Surprisingly robust photochemistry in subarctic particles during winter: evidence from photooxidants

Abstract. Subarctic cities notoriously experience severe winter pollution episodes with fine particle (PM2.5) concentrations above 35 µg m−3, the US Environmental Protection Agency (EPA) 24 h standard. While winter sources of primary particles in Fairbanks, Alaska, have been studied, the chemistry driving secondary particle formation is elusive. Biomass burning is a major source of wintertime primary particles, making the PM2.5 rich in light-absorbing brown carbon (BrC). When BrC absorbs sunlight, it produces photooxidants – reactive species potentially important for secondary sulfate and secondary organic aerosol formation – yet photooxidant measurements in high-latitude PM2.5 remain scarce. During the winter of 2022 Alaskan Layered Pollution And Chemical Analysis (ALPACA) field campaign in Fairbanks, we collected PM filters, extracted the filters into water, and exposed the extracts to simulated sunlight to characterize the production of three photooxidants: oxidizing triplet excited states of BrC, singlet molecular oxygen, and hydroxyl radical. Next, we used our measurements to model photooxidant production in highly concentrated aerosol liquid water. While conventional wisdom indicates photochemistry is limited during high-latitude winters, we find that BrC photochemistry is significant: we predict high triplet and singlet oxygen daytime particle concentrations up to 2×10-12 and 3×10-11 M, respectively, with moderate hydroxyl radical concentrations up to 5×10-15 M. Although our modeling predicts that triplets account for 0.4 %–10 % of daytime secondary sulfate formation, particle photochemistry cumulatively dominates, generating 76 % of daytime secondary sulfate formation, largely due to in-particle hydrogen peroxide, which contributes 25 %–54 %. Finally, we estimate triplet production rates year-round, revealing the highest rates in late winter when Fairbanks experiences severe pollution and in summer when wildfires generate BrC.

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Journal
Atmospheric chemistry and physics
Published
2025-08-29
DOI
https://doi.org/10.5194/acp-25-9561-2025
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
0.00

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article

Surprisingly robust photochemistry in subarctic particles during winter: evidence from photooxidants

Jingqiu Mao, William Robert Simpson, Sukriti Kapur, Anne Burns et al.
1 links
Atmospheric chemistry and physics
Atmospheric chemistry and aerosols
article

Surprisingly robust photochemistry in subarctic particles during winter: evidence from photooxidants

Jingqiu Mao, William Robert Simpson, Sukriti Kapur, Anne Burns, Jack E. Dibb, Allison Moon, Michael Oluwatoyin Sunday, James Campbell, Manabu Shiraiwa, Becky Alexander, J. Stutz, Meeta Cesler‐Maloney, Ting Fang, Laura Marie Dahler Heinlein, Fangzhou Guo, James Flynn, Junwei He, Kasey Edwards, Cort Anastasio
article en

Abstract

Abstract. Subarctic cities notoriously experience severe winter pollution episodes with fine particle (PM2.5) concentrations above 35 µg m−3, the US Environmental Protection Agency (EPA) 24 h standard. While winter sources of primary particles in Fairbanks, Alaska, have been studied, the chemistry driving secondary particle formation is elusive. Biomass burning is a major source of wintertime primary particles, making the PM2.5 rich in light-absorbing brown carbon (BrC). When BrC absorbs sunlight, it produces photooxidants – reactive species potentially important for secondary sulfate and secondary organic aerosol formation – yet photooxidant measurements in high-latitude PM2.5 remain scarce. During the winter of 2022 Alaskan Layered Pollution And Chemical Analysis (ALPACA) field campaign in Fairbanks, we collected PM filters, extracted the filters into water, and exposed the extracts to simulated sunlight to characterize the production of three photooxidants: oxidizing triplet excited states of BrC, singlet molecular oxygen, and hydroxyl radical. Next, we used our measurements to model photooxidant production in highly concentrated aerosol liquid water. While conventional wisdom indicates photochemistry is limited during high-latitude winters, we find that BrC photochemistry is significant: we predict high triplet and singlet oxygen daytime particle concentrations up to 2×10-12 and 3×10-11 M, respectively, with moderate hydroxyl radical concentrations up to 5×10-15 M. Although our modeling predicts that triplets account for 0.4 %–10 % of daytime secondary sulfate formation, particle photochemistry cumulatively dominates, generating 76 % of daytime secondary sulfate formation, largely due to in-particle hydrogen peroxide, which contributes 25 %–54 %. Finally, we estimate triplet production rates year-round, revealing the highest rates in late winter when Fairbanks experiences severe pollution and in summer when wildfires generate BrC.

Atmospheric chemistry and physicsVol. 25(16)
California Air Resources Board (US), University of Alaska Fairbanks (US), University of Louisville (US), University of New Hampshire (US), University of California, Los Angeles (US), Hong Kong University of Science and Technology (HK), University of Washington (US), University of California, Irvine (US), Aerodyne Research (US), University of Houston (US), University of California, Davis (US)
National Science Foundation, U.S. Department of Agriculture, New York State Department of Environmental Conservation, National Oceanic and Atmospheric Administration, University of California, Davis, University of California, Irvine, Division of Chemistry
Openalex Percentile: Top 72%
Atmospheric chemistry and aerosols
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