Global changes in aerosol single scattering albedo during COVID-19

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dc.contributor.author Ansari, Kamran
dc.contributor.author Ramachandran, S.
dc.coverage.spatial United States of America
dc.date.accessioned 2024-06-27T12:49:35Z
dc.date.available 2024-06-27T12:49:35Z
dc.date.issued 2024-09
dc.identifier.citation Ansari, Kamran and Ramachandran, S., "Global changes in aerosol single scattering albedo during COVID-19", Atmospheric Environment, DOI: 10.1016/j.atmosenv.2024.120649, vol. 333, Sep. 2024.
dc.identifier.issn 1352-2310
dc.identifier.issn 1878-2442
dc.identifier.uri https://doi.org/10.1016/j.atmosenv.2024.120649
dc.identifier.uri https://repository.iitgn.ac.in/handle/123456789/10163
dc.description.abstract A comprehensive global investigation on the impact of reduction (changes) in aerosol emissions due to Coronavirus disease-2019 (COVID-19) lockdowns on aerosol single scattering albedo (SSA) utilizing satellite observations and model simulations is conducted for the first time. The absolute change in Ozone Monitoring Instrument (OMI) retrieved, and two highly-spatially resolved models (Modern-Era Retrospective Analysis for Research and Applications-2 (MERRA-2) and Copernicus Atmosphere Monitoring Service (CAMS)) simulated SSA is <4% (<0.04–0.05) globally during COVID (2020) compared to normal (2015–2019) period. Change in SSA during COVID is not significantly different from long-term and year-to-year variability in SSA. A small change in SSA indicates that significant reduction in anthropogenic aerosol emissions during COVID-19 induced lockdowns has a negligible effect in changing the net contribution of aerosol scattering and/or absorption to total aerosol extinction. The changes in species-wise aerosol optical depth (AOD) are examined in detail to explain the observed changes in SSA. Model simulations show that total AOD decreased during COVID-19 lockdowns, consistent with satellite observations. The respective contributions of sulfate and black carbon (BC) to total AOD increased, which resulted in a negligible change in SSA during the spring and summer seasons of COVID over South Asia. Europe and North America experience a small increase in SSA (<2%) during the summer season of COVID due to a decrease in BC contribution. The change in SSA (2%) is the same for a small change in BC AOD contribution (3%), and for a significant change in sulfate AOD contribution (20%) to total AOD. Since, BC SSA is 5-times lower (higher absorption) than that of sulfate SSA, the change in SSA remains the same. For a significant change in SSA to occur, the BC AOD contribution needs to be changed significantly (4–5 times) compared to other aerosol species. A sensitivity analysis reveals that change in aerosol radiative forcing during COVID is primarily dependent on change in AOD rather than SSA. These quantitative findings can be useful to devise more suitable future global and regional mitigation strategies aimed at regulating aerosol emissions to reduce environmental impacts, air pollution, and public health risks.
dc.description.statementofresponsibility by Kamran Ansari and S. Ramachandran
dc.format.extent vol. 333
dc.language.iso en_US
dc.publisher Elsevier
dc.title Global changes in aerosol single scattering albedo during COVID-19
dc.type Article
dc.relation.journal Atmospheric Environment


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