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.

  • Progress Article
  • Published:

Maximum efficiency in the hydroxyl-radical-based self-cleansing of the troposphere

Abstract

The removal of trace gases from the troposphere is, in most cases, initialized by reactions with hydroxyl radicals, and the products of these reactions are eventually deposited on the Earth's surface. The concentration of these hydroxyl radicals is therefore a measure of atmospheric self-cleansing. In theory, hydroxyl-radical concentrations can be enhanced by the recycling of some of the reaction products. The only known efficient recycling process involves nitrogen oxide and leads to production of ozone, yet observations in regions with high hydrocarbon and low nitrogen oxide concentrations show substantially elevated hydroxyl-radical concentrations, up to ten times higher than expected. If we normalize observed hydroxyl-radical concentrations to the maximum achievable in model calculations with variable nitrogen oxide concentrations, this photochemical coordinate system uncovers a common feature in almost all of these observations: even in the presence of inadequate amounts of nitrogen oxides, hydroxyl-radical concentrations are enhanced to the theoretical maximum obtainable at very much higher nitrogen oxide concentrations. This means that this important part of the self-cleansing capability of the atmosphere is working at maximum efficiency even in regions with a high burden of biogenic hydrocarbons and low nitrogen oxide concentration. Since these processes do not involve nitrogen oxides, tropospheric ozone production is greatly reduced compared with the expectation from current theory.

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

Access options

Buy this article

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

Figure 1: Simplified illustration of tropospheric OH chemistry.
Figure 2: Correlations between OH and j(O1D).
Figure 3: Calculated OH–NO2 dependence.
Figure 4: Comparison of observed and calculated OH.
Figure 5: Conceptual dependence of OH on NO2.

Similar content being viewed by others

References

  1. Levy, H. II Normal atmosphere: Large radical and formaldehyde concentrations. Science 173, 141–143 (1971).

    Article  Google Scholar 

  2. Ehhalt, D. H. Photooxidation of trace gases in the troposphere. Phys. Chem. Chem. Phys. 1, 5401–5408 (1999).

    Article  Google Scholar 

  3. Liu, S. C. et al. Ozone production in the rural troposphere and the implications for regional and global ozone distributions. J. Geophys. Res. 92, 4191–4207 (1987).

    Article  Google Scholar 

  4. Ehhalt, D. H. & Rohrer, F. Dependence of the OH concentration on solar UV. J. Geophys. Res. 105, 3565–3571 (2000).

    Article  Google Scholar 

  5. Brauers, T., Hausmann, M., Bister, A., Kraus, A. & Dorn, H. P. OH radicals in the boundary layer of the Atlantic Ocean: 1. Measurements by long-path laser absorption spectroscopy. J. Geophys. Res. 106, 7399–7414 (2001).

    Article  Google Scholar 

  6. Whalley, L. K. et al. The chemistry of OH and HO2 radicals in the boundary layer over the tropical Atlantic Ocean. Atmos. Chem. Phys. 10, 1555–1576 (2010).

    Article  Google Scholar 

  7. Mao, J. Q. et al. Atmospheric oxidation capacity in the summer of Houston 2006: Comparison with summer measurements in other metropolitan studies. Atmos. Environ. 44, 4107–4115 (2009).

    Article  Google Scholar 

  8. Dusanter, S. et al. Measurements of OH and HO2 concentrations during the MCMA-2006 field campaign — Part 2: Model comparison and radical budget. Atmos. Chem. Phys. 9, 6655–6675 (2009).

    Article  Google Scholar 

  9. Kanaya, Y. et al. Urban photochemistry in central Tokyo: 1. Observed and modeled OH and HO2 radical concentrations during the winter and summer of 2004. J. Geophys. Res. 112, D21312 (2007).

    Article  Google Scholar 

  10. Ren, X. R. et al. OH and HO2 chemistry in the urban atmosphere of New York City. Atmos. Environ. 37, 3639–3651 (2003).

    Article  Google Scholar 

  11. Tan, D. et al. HOx budgets in a deciduous forest: Results from the PROPHET summer 1998 campaign. J. Geophys. Res. 106, 24407–24427 (2001).

    Article  Google Scholar 

  12. Lelieveld, J. et al. Atmospheric oxidation capacity sustained by a tropical forest. Nature 452, 737–740 (2008).

    Article  Google Scholar 

  13. Hofzumahaus, A. et al. Amplified trace gas removal in the troposphere. Science 324, 1702–1704 (2009).

    Article  Google Scholar 

  14. Whalley, L. K. et al. Quantifying the magnitude of a missing hydroxyl radical source in a tropical rainforest. Atmos. Chem. Phys. 11, 7223–7233 (2011).

    Article  Google Scholar 

  15. Lu, K. D. et al. Missing OH source in a suburban environment near Beijing: observed and modelled OH and HO2 concentrations in summer 2006. Atmos. Chem. Phys. 13, 1057–1080 (2013).

    Article  Google Scholar 

  16. Archibald, A. T. et al. Impacts of HOx regeneration and recycling in the oxidation of isoprene: Consequences for the composition of past, present and future atmospheres. Geophys. Res. Lett. 38, 6655–6675 (2011).

    Article  Google Scholar 

  17. Peeters, J. & Müller, J-F. HOx radical regeneration in isoprene oxidation via peroxy radical isomerisations. II: experimental evidence and global impact. Phys. Chem. Chem. Phys. 12, 14227–14235 (2010).

    Article  Google Scholar 

  18. Taraborrelli, D. et al. Hydroxyl radical buffered by isoprene oxidation. Nature Geosci. 5, 190–193 (2012).

    Article  Google Scholar 

  19. Crounse, J. D., Paulot, F., Kjaergaard, H. G. & Wennberg, P. O. Peroxy radical isomerization in the oxidation of isoprene. Phys. Chem. Chem. Phys. 13, 13607–13613 (2011).

    Article  Google Scholar 

  20. Fuchs, H. et al. Experimental evidence for efficient hydroxyl radical regeneration in isoprene oxidation. Nature Geosci. 6, 1023–1026 (2013).

    Article  Google Scholar 

  21. Lu, K. D. et al. Observation and modelling of OH and HO2 concentrations in the Pearl River Delta 2006: a missing OH source in a VOC rich atmosphere. Atmos. Chem. Phys. 12, 1541–1569 (2012).

    Article  Google Scholar 

  22. Rohrer, F. & Berresheim, H. Strong correlation between levels of tropospheric hydroxyl radicals and solar ultraviolet radiation. Nature 442, 184–187 (2006).

    Article  Google Scholar 

  23. Eisele, F. L. et al. Understanding the production and interconversion of the hydroxyl radical during the Tropospheric OH Photochemistry Experiment. J. Geophys. Res. 102, 6457–6465 (1997).

    Article  Google Scholar 

  24. Mao, J. et al. Insights into hydroxyl measurements and atmospheric oxidation in a California forest. Atmos. Chem. Phys. 12, 8009–8020 (2012).

    Article  Google Scholar 

  25. Holland, F., Hofzumahaus, A., Schäfer, J., Kraus, A. & Pätz, H. W. Measurements of OH and HO2 radical concentrations and photolysis frequencies during BERLIOZ. J. Geophys. Res. 108, 8246 (2003).

    Article  Google Scholar 

  26. Peeters, J., Nguyenz, T. L. & Vereecken, L. HOx radical regeneration in the oxidation of isoprene. Phys. Chem. Chem. Phys. 11, 5935–5939 (2009).

    Article  Google Scholar 

  27. Kubistin, D. et al. Hydroxyl radicals in the tropical troposphere over the Suriname rainforest: comparison of measurements with the box model MECCA. Atmos. Chem. Phys. 10, 9705–9728 (2010).

    Article  Google Scholar 

  28. Tan, D. et al. HOx budgets in a deciduous forest: Results from the PROPHET summer 1998 campaign. J. Geophys. Res. 106, 24407–24427 (2001).

    Article  Google Scholar 

Download references

Acknowledgements

Discussions with D. H. Ehhalt, D. Klemp and D. Mihelcic are gratefully acknowledged. This work was supported by the National Natural Science Foundation of China (21190052 and 41121004) and the Strategic Priority Research Program of the Chinese Academy of Sciences (XDB05010500). The research was also supported by the Collaborative Innovation Center for Regional Environmental Quality. Our colleague Theo Brauers sadly passed away on 21 February 2014. We would like to take this opportunity to express our sincere appreciation for his excellent work.

Author information

Authors and Affiliations

Authors

Contributions

F.R. and K.L. contributed equally to this work. All other authors also contributed extensively to the work presented in this paper.

Corresponding authors

Correspondence to Franz Rohrer or Yuanhang Zhang.

Ethics declarations

Competing interests

The authors declare no competing financial interests.

Supplementary information

Supplementary Information

Supplementary Information (PDF 4170 kb)

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Rohrer, F., Lu, K., Hofzumahaus, A. et al. Maximum efficiency in the hydroxyl-radical-based self-cleansing of the troposphere. Nature Geosci 7, 559–563 (2014). https://doi.org/10.1038/ngeo2199

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1038/ngeo2199

This article is cited by

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