Tropospheric ozone (O 3 ) is among the most damaging air pollutant to plants. Plants alter the atmospheric O 3 concentration in two distinct ways: (i) by the emission of volatile organic compounds (VOCs) that are precursors of O 3; and (ii) by dry deposition, which includes diffusion of O 3 into vegetation through stomata and destruction by nonstomatal pathways. Isoprene, monoterpenes, and higher terpenoids are emitted by plants in quantities that alter tropospheric O 3 . Deposition of O 3 into vegetation is related to stomatal conductance, leaf structural traits, and the detoxification capacity of the apoplast. The biochemical fate of O 3 once it enters leaves and reacts with aqueous surfaces is largely unknown, but new techniques for the tracking and identification of initial products have the potential to open the black box. Tropospheric O 3 formation O 3 (see Glossary) in the stratosphere filters UV radiation, but in the troposphere O 3 is a damaging air pollutant to human and plant health [Environmental Protection Agency (EPA): https://www.epa.gov/ground-level-ozone-pollution; Box 1]. Tropospheric O 3 (trioxygen) is an allotrope of oxygen that forms through chemical reactions with two chemically distinct precursors: nitrogen oxides (NO x = NO + NO 2 ) and reactive carbon molecules including carbon monoxide (CO), methane (CH 4 ), and VOCs (Figure 1) [1]. Rates of O 3 formation depend on sunlight and the relative concentrations of NO x and reactive carbon molecules; namely, methane and VOCs [1]. The reaction of nitric oxide (NO) with the peroxy radical (R 2 ) is the central reaction for the formation of O 3 in the troposphere [2]. In this reaction, NO is converted to NO 2 (Figure 1), which is rapidly photolyzed to form O 3 and recycle NO. The efficiency with which O 3 is produced from NO x pollution varies with the location and time of emissions. For example, in the polluted regions at the Earth's surface, NO x rapidly reacts to form HNO 3 , which serves as a reservoir for NO x [3]. In less polluted areas, NO 2 photolysis competes more effectively with HNO 3 production and more molecules of NO x react with peroxy radicals to form O 3 . In regions where NO x is propelled into the free troposphere, like the tropics, O 3 production is especially efficient [1,4]. Additionally, the VOC:NO x ratio determines the O 3 concentration [5]. In urban areas with elevated NO x due to high emissions, O 3 formation is limited by VOCs, leading to locally suppressed O 3 concentrations. NO x transported away from urban centers can mix with VOCs, resulting in greater O 3 concentrations in suburban areas [5].Global O 3 production in the troposphere is estimated to be between 4960 and 5530 Tg year −1 (Figure 1), with most O 3 produced from chemical reactions and a smaller amount exchanged with the stratosphere [6]. Although most of the O 3 produced in the troposphere is lost by chemical conversions, dry deposition of O 3 to the terrestrial biosphere accounts for nearly 20% of O 3 removal from the troposphere [7]. Temperature also in...