Volatility of secondary organic aerosol from the ozonolysis of monoterpenes

► All the SOA from monoterpene ozonolysis evaporates after 16 s at temperatures less than 90 °C. ► The α- and β-pinene SOA formed at high NOx conditions is more volatile. ► The formation relative humidity has a small effect on volatility. ► The results are consistent with the volatility basis-set parameters. ► There are significant mass transfer limitations in the evaporation of biogenic SOA.