Vegetation plays a pivotal role in the exchange of trace gases between the land surface and the atmosphere. The emissions of biogenic volatile organic compounds (BVOCs) with a global mean of 760 TgC a â1 (1980-2010), exceed those from anthropogenic sources with around 110 TgC a â1 (AVOCs, e.g., from transport, solvent use, production and storage processes, and combustion processes) by far (Calfapietra et al., 2013;Piccot et al., 1992;Sindelarova et al., 2014). In addition, BVOCs are generally more reactive than AVOCs. Once emitted into the air, BVOCs immediately start to oxidize with the hydroxyl radical (OH), ozone (O 3 ), nitrate radical (NO 3 ), and in coastal areas with chlorine (Cl) atoms, leading to first generation BVOC products (Peñuelas & Staudt, 2010). The reaction of BVOCs with OH is the dominant kind of BVOC decomposition in the troposphere, which is why the total BVOC-OH reactivity is generally used to quantify the emission impact on atmospheric chemistry