Atmos. Chem. Phys., 14, 1011-1024, 2014
www.atmos-chem-phys.net/14/1011/2014/
doi:10.5194/acp-14-1011-2014
© Author(s) 2014. This work is distributed
under the Creative Commons Attribution 3.0 License.
Influence of future climate and cropland expansion on isoprene emissions and tropospheric ozone
O. J. Squire1, A. T. Archibald1,2, N. L. Abraham1,2, D. J. Beerling3, C. N. Hewitt4, J. Lathière3,4,*, R. C. Pike1,**, P. J. Telford1,2, and J. A. Pyle1,2
1Centre for Atmospheric Science, Department of Chemistry, University of Cambridge, Cambridge, CB2 1EW, UK
2National Centre for Atmospheric Science, Department of Chemistry, University of Cambridge, Cambridge, CB2 1EW, UK
3Department of Animal and Plant Sciences, University of Sheffield, Sheffield, S10 2TN, UK
4Lancaster Environment Centre, Lancaster University, Lancaster, LA1 4YQ, UK
*now at: Laboratoire des Sciences du Climat et de l'Environnement, IPSL, UVSQ, CEA, CNRS, Gif-sur-Yvette, France
**now at: Draper Fisher Jurvetson, 2882 Sand Hill Road, Suite 150 Menlo Park, CA 94025, USA

Abstract. Over the 21st century, changes in CO2 levels, climate and land use are expected to alter the global distribution of vegetation, leading to changes in trace gas emissions from plants, including, importantly, the emissions of isoprene. This, combined with changes in anthropogenic emissions, has the potential to impact tropospheric ozone levels, which above a certain level are harmful to animals and vegetation. In this study we use a biogenic emissions model following the empirical parameterisation of the MEGAN model, with vegetation distributions calculated by the Sheffield Dynamic Global Vegetation Model (SDGVM) to explore a range of potential future (2095) changes in isoprene emissions caused by changes in climate (including natural land use changes), land use, and the inhibition of isoprene emissions by CO2. From the present-day (2000) value of 467 Tg C yr−1, we find that the combined impact of these factors could cause a net decrease in isoprene emissions of 259 Tg C yr−1 (55%) with individual contributions of +78 Tg C yr−1 (climate change), −190 Tg C yr−1 (land use) and −147 Tg C yr−1 (CO2 inhibition). Using these isoprene emissions and changes in anthropogenic emissions, a series of integrations is conducted with the UM-UKCA chemistry-climate model with the aim of examining changes in ozone over the 21st century. Globally, all combined future changes cause a decrease in the tropospheric ozone burden of 27 Tg (7%) from 379 Tg in the present-day. At the surface, decreases in ozone of 6–10 ppb are calculated over the oceans and developed northern hemispheric regions, due to reduced NOx transport by PAN and reductions in NOx emissions in these areas respectively. Increases of 4–6 ppb are calculated in the continental tropics due to cropland expansion in these regions, increased CO2 inhibition of isoprene emissions, and higher temperatures due to climate change. These effects outweigh the decreases in tropical ozone caused by increased tropical isoprene emissions with climate change. Our land use change scenario consists of cropland expansion, which is most pronounced in the tropics. The tropics are also where land use change causes the greatest increases in ozone. As such there is potential for increased crop exposure to harmful levels of ozone. However, we find that these ozone increases are still not large enough to raise ozone to such damaging levels.

Citation: Squire, O. J., Archibald, A. T., Abraham, N. L., Beerling, D. J., Hewitt, C. N., Lathière, J., Pike, R. C., Telford, P. J., and Pyle, J. A.: Influence of future climate and cropland expansion on isoprene emissions and tropospheric ozone, Atmos. Chem. Phys., 14, 1011-1024, doi:10.5194/acp-14-1011-2014, 2014.
 
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