<p>Surface ozone pollution, a major threat to ecosystems and human health, can be exacerbated by interactions between anthropogenic and biogenic emissions. Here we combine field observations with numerical models to reveal a previously unrecognized pathway that intensifies ozone pollution: urban expansion fragments forests, forming Urban-Forest-Urban plumes that trigger cascading ozone production. In South China, five-year observations show ozone levels in Urban-Forest-Urban plumes are 35%–105% higher than in other plume types during hot seasons. Urban pollutants infiltrating forests elevate atmospheric oxidation capacity, accelerating biogenic volatile organic compounds oxidation and boosting their ozone contribution by up to twelvefold. The resulting long-lived oxygenated volatile organic compounds are transported downwind and further react with urban nitrogen oxides, enhancing ozone production. This mechanism shows strong temperature dependence, with up to 10% more ozone per 1 °C warming, underscoring its growing significance under climate change.</p><p></p>

错误:搜索内容不能为空,请输入英文关键词
错误:关键词超出字数限制,请精简
高级检索

Landscape fragmentation triggers cascading enhancement of surface ozone production

  • Jiangyong Li,
  • Hao Wang,
  • Daocheng Gong,
  • Qinqin Li,
  • Yu Wang,
  • Wenlong Zhao,
  • Chunlin Zhang,
  • Zihan Zhou,
  • Yiming Zhao,
  • Qiao Xu,
  • Yan Zhou,
  • Congrong He,
  • Zoran Ristovski,
  • Lidia Morawska,
  • Shaw Chen Liu,
  • Boguang Wang

摘要

Surface ozone pollution, a major threat to ecosystems and human health, can be exacerbated by interactions between anthropogenic and biogenic emissions. Here we combine field observations with numerical models to reveal a previously unrecognized pathway that intensifies ozone pollution: urban expansion fragments forests, forming Urban-Forest-Urban plumes that trigger cascading ozone production. In South China, five-year observations show ozone levels in Urban-Forest-Urban plumes are 35%–105% higher than in other plume types during hot seasons. Urban pollutants infiltrating forests elevate atmospheric oxidation capacity, accelerating biogenic volatile organic compounds oxidation and boosting their ozone contribution by up to twelvefold. The resulting long-lived oxygenated volatile organic compounds are transported downwind and further react with urban nitrogen oxides, enhancing ozone production. This mechanism shows strong temperature dependence, with up to 10% more ozone per 1 °C warming, underscoring its growing significance under climate change.