| Literature DB >> 35136274 |
Miguel Ricardo A Hilario1, Ewan Crosbie2,3, Paola Angela Bañaga4,5, Grace Betito4,5, Rachel A Braun6,7, Maria Obiminda Cambaliza4,5, Andrea F Corral6, Melliza Templonuevo Cruz4,8, Jack E Dibb9, Genevieve Rose Lorenzo1, Alexander B MacDonald6, Claire E Robinson2,3, Michael A Shook2, James Bernard Simpas4,5, Connor Stahl6, Edward Winstead2,3, Luke D Ziemba2, Armin Sorooshian1,6.
Abstract
Leveraging aerosol data from multiple airborne and surface-based field campaigns encompassing diverse environmental conditions, we calculate statistics of the oxalate-sulfate mass ratio (median: 0.0217; 95% confidence interval: 0.0154-0.0296; R = 0.76; N = 2,948). Ground-based measurements of the oxalate-sulfate ratio fall within our 95% confidence interval, suggesting the range is robust within the mixed layer for the submicrometer particle size range. We demonstrate that dust and biomass burning emissions can separately bias this ratio toward higher values by at least one order of magnitude. In the absence of these confounding factors, the 95% confidence interval of the ratio may be used to estimate the relative extent of aqueous processing by comparing inferred oxalate concentrations between air masses, with the assumption that sulfate primarily originates from aqueous processing.Entities:
Year: 2021 PMID: 35136274 PMCID: PMC8819676 DOI: 10.1029/2021gl096520
Source DB: PubMed Journal: Geophys Res Lett ISSN: 0094-8276 Impact factor: 4.720