Wang Xiao-Lan, Wang Yan, Yan Shi-Ming, Yue Jiang, Guo Wei, Hao Zhen-Rong
Shanxi Province Institute of Meteorological Sciences, Taiyuan 030002, China.
Shanxi Province Meteorological Information Center, Taiyuan 030006, China.
Huan Jing Ke Xue. 2022 Jul 8;43(7):3423-3438. doi: 10.13227/j.hjkx.202109056.
In this study, we analyzed the hourly concentration data of PM and PM in major cities in Jinzhong basin from 2017 to 2019. The main distribution characteristics of aerosols in Jinzhong and Taiyuan were determined, and PM hourly concentration data and HYSPLIT in Jinzhong basin in winter were discussed. The results showed that the overall level of particulate matter concentration in Taiyuan was higher than that in Jinzhong, and the monthly and seasonal variation characteristics were similar. All showed high concentrations in winter and low concentrations in summer, and the highest concentration value appeared in January. The aerosol pollution caused by the static and stable weather in Jinzhong was more common than that caused by the sand and dust weather in Taiyuan. The distribution of particulate matter showed the characteristics of more intermediate values in Jinzhong and more high and fewer low values in Taiyuan, and winter was the highest incidence season of PM pollution in Jinzhong basin. PM transmission passageways in the main cities of Jinzhong basin in winter could be divided into four categories:class 1 was transmitted along the transverse valley of Taihang Mountain, and class 2 was the southeast transmission channel. Class 1 and class 2 were the short-range transmission passageways; air masses carried more moisture, and PM transmitted along such passageways allowed moisture to be absorbed more easily, increasing levels and aggravating local pollution. Class 3 was the northwest passageway, corresponding to the most serious pollution period of PM in Jinzhong basin before the arrival of cold air, which also corresponded to the dust transmission passageway. Class 4 was the Fenwei Plain passageway, corresponding to high-concentration PM pollution. Areas with dense pollution tracks (more than 100 pollution tracks) and areas with slow air flow movement (RTA pollution track end points greater than 50) easily became potential source areas of target cities (PSCF contribution greater than 0.7). The main potential source areas of PM in winter in Jinzhong (PSCF contributing more than 0.7) were mainly distributed in Linfen, Jincheng, and other places in Shanxi province, as well as in the north of Henan province, the south of Hebei province, and central and south Shaanxi province. The distribution range of main potential source areas of PM in Taiyuan in winter was wider than that in Jinzhong, including the south of Lvliang, Yangquan, Linfen, and Yuncheng and the south of Jinzhong in Shanxi, as well as most areas in southern Shaanxi, northern Henan province, and southern Hebei province. In addition, the PSCF distribution of high-value centers above 0.9 was wider than that of Jinzhong. When pollution occurs in cities that PSCF contributed more than 0.9, special attention should be paid to the influence of mutual transmission between them and cities in Jinzhong basin. Jinzhong and Taiyuan showed different distribution characteristics corresponding to the surface wind direction when light and higher pollution occur, when the wind direction near the ground in Jinzhong was E, the frequency of light and higher pollution was 8.1%; it was the highest in all wind directions. When the wind direction near the ground in Taiyuan was SSW, the frequency of light to higher polluted weather was the highest in all wind directions (5.1%). In the case of calm wind, the frequency of light to higher pollution in Taiyuan (3.4%) was higher than that in Jinzhong (0.5%).
本研究分析了2017 - 2019年晋中盆地主要城市PM和PM的小时浓度数据。确定了晋中与太原气溶胶的主要分布特征,并探讨了晋中盆地冬季PM小时浓度数据及HYSPLIT情况。结果表明,太原颗粒物浓度总体水平高于晋中,月变化和季节变化特征相似。均呈现冬季浓度高、夏季浓度低的特点,最高浓度值出现在1月。晋中静稳天气造成的气溶胶污染比太原沙尘天气造成的更为常见。颗粒物分布呈现晋中中间值较多、太原高值较多且低值较少的特点,冬季是晋中盆地PM污染的高发季节。晋中盆地主要城市冬季PM传输通道可分为四类:1类沿太行山横向谷地传输,2类为东南传输通道。1类和2类为短距离传输通道;气团携带较多水汽,沿此类通道传输的PM更容易吸附水汽,使浓度升高并加重局部污染。3类为西北通道,对应冷空气到来前晋中盆地PM污染最严重时期,也对应沙尘传输通道。4类为汾渭平原通道,对应高浓度PM污染。污染轨迹密集(超过100条污染轨迹)且气流运动缓慢区域(RTA污染轨迹端点大于50)易成为目标城市潜在源区(PSCF贡献大于0.7)。晋中冬季PM主要潜在源区(PSCF贡献大于0.7)主要分布在山西省临汾、晋城等地,以及河南省北部、河北省南部、陕西省中南部。太原冬季PM主要潜在源区分布范围比晋中更广,包括山西省吕梁南部、阳泉、临汾、运城以及晋中南部,还有陕西省南部大部分地区、河南省北部、河北省南部。此外,PSCF大于0.9的高值中心分布范围比晋中更广。当PSCF贡献大于0.9的城市发生污染时,应特别关注其与晋中盆地城市间相互传输的影响。晋中与太原在轻度及较高污染发生时对应地面风向呈现不同分布特征,晋中地面风向为E时,轻度及较高污染频率为8.1%;在所有风向中最高。太原地面风向为SSW时,轻度至较高污染天气频率在所有风向中最高(5.1%)。在静风情况下,太原轻度至较高污染频率(3.4%)高于晋中(0.5%)。