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Radiative absorption enhancements due to the mixing state of atmospheric black carbon
Authors:Christopher D Cappa  Timothy B Onasch  Paola Massoli  Douglas R Worsnop  Timothy S Bates  Eben S Cross  Paul Davidovits  Jani Hakala  Katherine L Hayden  B Tom Jobson  Katheryn R Kolesar  Daniel A Lack  Brian M Lerner  Shao-Meng Li  Daniel Mellon  Ibraheem Nuaaman  Jason S Olfert  Tuukka Petäjä  Patricia K Quinn  Chen Song  R Subramanian  Eric J Williams  Rahul A Zaveri
Institution:Department of Civil and Environmental Engineering, University of California, Davis, CA 95616, USA. cdcappa@ucdavis.edu
Abstract:Atmospheric black carbon (BC) warms Earth's climate, and its reduction has been targeted for near-term climate change mitigation. Models that include forcing by BC assume internal mixing with non-BC aerosol components that enhance BC absorption, often by a factor of ~2; such model estimates have yet to be clearly validated through atmospheric observations. Here, direct in situ measurements of BC absorption enhancements (E(abs)) and mixing state are reported for two California regions. The observed E(abs) is small-6% on average at 532 nm-and increases weakly with photochemical aging. The E(abs) is less than predicted from observationally constrained theoretical calculations, suggesting that many climate models may overestimate warming by BC. These ambient observations stand in contrast to laboratory measurements that show substantial E(abs) for BC are possible.
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