首页|基于激光雷达和微波辐射计的气溶胶质量浓度反演算法研究与分析

基于激光雷达和微波辐射计的气溶胶质量浓度反演算法研究与分析

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大气气溶胶是重要的大气污染物之一,气溶胶质量浓度的垂直分布及其与气象要素的相互影响,对理解大气污染传输具有重要意义。激光雷达因具有高时空分辨率的探测优势而成为研究气溶胶颗粒物立体分布的有力工具。本文利用深圳米散射激光雷达、微波辐射计和近地面气溶胶质量浓度监测仪,根据均方差选取最优参数,建立基于消光系数的温湿融合PM2。5质量浓度反演模型,并以深圳气象梯度观测塔4个高度的PM2。5质量浓度小时均值为基准,对模拟结果进行了验证分析。结果显示:模拟值与观测值两者的变化趋势一致性较好,相关系数受模拟高度、相对湿度影响,并进行了晴天、多云天气下的比对,深圳气象梯度观测塔上4个高度的模拟值和实测值相关系数均大于0。68,平均绝对误差和均方根误差最大值分别为6。88 µg/m3和18。56 μg/m3。比较4个季节的模拟效果发现,冬季的模拟结果准确性要低于其他三个季节。最后通过个例分析,结合地面温度、相对湿度、风场和气压场,分析了深圳夏季颗粒物质量浓度的时空分布特征。
Aerosol Mass Concentration Retrieval Algorithm Based on LiDAR and Microwave Radiometry
Objective The technology for retrieving aerosol extinction coefficients from LiDAR is mature.However,further progress is required to retrieve the vertical distribution of aerosol mass concentration.In addition,accuracy evaluation of aerosol mass concentration from LiDAR is challenging owing to the lack of standard vertical PM2.5 mass concentration.Therefore,in this study,a PM2.5 mass concentration retrieval algorithm was developed by integrating real-time temperature,relative humidity,and extinction coefficient profiles.The PM2.5 mass concentration at four heights of the Shenzhen Meteorological Gradient Observation Tower was used as the standard value to evaluate the accuracy of the model under different weather conditions and seasons.Methods The influence of meteorological factors on the vertical distribution of aerosol mass concentration is extremely complex,particularly under precipitation conditions where the LiDAR signal attenuation is severe.Therefore,in this study,only the effects of temperature and relative humidity on the vertical distribution of aerosols under non-precipitation weather conditions were investigated.In practical applications,sample data are initially preprocessed,including the outlier handling(triple standard deviation removal),rainy day data,and missing value removal.The extinction coefficient at the lowest height of the LiDAR,ground temperature,relative humidity from the microwave radiometer,and PM2.5 mass concentration near the ground were substituted into an exponential model.The data from 2500 h were subsequently used for model fitting.The model parameters were automatically determined based on the minimum mean square error.Thus,the extinction coefficient,temperature,and relative humidity profiles at a specific height could be selected to calculate the PM2.5 mass concentration at the corresponding height.To investigate the accuracy of the PM2.5 mass concentration inversion,comparisons were conducted between PM2.5 mass concentrations at four heights(70,120,220,and 335 m)on the Shenzhen Meteorological Gradient Observation Tower.Results and Discussions By comparing different weather conditions,the correlation coefficients between the simulated and measured values at the four heights are over 0.68(Figs.3 and 4).The maximum mean absolute error(MAE)and root mean square error(RMSE)are 6.88 μg/m3 and 18.56 μg/m3,respectively,appearing at a height of 335 m on sunny days.In different seasons,the correlation coefficients at the four heights range from 0.78-0.93,0.71-0.81,0.73-0.80,and 0.63-0.75,respectively(Table 4).The PM2.5 mass concentration spatiotemporal distribution and transport process on July 29,2022,was selected as a case study for analysis(Fig.6).Before 08:00,the aerosol extinction coefficient within 1 km of the boundary layer is relatively low(<0.3 km-1),and the PM2.5 mass concentration,and extinction coefficient decreased with increasing altitude.However,the decrease in gradient was insignificant.This is because the PM2.5 mass concentration mixed unevenly with altitude changes owing to stable stratification on that day.Moreover,relatively weak winds are not conducive to diffusion.Under high temperature and relative humidity conditions,the hygroscopicity of aerosols at high altitudes increases.Thus,the averaged extinction coefficient over 0.48 km is greater than 0.5 km-1,and high PM2.5 mass concentration(40 μg/m3)is observed simultaneously.This indicates that atmospheric aerosol vertical distribution is significantly influenced by temperature and relative humidity.In addition,the vertical distribution of aerosols is fully reflected in the height variation of PM2.5 mass concentration,which provides an analytical tool for examining the vertical distribution of aerosol microscopic physical characteristics.Conclusions This study established a multivariate PM2.5 mass concentration fitting model based on an exponential model combining temperature,relative humidity,and extinction profiles.The optimal parameters were selected based on the minimum mean-square deviation index,and the output was validated.Compared to the linear and exponential basic models,the accuracy of the multivariate fitting model has been improved,with correlation coefficients at all four heights above 0.80.The minimum MAE and RMSE are approximately 4 μg/m3and 7 μg/m3,respectively.Under clear and cloudy weather conditions,the correlation coefficients at four altitudes exceed 0.68,and the MAE and RMSE are below 7 μg/m3and 19 μg/m3,respectively.The simulation results spanning different seasons demonstrate that the average mass concentration of PM2.5 in Shenzhen is below 35 μg/m3.The simulated PM2.5 mass concentration exhibited seasonal variation patterns.In addition,the simulation results for spring,summer,and autumn are better than those for winter.This may be due to the uncertainty caused by the relatively high aerosol mass concentrations in winter.Considering the uncertainty caused by the LiDAR and microwave radiometer measurement processes,the validation results of the proposed multivariate model performed well within an acceptable range.

LiDARPM2.5 mass concentrationextinction coefficient

季承荔、陈臻懿、黄艺峰、茆佳佳、王志成、古锐昌、刘爱明、张春生、项衍

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中国气象局气象探测中心,北京 100081

中国气象局气象探测工程技术研究中心,北京 100081

北京工商大学轻工科学与工程学院,北京 100048

深圳市国家气候观象台,广东深圳 518040

安徽大学物质科学与信息技术研究院,安徽合肥 230601

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激光雷达 PM2.5质量浓度 消光系数

中国气象局创新发展专项中国气象局创新发展专项民用航天技术预研项目中国科学院环境光学与技术重点实验室开放基金

CXFZ2024J011CXFZ2024J057D0203052005DP173065-2021-07

2024

中国激光
中国光学学会 中科院上海光机所

中国激光

CSTPCD北大核心
影响因子:2.204
ISSN:0258-7025
年,卷(期):2024.51(5)