, 98195, Washington, USA

    Andrew J. Schauer

Authors
  1. Lei Geng
    View author publications

    You can also search for this author in PubMed Google Scholar

  2. Lee T. Murray
    View author publications

    You can also search for this author in PubMed Google Scholar

  3. Loretta J. Mickley
    View author publications

    You can also search for this author in PubMed Google Scholar

  4. Pu Lin
    View author publications

    You can also search for this author in PubMed Google Scholar

  5. Qiang Fu
    View author publications

    You can also search for this author in PubMed Google Scholar

  6. Andrew J. Schauer
    View author publications

    You can also search for this author in PubMed Google Scholar

  7. Becky Alexander
    View author publications

    You can also search for this author in PubMed Google Scholar

Contributions

B.A. conceived the study; L.G. performed the measurements, analysed the experimental and model data, proposed the hypotheses and wrote the manuscript with B.A.; L.T.M. constructed the ICECAP model under the supervision of L.J.M., and provided the model results; L.T.M., P.L. and Q.F. contributed to the hypotheses; A.J.S. assisted with the laboratory work. All authors contributed to the data interpretation and writing.

Corresponding author

Correspondence to Becky Alexander.

Ethics declarations

Competing interests

The authors declare no competing financial interests.

Additional information

Reviewer Information Nature thanks T. Roeckmann and the other anonymous reviewer(s) for their contribution to the peer review of this work.

Publisher's note: Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations

Supplementary information

Supplementary Information

This file contains a Supplementary Discussion, Supplementary Table 1 and Supplementary References. (PDF 908 kb)

PowerPoint slides

Source data

Rights and permissions

Reprints and Permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Geng, L., Murray, L., Mickley, L. et al. Isotopic evidence of multiple controls on atmospheric oxidants over climate transitions. Nature 546, 133–136 (2017). https://doi.org/10.1038/nature22340

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1038/nature22340

This article is cited by

Comments

By submitting a comment you agree to abide by our Terms and Community Guidelines. If you find something abusive or that does not comply with our terms or guidelines please flag it as inappropriate.

Search

Advanced search

Quick links

Nature Briefing

Sign up for the Nature Briefing newsletter — what matters in science, free to your inbox daily.

Get the most important science stories of the day, free in your inbox. Sign up for Nature Briefing