首页|南京地区局地积累型和外来输送型O3污染模拟研究

南京地区局地积累型和外来输送型O3污染模拟研究

Modelling of Local Accumulation and External Transport of O3 Pollution in Nanjing Area

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利用观测资料和WRF-Chem空气质量模式对南京地区局地积累型和外来输送型O3污染过程的时空分布特征和潜在机制进行了研究.结果表明:①水平分布特征,在两次03污染整体过程中,外来输送型O3污染浓度高值区分布范围相比局地积累型更大且较为分散.但在两次O3污染过程中最严重的白天,局地积累型O3污染浓度高值区分布范围大且集中,O3浓度大部分均超过160 μg/m3;而外来输送型O3污染浓度高值区分布范围更小且更为分散,O3浓度在120~160µg/m3的地区范围显著大于局地积累型O3污染;②垂直分布特征,在污染过程前期,局地积累型O3污染在2 km以下高度处有着高浓度O3,浓度最高超250 µg/m3,而外来输送型O3污染浓度高值区主要集中在2~2.5 km高度处,且高值区浓度最高不超过200 µg/m3;在污染过程中期,局地积累型O3污染浓度高值区集中在2 km高度下,且在1 km左右高度处O3浓度出现最大值;而外来输送型O3污染浓度高值区最高可达到2.6 km左右,并且浓度最大值集中在1.5 km高度以下,均超过250 μg/m3;在污染过程后期,局地积累型O3污染浓度高值区逐渐消散,但外来输送型O3污染在0.5~3 km高度内仍出现大范围O3浓度高值区;③在生成机理方面,近地面O3的高浓度在局地积累型O3污染中主要依赖于垂直混合,96 h内总贡献为451.7 μg/m3,在总过程量中占比为66.2%,而在外来输送型O3污染中主要依赖于水平平流和垂直混合,72h内总贡献分别为1 050.2 µg/m3和799.1 μg/m3,总量在总过程量中占比为61.5%.在500 m高度处,局地积累型O3污染前期O3的高浓度主要依赖于垂直平流和化学过程,中期只依赖于化学过程,后期则主要依赖于水平平流和化学过程.但在外来输送型O3污染前中后期中高O3浓度均主要依赖于水平平流和化学过程.在1 000 m高度处,两个过程中O3浓度的正贡献均主要受化学过程控制.
The spatial and temporal distribution characteristics and potential mechanisms of local accumulation and transported O3 pollution in Nanjing were investigated using observation data and the WRF-Chem air quality model.The results show that,for the horizontal distribution characteristics the distribution of high values of exogenous O3 pollution is larger and more dispersed than that of local accumulation O3 pollution during the two O3 pollution episodes.However,during the most severe daytime hours of both O3 pollution processes,the distribution of high value areas of local accumulation O3 pollution was large and concentrated,with most of the O3 concentrations exceeding 160 μg/m3,while the distribution of high value areas of external transport O3 pollution was smaller and more dispersed,with concentrations in the range of 120-160 μg/m3 being significantly larger than that of local accumulation O3 pollution.For the vertical distribution characteristics,in the early stage of the pollution episode,local accumulation O3 pollution has high O3 concentrations below 2 km height,with concentrations up to 250 µg/m3,while the high value areas of external transport O3 pollution are mainly concentrated at 2-2.5 km height,and the highest concentration does not exceed 200 μg/m3;in the middle of the pollution process,the high value area of local accumulation O3 pollution concentration is concentrated under 2 km height,and the maximum O3 concentration occurs at about 1 km height;while the high value area of external transport O3 pollution concentration can reach up to about 2.6 km height,and the maximum concentration is concentrated under 1.5 km height,and all exceed 250 μg/m3;in the late stage of the pollution process,the high value area of local accumulation O3 pollution concentration gradually dissipates,but the external transport of O3 pollution still appears in a wide areas within 0.5-3 km altitude.In terms of generation mechanism,high near-surface O3 concentrations are mainly depended on vertical mixing in local accumulation O3 pollution,with a total contribution of 451.7 μg/m3 over 96 h,accounting for 66.2%of the total process volume,while in external transport O3 pollution it is mainly depended on horizontal advection and vertical mixing,with a total contribution of 1 050.2 μg/m3 and 799.1 μg/m3 over 72 h,respectively,with a total contribution of 61.5%to the total process volume.At an altitude of 500 m,the high concentration of O3 in the early stage of local accumulation O3 pollution mainly depends on vertical advection and chemical processes,while it only depends on chemical processes in the middle stage,and mainly depends on horizontal advection and chemical processes in the later stage.However,the medium-high O3 concentration in the early,middle,and late stages of external transport O3 pollution mainly depends on horizontal advection and chemical processes.At an altitude of 1 000 m,the positive contribution of O3 concentration in both episodes is mainly controlled by the chemical process.

O3observational analysisWRF-Chemprocess analysisNanjing

裴宇儇、彭薇、王红磊、卢文、赵天良、刘思晗、武自豪、可玥

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南京信息工程大学气象灾害预报预警与评估协同创新中心,中国气象局气溶胶-云-降水重点开放实验室,南京 210044

湖南省气象信息中心气象防灾减灾湖南省重点实验室,长沙 410118

O3 观测分析 WRF-Chem 过程分析 南京

国家重点研发计划国家自然科学基金国家自然科学基金江苏省自然科学基金

2022YFC37012044227519641830965BK20231300

2024

地球与环境
中国科学院地球化学研究所

地球与环境

CSTPCD北大核心
影响因子:0.875
ISSN:1672-9250
年,卷(期):2024.52(2)
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