The CALIPSO retrieved spatiotemporal and vertical distributions of AOD and extinction coefficient for different aerosol types during 2007–2019: A recent perspective over global and regional scales. (1st April 2022)

• Record Type: Journal Article
• Authors: Pan, Honglin; Huang, Jianping; Kumar, Kanike Raghavendra; An, Linli; Zhang, Jinxia
• Is Part Of: Atmospheric environment. Volume 274(2022)
• Publication Date: 2022-04-01
• Subjects: CALIPSO -- AOD -- Extinction coefficient -- Aerosol types -- Spatiotemporal and vertical distributions; Air -- Pollution -- Periodicals; Air -- Pollution -- Meteorological aspects -- Periodicals; 551.51
• DOI: 10.1016/j.atmosenv.2022.118986
• Languages: English
• ISSNs: 1352-2310

Abstract

Abstract: In the present study, we investigated the global climatology of the spatiotemporal and vertical distributions of aerosol optical properties for different aerosol types, mainly including total aerosols (All), desert dust (DD), polluted dust (PD), and elevated smoke (ES). The data used for the study is derived from the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) for Research and Application. We found that the seasonal distribution of the global mean aerosol optical depth (AOD) of All type in the land area are in the order JJA (0.157) > MAM (0.134) > DJF (0.127) > SON (0.124). This is attributed to the more frequent sand and dust activities over the Taklimakan Desert and the Sahara Desert in MAM and JJA. Owing to the transportation of DD, ES, and PD from the aerosol source, the ocean areas (especially for downwind regions) present the high AOD, and with the same seasonal distribution trend as in the land area. Also, the mean extinction coefficient (EC) for all aerosols decreases with the increase of height in all seasons for both hemispheres. The maximum mean EC for All aerosols is 0.0102 km −1 (0.016 km −1 ) during the day (night) in DJF (JJA) in the northern hemisphere, while the maximum is 0.006 km −1 (0.008 km −1 ) during the day (night) in JJA (SON) in the southern hemisphere. Also, the occurrence of frequencies of DD, PD, and ES aerosols are distributed throughout the entire troposphere in all seasons, but the clean marine (CM) and polluted continent (PC) are mostly below 3 km. Graphical abstract: Image 1 Highlights: The CALIPSO retrieved global AOD for all aerosol types showed a maximum in summer. The spatiotemporal changes in AOD were observed for all types of aerosols. The biggest difference in total AOD between land and ocean areas occurred in summer. Annual variations of AOD are relatively stable for all aerosol types.