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Long-term spatiotemporal variations of aerosol optical depth over Yellow and Bohai Sea
- Shen, Xiaojing, Bilal, Muhammad, Qiu, Zhongfeng, Sun, Deyong, Wang, Shengqiang, Zhu, Weijun
- Environmental science and pollution research international 2019 v.26 no.8 pp. 7969-7979
- aerosols, algorithms, autumn, biomass, dust, moderate resolution imaging spectroradiometer, optical properties, sediments, spatial variation, summer, temporal variation, winter, Yellow Sea
- In this study, MODerate resolution Imaging Spectroradiometer (MODIS) Collection 6.1 (C6.1) level-2 Dark Target (DT) Aerosol Optical Depth (AOD) observations at 550 nm (AOD₅₅₀) for the highest quality flag assurance (QA = 3) were obtained to analyze spatiotemporal variations of aerosol optical properties over the Yellow and the Bohai Sea from 2002 to 2017. Spectral AOD observations at 470 nm (AOD₄₇₀) and 660 nm (AOD₆₆₀) were obtained to calculate Angstrom Exponent (AE₄₇₀–₆₆₀) and classify the aerosol types including clean continental (CC), clean maritime (CM) biomass and urban industrial (BUI), dust (D), and mixed (MXD) aerosol types. Results showed a very distinct spatial pattern of AOD distribution over the Bohai Sea which looks suspicious, i.e., high aerosol loadings (AOD > 0.8) throughout the entire time period, whereas relative low AOD distribution was observed over the adjacent land pixels especially in autumn and winter, which suggested that the DT algorithm might be influenced by a large number of sediments located in the Bohai Sea. Significant differences in spatial distributions were found in different seasons in terms of area coverage as a maximum number of pixels were available during autumn, and regional high and low aerosol loadings were observed during autumn and summer, respectively. Trend analysis from 2002 to 2017 showed that AOD was increased up to 0.04 over the Bohai Sea and decreased up to 0.04 over the Yellow Sea, and this trend varies from month to month. Aerosol classification showed significant contributions of BUI and CC over the region, and contributions of CM, DUST, and MXD aerosols over the Yellow Sea were relatively high compared to the Bohai Sea.