2024
DOI: 10.1029/2023gl107273
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Airborne Observations Constrain Heterogeneous Nitrogen and Halogen Chemistry on Tropospheric and Stratospheric Biomass Burning Aerosol

Zachary C. J. Decker,
Gordon A. Novak,
Kenneth Aikin
et al.

Abstract: Heterogeneous chemical cycles of pyrogenic nitrogen and halides influence tropospheric ozone and affect the stratosphere during extreme Pyrocumulonimbus (PyroCB) events. We report field‐derived N2O5 uptake coefficients, γ(N2O5), and ClNO2 yields, φ(ClNO2), from two aircraft campaigns observing fresh smoke in the lower and mid troposphere and processed/aged smoke in the upper troposphere and lower stratosphere (UTLS). Derived φ(ClNO2) varied across the full 0–1 range but was typically <0.5 and smallest in a … Show more

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Cited by 1 publication
(2 citation statements)
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“…Cl chemistry is expected to be a minor atmospheric loss process for furanoids, and Cl mixing ratios in smoke are generally low. 153 However, additional room-temperature, and pressure-dependent kinetic studies would provide further insight into furanoid atmospheric degradation mechanisms and the contribution of the H atom abstraction pathway to the overall rate coefficient.…”
Section: Acs Earth Andmentioning
confidence: 99%
See 1 more Smart Citation
“…Cl chemistry is expected to be a minor atmospheric loss process for furanoids, and Cl mixing ratios in smoke are generally low. 153 However, additional room-temperature, and pressure-dependent kinetic studies would provide further insight into furanoid atmospheric degradation mechanisms and the contribution of the H atom abstraction pathway to the overall rate coefficient.…”
Section: Acs Earth Andmentioning
confidence: 99%
“…The Cl atmospheric degradation of furanoids is not expected to be a significant tropospheric loss, though the detection of chlorinated compounds may serve as tracers for this chemistry . There are a few studies that have reported gas-phase products and proposed reaction mechanisms for Cl-addition and H-abstraction pathways. ,,, All studies have been performed at room-temperature (296 ± 2 K) and atmospheric-pressure (1000 ± 20 mbar) conditions in smog chambers.…”
Section: Gas-phase Tropospheric Degradation Of Furanoidsmentioning
confidence: 99%