Validation and calibration of aerosol optical depth and classification of aerosol types based on multi-source data over China

被引:7
|
作者
Wang, Jing [1 ]
Liu, Yusi [2 ,3 ]
Chen, Li [1 ]
Liu, Yaxin [1 ]
Mi, Ke [1 ]
Gao, Shuang [1 ]
Mao, Jian [1 ]
Zhang, Hui [1 ]
Sun, Yanling [1 ]
Ma, Zhenxing [1 ]
机构
[1] Tianjin Normal Univ, Sch Geog & Environm Sci, Tianjin 300387, Peoples R China
[2] Chinese Acad Meteorol Sci, China Meteorol Adm, State Key Lab Severe Weather, Beijing 100081, Peoples R China
[3] Chinese Acad Meteorol Sci, China Meteorol Adm, Key Lab Atmospher Chem, Beijing 100081, Peoples R China
关键词
Aerosol optical depth; Aerosol types; Extremely randomized trees; Reanalysis; PM2.5; POLLUTION; PRODUCTS; NETWORK; AERONET; URBAN;
D O I
10.1016/j.scitotenv.2023.166603
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A refined classification of aerosol types is essential to identify and control air pollution sources. This study focused on improving the resolution and accuracy of aerosol optical depth (AOD) and further refining the classification of aerosol types in China. We validated the accuracy of the AOD acquired using the Modern-Era Retrospective Analysis for Research and Applications version 2 (MERRA2) and Copernicus Atmosphere Monitoring Service (CAMS) by comparing it with that acquired using from the Aeronet Robotic Network (AERONET). We simulated the AOD with high spatial resolution and accuracy based on the extremely randomized trees (ERT), adaptive boosting (AdaBoost), and gradient boosting decision trees (GBDT) models and identified aerosol types based on the Angstrom Exponent (AE) from the Moderate Resolution Imaging Spectroradiometer (MODIS) and the calibrated AOD. The results showed that CAMS overestimates AOD (21.4 %) and MERRA2 underestimates AOD (-17.3 %). Among the three machine learning models, the ERT model performed best, with a determination coefficient (R2) of 0.825 and the root-mean-square error (RMSE) of 0.174. Biomass burning/urban-industrial aerosols dominated China, with the largest contributions to southern, eastern, and central China in spring and summer. Clean continental aerosols contributed the most to southwestern China in fall and winter, whereas desert dust aerosols contributed the most to northwestern and eastern China in spring.
引用
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页数:11
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