(H.R.); 0000-0002-9825-867X (J.-P.S.).Isoprene emissions from poplar (Populus spp.) plantations can influence atmospheric chemistry and regional climate. These emissions respond strongly to temperature, [CO 2 ], and drought, but the superimposed effect of these three climate change factors are, for the most part, unknown. Performing predicted climate change scenario simulations (periodic and chronic heat and drought spells [HDSs] applied under elevated [CO 2 ]), we analyzed volatile organic compound emissions, photosynthetic performance, leaf growth, and overall carbon (C) gain of poplar genotypes emitting (IE) and nonemitting (NE) isoprene. We aimed (1) to evaluate the proposed beneficial effect of isoprene emission on plant stress mitigation and recovery capacity and (2) to estimate the cumulative net C gain under the projected future climate. During HDSs, the chloroplastidic electron transport rate of NE plants became impaired, while IE plants maintained high values similar to unstressed controls. During recovery from HDS episodes, IE plants reached higher daily net CO 2 assimilation rates compared with NE genotypes. Irrespective of the genotype, plants undergoing chronic HDSs showed the lowest cumulative C gain. Under control conditions simulating ambient [CO 2 ], the C gain was lower in the IE plants than in the NE plants. In summary, the data on the overall C gain and plant growth suggest that the beneficial function of isoprene emission in poplar might be of minor importance to mitigate predicted short-term climate extremes under elevated [CO 2 ]. Moreover, we demonstrate that an analysis of the canopy-scale dynamics of isoprene emission and photosynthetic performance under multiple stresses is essential to understand the overall performance under proposed future conditions. Climate change will lead to an increase in global temperatures of at least 2°C in the near future (IPCC, 2014). There is at present substantial evidence that this climate change is leading to an increase in the frequency and intensity of extreme events such as heat and drought waves (Feyen and Dankers, 2009;Fischer and Schär, 2010;Perkins et al., 2012;Thornton et al., 2014), creating a sequence of recurring stress and recovery cycles for plants. Coumou and Rahmstorf (2012) showed that, in the last 15 years, five extreme heat wave events have occurred worldwide, four of which were observed also in Europe. Interactions between heat and drought under predicted elevated [CO 2 ] (IPCC, 2014) generate complex, often nonadditive physiological responses. Such effects cannot be predicted by singlefactor analyses and highlight the importance of carrying out controlled, multistress scenarios to investigate plant performance under future climate conditions (Clausen et al., 2011; Alemayehu et al., 2014).Photosynthesis, respiration, and photorespiration are the three dominating processes determining carbon (C) exchange and C metabolism in plants (Bauwe et al., 2010;Mahecha et al., 2010). In addition, the emission of biogenic volatile organic c...