Spatiotemporal relationship between Himawari-8 hourly columnar aerosol optical depth (AOD) and ground-level PM 2.5 mass concentration in mainland China

Himawari-8 aerosol products have been widely used to estimate the near-surface hourly PM concentrations due to the high temporal resolution. However, most studies focus on the evaluation model. As the foundation of the estimation, the relationship between near-surface PM and columnar aerosol optical...

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Bibliographic Details
Published inThe Science of the total environment Vol. 765; p. 144241
Main Authors Xu, Qiangqiang, Chen, Xiaoling, Yang, Shangbo, Tang, Linling, Dong, Jiadan
Format Journal Article
LanguageEnglish
Published Netherlands 15.04.2021
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Summary:Himawari-8 aerosol products have been widely used to estimate the near-surface hourly PM concentrations due to the high temporal resolution. However, most studies focus on the evaluation model. As the foundation of the estimation, the relationship between near-surface PM and columnar aerosol optical depth (AOD) has not been comprehensively investigated. In this study, we investigate the relationship between PM and advanced Himawari imager (AHI) AOD for 2016-2018 across mainland China on different spatial and temporal scales and the factors affecting the association. We calculated the Pearson correlation coefficients and the PM /AOD ratio as the analysis indicators in 345 cities and 14 urban agglomerations based on the collocations of PM and AHI AOD. From 9:00 to 17:00 local time, the PM -AOD correlation become significantly stronger while The PM /AOD ratio markedly decrease in Beijing-Tianjin-Hebei, Yangtze River Delta, and Chengyu regions. The strongest correlation is between 12:00 and 14:00 LT (at noon) and between 13:00 and 17:00 LT (afternoon), respectively. The ratio in a day shows an obvious unimodal mode, and the peak occurred at around 10:00 or 11:00 LT, especially in autumn and winter. There is a pronounced variation of the PM -AOD relationship in a week during the winter. Moreover, there are the strongest correlation and the largest ratio for most urban agglomerations during the winter. We also find that PM and AOD are not always correlated under different meteorological conditions and precursor concentrations. Furthermore, for the scattering-dominated fine-mode aerosol, there is a high correlation and a low ratio between PM and AOD. The correlation between PM and AHI AOD significantly increases with increasing the number of AOD retrievals on a day. The findings will provide meaningful information and important implications for satellite retrieval of hourly PM concentration and its exposure estimation in China, especially in some urban agglomerations.
ISSN:1879-1026