Spatial disparities of ozone pollution in the Sichuan Basin spurred by extreme, hot weather
<p>Under the influence of climate change, the increasing occurrence of extreme weather events, such as heatwaves, has led to an enhanced frequency of ozone (O<span class="inline-formula"><sub>3</sub></span>) pollution issues. In August 2022, the Sichuan Basin...
| Main Authors: | , , , , , , , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2024-03-01
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| Series: | Atmospheric Chemistry and Physics |
| Online Access: | https://acp.copernicus.org/articles/24/3029/2024/acp-24-3029-2024.pdf |
| Summary: | <p>Under the influence of climate change, the increasing occurrence of extreme weather events, such as heatwaves, has led to an enhanced frequency of ozone (O<span class="inline-formula"><sub>3</sub></span>) pollution issues. In August 2022, the Sichuan Basin (SCB), a typical large-scale geographical terrain located in southwestern China, experienced the most severe heatwave in the last 20 years. The heatwave led to substantial disparities in O<span class="inline-formula"><sub>3</sub></span> levels across the region. Here, by integrating observations, machine learning, and numerical simulations, we aim to understand the diverse O<span class="inline-formula"><sub>3</sub></span> formation mechanisms in two megacities, Chengdu (western location) and Chongqing (eastern location). Observational data showed that Chengdu experienced a consecutive 17 d period of O<span class="inline-formula"><sub>3</sub></span> exceedance, in contrast to Chongqing, where O<span class="inline-formula"><sub>3</sub></span> concentrations remained below the standard. Meteorological and precursor factors were assessed, highlighting high temperatures, intense solar radiation, and overnight accumulative pollutants as key contributors to O<span class="inline-formula"><sub>3</sub></span> concentrations. The interplay of isoprene, temperature, and O<span class="inline-formula"><sub>3</sub></span>, alongside the observation-based box model and MEGAN simulations, underscored the significant role of intensified biogenic volatile organic compounds (BVOCs) in O<span class="inline-formula"><sub>3</sub></span> formation. Interestingly, Chongqing exhibited nearly double the BVOC emissions of Chengdu, yet contributed less to O<span class="inline-formula"><sub>3</sub></span> concentrations. This discrepancy was addressed through CMAQ-DDM (Decoupled Direct Method) simulations and satellite diagnosis by investigating the O<span class="inline-formula"><sub>3</sub></span>–NO<span class="inline-formula"><sub><i>x</i></sub></span>–VOC sensitivity. Notably, Chengdu displayed a VOC-driven sensitivity, while Chongqing showed a transitional regime. Moreover, the regional transport also played a pivotal role in the spatial divergence of O<span class="inline-formula"><sub>3</sub></span> pollution. Cross-regional transport predominantly influenced Chongqing (contributing <span class="inline-formula">∼</span> 80 %), whereas Chengdu was mainly affected by the emissions within the basin. The local accumulated pollutants gave rise to the atmospheric oxidizing capacity, resulting in a substantial photochemical contribution to O<span class="inline-formula"><sub>3</sub></span> levels (49.9 ppbv h<span class="inline-formula"><sup>−1</sup></span>) in Chengdu. This comparison of the difference provides insights into the complex interplay of meteorology, natural emissions, and anthropogenic sources during heatwaves, guiding the necessity of targeted pollution control measures on regional scales.</p> |
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| ISSN: | 1680-7316 1680-7324 |