Temperature response measurements from eucalypts give insight into the impact of Australian isoprene emissions on air quality in 2050

• Published in: Atmospheric chemistry and physics 2020-05, Vol.20 (10), p.6193-6206
• Main Authors: Emmerson, Kathryn M, Possell, Malcolm, Aspinwall, Michael J, Pfautsch, Sebastian, Tjoelker, Mark G
• Format: Article
• Language: English
• Subjects: Aerosols; Air; Air pollution; Air pollution control; Air quality; Anthropogenic factors; Carbon dioxide; Carbon dioxide atmospheric concentrations; Chemical transport; Cities and towns; Climate; Climate change; Emission measurements; Emissions; Emissions (Pollution); Environmental conditions; Eucalyptus; Flowers & plants; Gases; Human influences; Isoprene; Isoprene emissions; Mathematical models; Mixing ratio; Nature; Nitrogen compounds; Oxides; Ozone; Ozone mixing ratio; Photosynthesis; Photosynthetically active radiation; Radiation; Radiation (Physics); Summer; Temperature; Temperature measurement
• ISSN: 1680-7324; 1680-7316; 1680-7324
• DOI: 10.5194/acp-20-6193-2020

Predicting future air quality in Australian cities dominated by eucalypt emissions requires an understanding of their emission potentials in a warmer climate. Here we measure the temperature response in isoprene emissions from saplings of four different Eucalyptus species grown under current and future average summertime temperature conditions. The future conditions represent a 2050 climate under Representative Concentration Pathway 8.5, with average daytime temperatures of 294.5 K. Ramping the temperature from 293 to 328 K resulted in these eucalypts emitting isoprene at temperatures 4–9 K higher than the default maximum emission temperature in the Model of Emissions of Gases and Aerosols from Nature (MEGAN). New basal emission rate measurements were obtained at the standard conditions of 303 K leaf temperature and 1000 µmol m−2 s−1 photosynthetically active radiation and converted into landscape emission factors. We applied the eucalypt temperature responses and emission factors to Australian trees within MEGAN and ran the CSIRO Chemical Transport Model for three summertime campaigns in Australia. Compared to the default model, the new temperature responses resulted in less isoprene emission in the morning and more during hot afternoons, improving the statistical fit of modelled to observed ambient isoprene. Compared to current conditions, an additional 2 ppb of isoprene is predicted in 2050, causing hourly increases up to 21 ppb of ozone and 24-hourly increases of 0.4 µg m−3 of aerosol in Sydney. A 550 ppm CO2 atmosphere in 2050 mitigates these peak Sydney ozone mixing ratios by 4 ppb. Nevertheless, these forecasted increases in ozone are up to one-fifth of the hourly Australian air quality limit, suggesting that anthropogenic NOx should be further reduced to maintain healthy air quality in future.