Effects of mixing state on optical and radiative properties of black carbon in the European Arctic

• Published in: Atmospheric Chemistry and Physics
• Main Authors: Zanatta, Marco, Laj, Paolo, Gysel, Martin, Baltensperger, Urs, Vratolis, Stergios, Eleftheriadis, Konstantinos, Kondo, Yutaka, Dubuisson, Philippe, Winiarek, Victor, Kazadzis, Stelios, Tunved, Peter, Jacobi, Hans-Werner
• Other Authors: Institut des Géosciences de l’Environnement (IGE), Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ), Paul Scherrer Institute (PSI), National Centre for Scientific Research Demokritos, Laboratoire d’Optique Atmosphérique - UMR 8518 (LOA), Institut national des sciences de l'Univers (INSU - CNRS)-Université de Lille-Centre National de la Recherche Scientifique (CNRS), Institute for Applied Environmental Research Stockholm, Stockholm University
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2018
• Subjects: [SDU.OCEAN]Sciences of the Universe [physics]/Ocean; Atmosphere; Arctic; black carbon
• Online Access: https://hal.archives-ouvertes.fr/hal-02341852; https://hal.archives-ouvertes.fr/hal-02341852/document; https://hal.archives-ouvertes.fr/hal-02341852/file/acp-18-14037-2018.pdf; https://doi.org/10.5194/acp-18-14037-2018

International audience Atmospheric aging promotes internal mixing of black carbon (BC), leading to an enhancement of light absorption and radiative forcing. The relationship between BC mixing state and consequent absorption enhancement was never estimated for BC found in the Arctic region. In the present work, we aim to quantify the absorption enhancement and its impact on radiative forcing as a function of mi-crophysical properties and mixing state of BC observed in situ at the Zeppelin Arctic station (78 • N) in the spring of 2012 during the CLIMSLIP (Climate impacts of short-lived pollutants in the polar region) project. Single-particle soot photometer (SP2) measurements showed a mean mass concentration of refractory black carbon (rBC) of 39 ng m −3 , while the rBC mass size distribution was of lognormal shape, peaking at an rBC mass-equivalent diameter (D rBC) of around 240 nm. On average, the number fraction of particles containing a BC core with D rBC >80 nm was less than 5 % in the size range (overall optical particle diameter) from 150 to 500 nm. The BC cores were internally mixed with other particulate matter. The median coating thickness of BC cores with 220 nm < D rBC < 260 nm was 52 nm, resulting in a core-shell diameter ratio of 1.4, assuming a coated sphere morphology. Combining the aerosol absorption coefficient observed with an Aethalometer and the rBC mass concentration from the SP2, a mass absorption cross section (MAC) of 9.8 m 2 g −1 was inferred at a wavelength of 550 nm. Consistent with direct observation, a similar MAC value (8.4 m 2 g −1 at 550 nm) was obtained indirectly by using Mie theory and assuming a coated-sphere morphology with the BC mixing state constrained from the SP2 measurements. According to these calculations, the lens-ing effect is estimated to cause a 54 % enhancement of the MAC compared to that of bare BC particles with equal BC core size distribution. Finally, the ARTDECO radiative transfer model was used to estimate the sensitivity of the radiative balance ...