“…Until recently, attention has focused on the quantification of VOC emissions, which influence local air quality, as a result of ozone and particle formation, and climate, via complex contributions to climate‐aerosol feedbacks (Arneth et al, 2010). Vegetation is the primary source of biogenic VOCs to the atmosphere, but soils also contribute significant emissions, at least in specific situations, like the dry season in the Amazonas (Bourtsoukidis et al, 2018), permafrost thaw in the Arctic (Kramshøj et al, 2018), or shoulder seasons in boreal forest (Mäki et al, 2019). More recently, advances in instrumentation that have allowed for continuous measurements in situ have led to observations of bidirectional ecosystem VOC fluxes (Millet et al, 2018; Park et al, 2013) that have highlighted the importance of both emissions and deposition .…”