College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China.
National Institute of Metrology, Beijing, 100029, China.
Environ Pollut. 2023 Oct 15;335:122290. doi: 10.1016/j.envpol.2023.122290. Epub 2023 Jul 29.
China has become one of the most prominent areas of global land cover change during the past few decades. These changes can directly influence meteorological parameters thus further regulating tropospheric ozone (O) formation. Moreover, changes in biogenic emissions due to land cover variation can also have an indirect effect on O concentration. This study applied the Community Multiscale Air Quality model to comprehensively evaluate the impacts of significant land cover change on O levels in China during summertime between 2001 and 2019. The results showed that the daily maximum 8-h average O concentration (MDA8 O) increased by 3.6-8.9 μg/m, 2.8-8.0 μg/m, 3.8-9.6 μg/m, -1.5-6.2 μg/m, and -0.6-2.5 μg/m in Beijing-Tianjin-Hebei region, Yangtze River Delta, Pearl River Delta, Sichuan Basin, and Fenwei Plain, respectively, in response to land cover variation. The research identified that the direct effect was the primary factor in raising O levels which mainly altered O concentration by changing vertical import and dry deposition velocity. Moreover, land cover variation tended to decrease biogenic nitric oxide emission and increase biogenic volatile organic compounds emission on the whole, and cause an obvious increase of MDA8 O by 1.8-4.9 μg/m in Pearl River Delta due to the indirect effect. This study offered valuable insights into the impacts of land cover change on O levels, highlighting the need for policymakers to consider land cover variation on air pollutants concentration for devising comprehensive multi-pollutant control strategies.
中国在过去几十年间已成为全球土地覆盖变化最为显著的地区之一。这些变化会直接影响气象参数,从而进一步调节对流层臭氧(O)的形成。此外,由于土地覆盖变化导致的生物排放变化也会对 O 浓度产生间接影响。本研究应用了社区多尺度空气质量模型,全面评估了 2001 年至 2019 年夏季期间重大土地覆盖变化对中国 O 水平的影响。结果表明,北京-天津-河北地区、长江三角洲、珠江三角洲、四川盆地和汾渭平原的日最大 8 小时平均臭氧浓度(MDA8 O)分别增加了 3.6-8.9μg/m、2.8-8.0μg/m、3.8-9.6μg/m、-1.5-6.2μg/m 和-0.6-2.5μg/m,这是由于土地覆盖变化引起的。研究发现,直接效应是提高 O 水平的主要因素,主要通过改变垂直输入和干沉降速度来改变 O 浓度。此外,土地覆盖变化总体上倾向于减少生物源一氧化氮排放,增加生物源挥发性有机化合物排放,并由于间接效应,导致珠江三角洲的 MDA8 O 明显增加 1.8-4.9μg/m。本研究深入探讨了土地覆盖变化对 O 水平的影响,强调了政策制定者在制定综合多污染物控制策略时需要考虑土地覆盖变化对空气污染物浓度的影响。