Exploring the factors responsible for aerosol asymmetric trends over Indo-Gangetic Plain using remote sensing observations

• Published in: Journal of atmospheric and solar-terrestrial physics 2024-05, Vol.258, p.106220, Article 106220
• Main Authors: Shukla, Krishna Kumar, Attada, Raju, Sarangi, Chandan, Kunchala, Ravi Kumar, Devulapalli, Venkata Phanikumar
• Format: Article
• Language: English
• Subjects: Aerosol optical depth; Black carbon; Dust; Indo-gangetic plain
• ISSN: 1364-6826; 1879-1824
• DOI: 10.1016/j.jastp.2024.106220

The present study investigates the influencing factors responsible for the asymmetry in aerosol optical depth (AOD) trends using long-term datasets (2003–2019) over western and eastern Indo-Gangetic Plain (IGP) regions during the pre-monsoon season. Analysis from Modern-Era Retrospective Analysis for Research and Applications Version-2 (MERRA-2) for different aerosols illustrates that dust aerosols dominate over the western IGP (W-IGP), while sulphate and carbonaceous aerosols (black carbon (BC) and organic carbon (OC)) majorly contributed to the total AOD over the eastern IGP (E-IGP). Our study reveals a significant decline in AOD over the W-IGP, while a rising trend over E-IGP from Moderate Resolution Imaging Spectroradiometer (MODIS) satellite observations. A dipole pattern in AOD trends over IGP indicates the aerosol loading from combined effects of various natural and anthropogenic emissions under favourable meteorological conditions over the W-IGP and E-IGP, respectively. Furthermore, the declining AOD trend over W-IGP is mainly attributed to increased pre-monsoonal rainfall, which supports the wet deposition, increases soil moisture, thus reducing soil erodibility, and correlates strongly with meteorological factors. The rising AOD trend over the E-IGP appears to be influenced by increased anthropogenic emissions (i.e., BC, OC, and sulphate) from the industrialization of the region, decreased rainfall, and enhanced westerly-induced advection of aerosols from W-IGP. Our study indicates that the regional meteorological variables and anthropogenic sources influence changes in the AOD trends over the IGP region. •A dipole pattern in AOD trends is noticed over western and eastern IGP.•The W-IGP has more contribution from natural aerosols, whereas E-IGP dominate regionally emitted anthropogenic aerosols.•Regional meteorology and circulation pattern play an essential role in the AOD dipole pattern over IGP.