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Biogenic isoprene emissions from herbaceous plants are generally lower than those from trees. However, our study finds widespread isoprene emission in herbaceous sedge plants, with a stronger temperature response surpassing current tree-derived models. We measured and compared isoprene emissions from sedges grown in different climatic zones, all showing an exponential temperature response with a Q10 range of 7.2 to 12, significantly higher than the Q10 of about 3 for other common isoprene emitters. The distinct temperature sensitivity of sedges makes them a hidden isoprene source, significant during heat waves but not easily detected in mild weather. For instance, isoprene emissions fromCarex praegraciliscan increase by 320% with a peak emission of over 100 nmol m⁻²s⁻¹compared to preheat wave emissions. During heat waves, the peak isoprene emissions fromC. praegraciliscan match those fromLophostemon confertus, a commonly used street tree species which is considered the dominant urban isoprene source due to higher biomass and emission capacities. This surge in isoprene from globally distributed sedges, including those in urban landscapes, could contribute to peak ozone and aerosol pollutants during heat waves. 

As worldwide trends move toward replacing combustion transportation modes with electric vehicles, characterizing non-tailpipe emissions, such as those from brake wear, becomes increasingly important. Nitrous acid (HONO), nitryl chloride (ClNO2), and dinitrogen pentoxide (N2O5) are important sources of radical oxidants (e.g., •OH, •Cl, •NO3) and nitrogen oxides (NOx) in the atmosphere, driving the chemistry that leads to air quality degradation. Discrepancies between measurements and model predictions indicat that there are significant unknown sources of these species, particularly HONO, where the contributions of different formation processes have been controversial since the first ambient observations in the 1970s. We report the generation of these reactive nitrogen species during automotive braking using chemical ionization mass spectrometry configured with iodide reagent ion. Substantial HONO levels are observed from ceramic and semi-metallic brake pads, and smaller quantities of ClNO2 and N2O5 were also detected. We propose that HONO is formed in the hot plume emanating from the brake rotor via abstraction by NO2 of allylic and aldehyde hydrogen atoms found in the complex mixture of volatile organic compounds emitted simultaneously. These results suggest that emissions from automotive braking must be taken into account in urban oxidation chemistry. 

Abstract It has been widely reported that isoprene emissions from the Arctic ecosystem have a strong temperature response. Here we identify sedges (Carexspp. andEriophorumspp.) as key contributors to this high sensitivity using plant chamber experiments. We observe that sedges exhibit a markedly stronger temperature response compared to that of other isoprene emitters and predictions by the widely accepted isoprene emission model, the Model of Emissions of Gases and Aerosols from Nature (MEGAN). MEGAN is able to reproduce eddy-covariance flux observations at three high-latitude sites by integrating our findings. Furthermore, the omission of the strong temperature responses of Arctic isoprene emitters causes a 20% underestimation of isoprene emissions for the high-latitude regions of the Northern Hemisphere during 2000-2009 in the Community Land Model with the MEGAN scheme. We also find that the existing model had underestimated the long-term trend of isoprene emissions from 1960 to 2009 by 55% for the high-latitude regions. 

It has been widely reported that isoprene emissions from Arctic ecosystems show a strong temperature response, and that Arctic warming is increasing ecosystem isoprene emissions. We conducted leaf-chamber experiments on two major groups of Arctic isoprene emitters—sedges and willows—near Toolik Field Station, Alaska, USA. We identify sedges (Carex spp. and Eriophorum spp.) as key contributors to this high temperature sensitivity. Sedges exhibit a markedly stronger temperature response than other isoprene emitters and than predicted by widely used isoprene emission models. In addition, we find that the hourly temperature response curve of Salix spp., the dominant isoprene-emitting shrub in the Arctic, is similar to that of temperate plants. In contrast, willow isoprene emission capacity or emission factor shows a more substantial-than-expected response to the previous day’s mean ambient temperature. 

Abstract Warming climate in the Arctic is leading to an increase in isoprene emission from ecosystems. We assessed the influence of temperature on isoprene emission from Arctic willows with laboratory and field measurements. Our findings indicate that the hourly temperature response curve ofSalixspp., the dominant isoprene emitting shrub in the Arctic, aligns with that of temperate plants. In contrast, the isoprene capacity of willows exhibited a more substantial than expected response to the mean ambient temperature of the previous day, which is much stronger than the daily temperature response predicted by the current version of the Model of Emissions of Gases and Aerosols from Nature (MEGAN). With a modified algorithm from this study, MEGAN predicts 66% higher isoprene emissions for Arctic willows during an Arctic heatwave. However, despite these findings, we are still unable to fully explain the high temperature sensitivity of isoprene emissions from high latitude ecosystems.