Description
Summary:Long-term measurements of the mass concentration of black carbon (BC) in the atmosphere ( M BC ) with well-constrained accuracy are indispensable to quantify its emission, transport, and deposition. The aerosol light absorption coefficient ( b abs ), usually measured by a filter-based absorption photometer, including an Aethalometer (AE), is often used to estimate M BC . The measured b abs is converted to M BC by assuming a value for the mass absorption cross section (MAC). Previously, we derived the MAC for AE (MAC (AE)) from measured b abs and independently measured M BC values at two sites in the Arctic. M BC was measured with a filter-based absorption photometer with a heated inlet (COSMOS). The accuracy of the COSMOS-derived M BC ( M BC (COSMOS)) was within about 15%. Here, we obtained additional MAC (AE) measurements to improve understanding of its variability and uncertainty. We measured b abs (AE) and M BC (COSMOS) at Alert (2018–2020), Barrow (2012–2022), Ny-Ålesund (2012–2019), and Pallas ...