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Light absorption enhancement of black carbon in a pyrocumulonimbus cloud.
Beeler, Payton; Kumar, Joshin; Schwarz, Joshua P; Adachi, Kouji; Fierce, Laura; Perring, Anne E; Katich, J M; Chakrabarty, Rajan K.
  • Beeler P; Center for Aerosol Science and Engineering, Department of Energy, Environmental and Chemical Engineering, Washington University in St. Louis, St. Louis, MO, USA.
  • Kumar J; Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, WA, USA.
  • Schwarz JP; Center for Aerosol Science and Engineering, Department of Energy, Environmental and Chemical Engineering, Washington University in St. Louis, St. Louis, MO, USA.
  • Adachi K; National Oceanic and Atmospheric Administration (NOAA) Chemical Sciences Laboratory (CSL), Boulder, CO, USA.
  • Fierce L; Department of Atmosphere, Ocean and Earth System Modelling Research, Meteorological Research Institute, Tsukuba, Japan.
  • Perring AE; Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, WA, USA.
  • Katich JM; Department of Chemistry, Colgate University, Hamilton, NY, USA.
  • Chakrabarty RK; Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA.
Nat Commun ; 15(1): 6243, 2024 Jul 25.
Article en En | MEDLINE | ID: mdl-39054319
ABSTRACT
Pyrocumulonimbus (pyroCb) firestorm systems have been shown to inject significant amounts of black carbon (BC) to the stratosphere with a residence time of several months. Injected BC warms the local stratospheric air, consequently perturbing transport and hence spatial distributions of ozone and water vapor. A distinguishing feature of BC-containing particles residing within pyroCb smoke is their thick surface coatings made of condensed organic matter. When coated with non-refractory materials, BC's absorption is enhanced, yet the absorption enhancement factor (Eabs) for pyroCb BC is not well constrained. Here, we perform particle-scale measurements of BC mass, morphology, and coating thickness from inside a pyroCb cloud and quantify Eabs using an established particle-resolved BC optics model. We find that the population-averaged Eabs for BC asymptotes to 2.0 with increasing coating thickness. This value denotes the upper limit of Eabs for thickly coated BC in the atmosphere. Our results provide observationally constrained parameterizations of BC absorption for improved radiative transfer calculations of pyroCb events.