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Abstract
Ozone air pollution is identified as one of the main threats bearing upon human health and ecosystems, with 25 000 deaths in 2005 attributed to surface ozone in Europe (IIASA 2013 TSAP Report #10). In addition, there is a concern that climate change could negate ozone pollution mitigation strategies, making them insufficient over the long run and jeopardising chances to meet the long term objective set by the European Union Directive of 2008 (Directive 2008/50/EC of the European Parliament and of the Council of 21 May 2008) (60 ppbv, daily maximum). This effect has been termed the ozone climate penalty. One way of assessing this climate penalty is by driving chemistry-transport models with future climate projections while holding the ozone precursor emissions constant (although the climate penalty may also be influenced by changes in emission of precursors). Here we present an analysis of the robustness of the climate penalty in Europe across time periods and scenarios by analysing the databases underlying 11 articles published on the topic since 2007, i.e. a total of 25 model projections. This substantial body of literature has never been explored to assess the uncertainty and robustness of the climate ozone penalty because of the use of different scenarios, time periods and ozone metrics. Despite the variability of model design and setup in this database of 25 model projection, the present meta-analysis demonstrates the significance and robustness of the impact of climate change on European surface ozone with a latitudinal gradient from a penalty bearing upon large parts of continental Europe and a benefit over the North Atlantic region of the domain. Future climate scenarios present a penalty for summertime (JJA) surface ozone by the end of the century (2071–2100) of at most 5 ppbv. Over European land surfaces, the 95% confidence interval of JJA ozone change is [0.44; 0.64] and [0.99; 1.50] ppbv for the 2041–2070 and 2071–2100 time windows, respectively.
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1 Institut National de l’Environnement Industriel et des Risques (INERIS), Verneuil-en-Halatte, France
2 Swedish Meteorological and Hydrological Institute (SMHI), Norrköping, Sweden
3 Danish Meteorological Institute, Lyngbyvej 100, DK 2100, København Ø, Denmark
4 Aarhus University, Department of Environmental Science, Frederiksborgvej 399, DK 4000 Roskilde, Denmark
5 School of GeoSciences, University of Edinburgh, U K
6 Institute for Environmental Research and Sustainable Development, National Observatory of Athens, Athens, Greece
7 Department of Meteorology and Climatology, School of Geology, Aristotle University of Thessaloniki, Thessaloniki, Greece
8 National Oceanic and Atmospheric Administration (NOAA), USA
9 Netherlands Organisation for Applied Scientific Research (TNO), Delft, The Netherlands
10 Laboratory of Atmospheric Physics, School of Physics, Aristotle University of Thessaloniki, Thessaloniki, Greece
11 Finnish Meteorological Institute, PO Box 503, FI 00101 Helsinki, Finland
12 Division of Environmental Physics and Meteorology, National and Kapodistrian University of Athens, Athens, Greece
13 Division of Environmental Physics and Meteorology, National and Kapodistrian University of Athens, Athens, Greece; Institute for Environmental Research and Sustainable Development, National Observatory of Athens, Athens, Greece
14 Lancaster Environment Centre, Lancaster University, Lancaster, U K