Zhao Shuyu, Feng Tian, Xiao Wangxing, Zhao Shuyun, Tie Xuexi
Ningbo Meteorological Bureau Ningbo China.
Department of Geography & Spatial Information Techniques Ningbo University Ningbo China.
J Geophys Res Atmos. 2022 Dec 27;127(24):e2021JD036345. doi: 10.1029/2021JD036345. Epub 2022 Dec 16.
Two persistent and heavy haze episodes during the COVID-19 lockdown (from 20 Jan to 22 Feb 2020) still occur in northern China, when anthropogenic emissions, particularly from transportation sources, are greatly reduced. To investigate the underlying cause, this study comprehensively uses measurements for ambient surface pollutants, reanalysis meteorological data and the WRF-Chem model to calculate the contribution of NO emission change and weather-climate change to the "unexpectedly heavy" haze. Results show that a substantial NO reduction has slightly decreased PM concentration. By contrast, the weakest East Asian winter monsoon (EAWM) in the 2019-2020 winter relative to the past decade is particularly important for haze occurrence. A warmer and moister climate is also favorable. Model results suggest that climate anomalies lead to a 25-50 μg m increase of PM concentration, and atmospheric transport is also an important contributor to two haze episodes. The first haze is closely related to the atmospheric transport of pollutants from NEC to the south, and fireworks emissions in NEC are a possible amplifying factor that warrants future studies. The second one is caused by the convergence of a southerly wind and a mountain wind, resulting in an intra-regional transport within BTH, with a maximal PM increment of 50-100 μg m. These results suggest that climate change and regional transport are of great importance to haze occurrence in China, even with significant emission reductions of pollutants.
在新冠疫情封锁期间(2020年1月20日至2月22日),中国北方仍出现了两次持续且严重的雾霾天气,而此时人为排放,尤其是交通源排放大幅减少。为探究其潜在原因,本研究综合利用地面环境污染物测量数据、再分析气象数据以及WRF-Chem模型,来计算氮氧化物排放变化和天气气候变化对“异常严重”雾霾的贡献。结果表明,氮氧化物排放量的大幅减少使细颗粒物浓度略有下降。相比之下,2019 - 2020年冬季相对于过去十年而言最弱的东亚冬季风对雾霾的出现尤为重要。更温暖潮湿的气候也较为有利。模型结果表明,气候异常导致细颗粒物浓度增加25 - 50微克/立方米,大气输送也是两次雾霾事件的重要促成因素。第一次雾霾与污染物从东北向南方的大气输送密切相关,东北地区的烟花燃放排放可能是一个放大因素,值得未来研究。第二次雾霾是由南风和山风的辐合导致的,造成了京津冀地区内部的污染物传输,细颗粒物浓度最大增量为50 - 100微克/立方米。这些结果表明,即使污染物排放量大幅减少,气候变化和区域传输对中国雾霾的出现仍至关重要。