Light absorption enhancement of black carbon in a pyrocumulonimbus cloud

Payton Beeler, Joshin Kumar, Joshua P. Schwarz, Kouji Adachi, Laura Fierce, Anne E. Perring, J. M. Katich and Rajan K. Chakrabarty ()
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Payton Beeler: Washington University in St. Louis
Joshin Kumar: Washington University in St. Louis
Joshua P. Schwarz: National Oceanic and Atmospheric Administration (NOAA) Chemical Sciences Laboratory (CSL)
Kouji Adachi: Meteorological Research Institute
Laura Fierce: Pacific Northwest National Laboratory
Anne E. Perring: Colgate University
J. M. Katich: National Oceanic and Atmospheric Administration (NOAA) Chemical Sciences Laboratory (CSL)
Rajan K. Chakrabarty: Washington University in St. Louis

Nature Communications, 2024, vol. 15, issue 1, 1-7

Abstract: 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.

Date: 2024
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DOI: 10.1038/s41467-024-50070-0

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