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Biogeosciences An interactive open-access journal of the European Geosciences Union
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
Research article
15 Dec 2017
Review status
This discussion paper is a preprint. It is a manuscript under review for the journal Biogeosciences (BG).
Recent past (1979–2014) and future (2070–2099) isoprene fluxes over Europe simulated with the MEGAN-MOHYCAN model
Maite Bauwens1, Trissevgeni Stavrakou1, Jean-François Müller1, Bert Van Schaeybroeck2, Lesley De Cruz2, Rozemien De Troch2, Olivier Giot2,3, Rafiq Hamdi2, Piet Termonia2, Quentin Laffineur2, Crist Amelynck1, Niels Schoon1, Bernard Heinesch4, Thomas Holst5, Almut Arneth6, Reinhart Ceulemans3, Arturo Sanchez-Lorenzo7, and Alex Guenther8 1Royal Belgian Institute for Space Aeronomy, Avenue Circulaire 3, Brussels, Belgium
2Royal Meteorological Institute, Avenue Circulaire 3, Brussels, Belgium
3Centre of Excellence PLECO (Plant and Vegetation Ecology), Department of Biology, University of Antwerp, 2610Wilrijk, Belgium
4Gembloux Agro-Bio Tech, University of Liège, Unité de Physique des Biosystèmes, Avenue de la Faculté d'Agronomie 8, 5030 Gembloux, Belgium
5Department of Physical Geography and Ecosystems Analysis, Lund University, Sweden
6Karlsruhe Institute of Technology, Institute of Meteorology and Climate Research, Atmospheric Environmental Research (IMK-IFU), Garmisch-Partenkirchen, Germany
7Pyrenean institute of Ecology (IPE), Spanish National Research Council, Zaragoza, Spain
8Department of Earth System Science, University of California, Irvine, California 92697, USA
Abstract. Isoprene is a highly reactive volatile organic compound emitted by vegetation, known to be a precursor of secondary organic aerosol and to enhance tropospheric ozone formation under polluted conditions. Isoprene emissions respond strongly to changes in meteorological parameters such as temperature and solar radiation; in addition, the increasing CO2 concentration has a dual effect, as it causes both a direct emission inhibition as well as an increase in biomass through fertilization. In this study we used the MEGAN (Model of Emissions of Gases and Aerosols from Nature) emission model coupled with the MOHYCAN (Model of HYdrocarbon emissions by the CANopy) canopy model to calculate the isoprene fluxes emitted by vegetation in the recent past (1979–2014) and in the future (2070–2099) over Europe at a resolution of 0.1° × 0.1°. As a result of the changing climate, modeled isoprene fluxes increased by 1.1 % yr−1 on average in Europe over 1979–2014, with the strongest trends found over eastern Europe and European Russia, whereas accounting also for the CO2 inhibition effect led to reduced emission trends (0.76 % yr−1). Comparisons with field campaign measurements at seven European sites suggest that the MEGAN-MOHYCAN model provides a reliable representation of the temporal variability of the isoprene fluxes over time scales between 1 hour to several months. For the 1979–2014 period the model was driven by the ECMWF ERA-Interim reanalysis fields, whereas for the comparison of current with projected future emissions, we used meteorology simulated with the ALARO regional climate model. Depending on the representative concentration pathways (RCPs) scenarios for greenhouse gas concentration trajectories driving the climate projections, isoprene emissions were found to increase as a result of climate change by +7 % (RCP2.6), +33 % (RCP4.5) and +83 % (RCP8.5), compared to the control simulation, and even stronger increases were found when considering the potential impact of CO2 fertilization, +15 % (RCP2.6), +52 % (RCP4.5) and +141 % (RCP8.5). However, the inhibitory CO2 effect goes a long way in cancelling these increases. Based on two distinct parameterizations, representing strong or moderate inhibition, the projected emissions accounting for all effects were estimated to be 0–17 % (strong inhibition) and 11–65 % (moderate inhibition) higher than in the control simulation. The difference obtained using the two CO2 parameterizations underscores the large uncertainty associated to this effect.
Citation: Bauwens, M., Stavrakou, T., Müller, J.-F., Van Schaeybroeck, B., De Cruz, L., De Troch, R., Giot, O., Hamdi, R., Termonia, P., Laffineur, Q., Amelynck, C., Schoon, N., Heinesch, B., Holst, T., Arneth, A., Ceulemans, R., Sanchez-Lorenzo, A., and Guenther, A.: Recent past (1979–2014) and future (2070–2099) isoprene fluxes over Europe simulated with the MEGAN-MOHYCAN model, Biogeosciences Discuss.,, in review, 2017.
Maite Bauwens et al.
Maite Bauwens et al.
Maite Bauwens et al.


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Short summary
Biogenic isoprene fluxes are simulated over Europe with the MEGAN-MOHYCAN model in the recent past and end-of-century climate at high spatiotemporal resolution (0.1 degree, 3 à min). Due to climate change, fluxes increased by 40 % over 1979–2014. Climate scenarios for 2070–2099 suggest an increase by 83 % due to climate, an even stronger increase when the potential impact of CO2 fertilization is considered (up to 141 %). Accoutning for CO2 inhibition cancels a large part of these increases.
Biogenic isoprene fluxes are simulated over Europe with the MEGAN-MOHYCAN model in the recent...