|Title||Comparing black and brown carbon absorption from AERONET and surface measurements at wintertime Fresno|
|Publication Type||Journal Article|
|Year of Publication||2019|
|Authors||Chen S.J, Russell LM, Cappa CD, Zhang X.L, Kleeman M.J, Kumar A., Liu D., Ramanathana V.|
|Type of Article||Article|
|Keywords||Absorptive aerosol optical depth; aeronet; aerosol light-absorption; angstrom exponent; biomass; black carbon; boundary-layer; brown carbon; chemistry; combustion; Environmental Sciences & Ecology; fossil-fuel; Meteorology & Atmospheric Sciences; optical-properties; san-joaquin valley; single-scattering albedo; urban|
The radiative impacts of black carbon (BC) and brown carbon (BrC) are widely recognized but remain highly uncertain. The Aerosol Robotic Network (AERONET) provides measurements of aerosol optical depth (AOD), aerosol absorption optical depth (AAOD), and other parameters. AERONET AAOD measurements have been used to estimate the relative contributions of BC and BrC to the total absorption at select sites and have the potential to be used across the global network, but the accuracy of the partitioning method has not been established and the uncertainties not characterized. We made surface-level measurements of aerosol optical properties from January 13 to February 10, 2013, and from December 25, 2014, to January 13, 2015, at Fresno, California. The contribution of BrC and BC to the absorption at 405 nm was estimated from the surface-level measurements using a combined mass absorption coefficient and thermodenuder method. The surface-level measurements were compared with BC and BrC absorption at 440 nm estimated from AERONET measurements of the absolute AAOD and the absorption angstrom ngstrom exponent (AERONET-AAE method). In 2013, AERONET results showed that BC and BrC contributed 67% and 33%, respectively, of absorption at 440 nm while the surface-level measurements showed that BC and BrC contributed 89% and 11%, respectively, of absorption at 405 nm. In 2014, AERONET results showed BC and BrC absorption were 72% and 28%, respectively, and the BC and BrC surface measurements were 68% and 32%, respectively. The boundary layer conditions showed that the comparison between AERONET measurements and surface-based estimates was more appropriate in 2014 than in 2013. As a result, AERONET measurements and surface-based estimates had strong or moderate correlations and slopes near unity in 2014. Thus, surface measurements were more representative of column BC and BrC absorption in 2014.