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Updated: Jul 19, 2025

Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements
Published on: September 7, 2019
Shortwave absorption by wildfire smoke dominated by dark brown carbon
Rajan K Chakrabarty1, Nishit J Shetty1, Arashdeep S Thind2
1Center for Aerosol Science and Engineering, Department of Energy, Environmental, and Chemical Engineering, Washington University in St Louis, St Louis, MO USA.
Wildfire smoke contains a resilient type of brown carbon that absorbs sunlight, contributing significantly to atmospheric warming. This finding necessitates revisions to climate models for accurate radiative forcing estimations.
Area of Science:
- Atmospheric Chemistry
- Climate Science
- Aerosol Science
Background:
- Wildfires release black carbon and brown carbon, impacting Earth's radiation budget.
- Brown carbon's warming effect is uncertain due to assumed photochemical bleaching, leading to poor climate model representation.
Purpose of the Study:
- To quantify shortwave absorption by wildfire smoke aerosols.
- To investigate the properties and atmospheric processing of brown carbon in wildfire plumes.
Main Methods:
- Measurements of ensemble-scale and particle-scale shortwave absorption in western US wildfire smoke plumes.
- Analysis of brown carbon's optical properties, including water insolubility and photobleaching resistance.
Main Results:
- A specific dark brown carbon type accounts for significant short (75%) and long (50%) visible light absorption.
- This brown carbon is water insoluble, resists daytime photobleaching, and its absorptivity increases with nighttime processing.
Conclusions:
- Brown carbon's radiative impact is substantial and more persistent than previously assumed.
- Current climate model parameterizations for brown carbon require updates to accurately estimate smoke aerosol radiative forcing and warming potential.
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