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iForest -Biogeosciences and Forestry
IntroductionAmbient ozone (O3) has been a widely studied air pollutant for many years due to its potential toxicity for all living organisms (Felzer et al. 2007, Cape 2008, Iriti & Faoro 2008. It is an important gas playing a key role in atmospheric chemistry (Seinfeldt & Pandis 1998). It contributes to the oxidative power of atmosphere which is essential for scavenging many pollutants from the air. Moreover, due to its absorption-radiation abilities, O3 is an important greenhouse gas (Singh & Fabian 2003, IPCC 2007. There are important mutual interactions between O3 and climate change (Isaksen 2003), which are not fully understood yet. The urgent need to address the knowledge gaps in interactions between air pollution, climate change and forests has been recently stressed (Serengil et al. 2011, Matyssek et al. 2012.Ozone represents one of the most prominent air pollution problems in Europe (De Leeuw & De Paus 2001, EEA 2010. Environmental O3 quality standards are exceeded over vast areas of Europe (Horálek et al. , 2009). Due to its phytotoxicity, O3 is still considered to be the most important air pollutant for forests (Paoletti et al. 2010). Due to the fact that O3 is a secondary pollutant formed from precursors during complex photochemical reactions and to the highly non-linear nature of O3 chemistry, it is and will be very difficult to decrease its ambient concentrations (Seinfeldt & Pandis 1998).Comparison of O3 levels with those measured a century ago indicates that current levels have increased by approximately two times. European measurements between 1850 and 1900 were found to be in the range of 17-23 ppb (Bojkov 1986). Modern day annual average background O3 concentrations over the mid-latitudes of the northern Hemisphere range between approximately 20-45 ppb, with variability influenced by geographic location, altitude and extent of anthropogenic impacts (Vingarzan 2004). Generally, three types of patterns in ambient O3 have been apparent recently: (1) an increase in the extent of O3 impact and the forest areas at risk; (2) a decrease in maximum 1-h O3 concentrations, at least in the northern hemisphere countries which have introduced O3 precursor control programs; and (3) an increase in background O3 concentrations over much of the world (Percy et al. 2003). It is not an easy task to assess the time trends of O3: the inter-annual variability is fairly high, so that long time series, which mostly are not available (Jonson et al. 2006), are needed to detect trends.In the Czech Republic (CR), ambient air pollution has been perceived as a major environmental problem since the 1950s, particularly due to extremely high emissions of SO2 and particulate matter from large powergenerating sources (Moldan & Schnoor 1992). Pollution in the form of surface O3 was recognized as an issue as late as in the 1990s. Its levels are regularly measured within the framework of a national ambient air quality network run by the Czech Hydrometeorological Institute (CHMI) since 1993. Fro...