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陈运, 蒋宁, 朱莉莉. 2021: 北太平洋异常高压对京津冀地区PM2.5污染影响分析. 暴雨灾害, 40(6): 608-616. DOI: 10.3969/j.issn.1004-9045.2021.06.005
引用本文: 陈运, 蒋宁, 朱莉莉. 2021: 北太平洋异常高压对京津冀地区PM2.5污染影响分析. 暴雨灾害, 40(6): 608-616. DOI: 10.3969/j.issn.1004-9045.2021.06.005
CHEN Yun, JIANG Ning, ZHU Lili. 2021: Impact of anomalous high pressure over the North Pacific on PM2.5pollution in Beijing-Tianjin-Hebei Region. Torrential Rain and Disasters, 40(6): 608-616. DOI: 10.3969/j.issn.1004-9045.2021.06.005
Citation: CHEN Yun, JIANG Ning, ZHU Lili. 2021: Impact of anomalous high pressure over the North Pacific on PM2.5pollution in Beijing-Tianjin-Hebei Region. Torrential Rain and Disasters, 40(6): 608-616. DOI: 10.3969/j.issn.1004-9045.2021.06.005

北太平洋异常高压对京津冀地区PM2.5污染影响分析

Impact of anomalous high pressure over the North Pacific on PM2.5pollution in Beijing-Tianjin-Hebei Region

  • 摘要: 以2021年3月2—5日京津冀地区持续4 d的PM2.5重污染过程为例,使用PM2.5质量浓度格点资料、城市空气质量指数(AQI)资料、NCEP再分析资料、海温资料以及HYSPLIT轨迹追踪模式,重点分析了北太平洋异常高压对京津冀地区PM2.5污染的影响。结果表明:(1)500 hPa北太平洋异常暖性高压系统的稳定维持是京津冀地区污染发生的有利环流形势,当该地区处于此异常高压后部并受偏南风控制时,不利于该地区污染物扩散;(2)低层850 hPa异常高压系统引导来自西北太平洋暖湿气流向京津冀地区输入使低层增温增湿,不利于污染物垂直扩散,并使污染物快速吸湿增长;(3)北太平洋异常高压与北太平洋中西部海温呈正相关,与赤道中东太平洋海温呈现负相关。北太平洋异常高压配合京津冀地面南风对该地区空气污染的发生具有一定的指示意义。

     

    Abstract: Taking the PM2.5 heavy air pollution event that lasted for 4 days in Beijing-Tianjin-Hebei Region from March 2 to 5 in 2021 as an example, we analyze mainly the impact of anomalous high pressure over the North Pacific on the air pollution in this region by using the PM2.5 mass concentration grid data, daily city air quality index (AQI), NCEP reanalysis data, sea surface temperature and the HYSPLIT trajectory tracking model. The main results are as follow. (1) The stability and maintenance of the anomalous warm high pressure system over the North Pacific at 500 hPa is favorable for the formation of air pollution in Beijing-Tianjin-Hebei Region. When this region is located on the west of the anomalous high pressure system and controlled by southerly winds in ground level, the air pollutants will be difficult to diffuse. (2) The anomalous high-pressure system at 850 hPa guides the warm and wet airflow from the Northwest Pacific to Beijing-Tianjin-Hebei Region and therefore increases the low-level temperature and humidity, which hinders the vertical diffusion and accelerates the hygroscopic growth of air pollutants. (3) The anomalous high pressure is positively correlated with the sea surface temperature in the central and western parts of the North Pacific and negatively correlated with the sea surface temperature in the central and eastern equatorial Pacific. This anomalous high pressure system, along with surface southerly wind, is an important indicator for air pollution in Beijing-Tianjin-Hebei Region.

     

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