Articles | Volume 17, issue 19
Atmos. Chem. Phys., 17, 12177–12196, 2017
https://doi.org/10.5194/acp-17-12177-2017
Atmos. Chem. Phys., 17, 12177–12196, 2017
https://doi.org/10.5194/acp-17-12177-2017
Research article
12 Oct 2017
Research article | 12 Oct 2017

Projected global ground-level ozone impacts on vegetation under different emission and climate scenarios

Pierre Sicard et al.

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Cited articles

Ainsworth, E. A., Yendrek, C. R., Sitch, S., Collins, W. J., and Emberson, L. D.: The effect of Tropospheric Ozone on net primary productivity and implications for climate change, Annu. Rev. Plant Biol., 63, 637–661, 2012.
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Anav, A., De Marco, A., Proietti, C., Alessandri, A., Dell'Aquila, A., Cionni, I., Friedlingstein, P., Khvorostyanov, D., Menut, L., Paoletti, E., Sicard, P., Sitch, S., and Vitale, M.: Comparing concentration-based (AOT40) and stomatal uptake (PODY) metrics for ozone risk assessment to European forests, Global Change Biol., 22, 1608–1627, https://doi.org/10.1111/gcb.13138, 2016.
Anav, A., Liu, Q., De Marco, A., Proietti, C., Savi, F., Paoletti, E., and Piao, S.: The role of plant phenology in stomatal ozone flux modelling, Glob, Change Biol., https://doi.org/10.1111/gcb.13823, in press, 2017.
Arbaugh, M. J. and Bytnerowicz, A.: Ambient ozone patterns and effects over the Sierra Nevada: synthesis and implications for future research, in: Ozone Air Pollution in the Sierra Nevada: Distribution and Effects on Forests, Developments in Environmental Science, vol. 2, edited by: Bytnerowicz, A., Arbaugh, M., Alonso, R., Elsevier, Amsterdam, 249–261, 2003.
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Short summary
A few issues about surface ozone, e.g. a better understanding of spatial changes and a better assessment of ozone impacts worldwide, are still challenging. To overcome these issues, this study assessed, for the first time, the spatial and temporal changes in the projected potential ozone impacts on carbon assimilation of vegetation at global scale, by comparing the ozone potential injury at present with that expected at the end of the 21st century from different global chemistry models.
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