Abstract

Abstract. We present an analysis of ozone (O3) photochemistry observed by aircraft measurements of boreal biomass burning plumes over eastern Canada in the summer of 2011. Measurements of O3 and a number of key chemical species associated with O3 photochemistry, including non-methane hydrocarbons (NMHCs), nitrogen oxides (NOx) and total nitrogen containing species (NOy), were made from the UK FAAM BAe-146 research aircraft as part of the "quantifying the impact of BOReal forest fires on Tropospheric oxidants over the Atlantic using Aircraft and Satellites" (BORTAS) experiment between 12 July and 3 August 2011. The location and timing of the aircraft measurements put BORTAS into a unique position to sample biomass burning plumes from the same source region in Northwestern Ontario with a range of ages. We found that O3 mixing ratios measured in biomass burning plumes were indistinguishable from non-plume measurements, but evaluating them in relationship to measurements of carbon monoxide (CO), total alkyl nitrates (ΣAN) and the surrogate species NOz (= NOy-NOx) revealed that the potential for O3 production increased with plume age. We used NMHC ratios to estimate photochemical ages of the observed biomass burning plumes between 0 and 10 days. The BORTAS measurements provided a wide dynamic range of O3 production in the sampled biomass burning plumes with ΔO3/ΔCO enhancement ratios increasing from 0.020 ± 0.008 ppbv ppbv−1 in plumes with photochemical ages less than 2 days to 0.55 ± 0.29 ppbv ppbv−1 in plumes with photochemical ages greater than 5 days. We found that the main contributing factor to the variability in the ΔO3/ΔCO enhancement ratio was ΔCO in plumes with photochemical ages less than 4 days, and that was a transition to ΔO3 becoming the main contributing factor in plumes with ages greater than 4 days. In comparing O3 mixing ratios with components of the NOy budget, we observed that plumes with ages between 2 and 4 days were characterised by high aerosol loading, relative humidity greater than 40%, and low ozone production efficiency (OPE) of 7.7 ± 3.5 ppbv ppbv−1 relative to ΣAN and 1.6 ± 0.9 ppbv ppbv−1 relative to NOz. In plumes with ages greater than 4 days, OPE increased to 472 ± 28 ppbv ppbv−1 relative to ΣAN and 155 ± 5 ppbv ppbv−1 relative to NOz. From the BORTAS measurements we estimated that aged plumes with low aerosol loading were close to being in photostationary steady state and O3 production in younger plumes was inhibited by high aerosol loading and greater production of ΣAN relative to O3. The BORTAS measurements of O3 photochemistry in boreal biomass burning plumes were found to be consistent with previous summertime aircraft measurements made over the same region during the Arctic Research of the Composition of the Troposphere (ARCTAS-B) in 2008 and Atmospheric Boundary Layer Experiment (ABLE 3B) in 1990.

Highlights

  • The quantifying the impact of BOReal forest fires on Tropospheric oxidants over the Atlantic using Aircraft and Satellites (BORTAS) experiment was conducted in two phases: July–August 2010 and 2011 (Palmer et al, 2013)

  • We found that O3 mixing ratios measured in biomass burning plumes were indistinguishable from nonplume measurements, but evaluating them in relationship to measurements of carbon monoxide (CO), total alkyl nitrates ( AN) and the surrogate species NOz (= NOy − nitrogen oxides (NOx)) revealed that the potential for O3 production increased with plume age

  • We have presented an analysis of O3 photochemistry from in situ aircraft measurements made in boreal biomass burning plumes from a synthesis of aircraft measurements made www.atmos-chem-phys.net/13/7321/2013/

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Summary

Introduction

The quantifying the impact of BOReal forest fires on Tropospheric oxidants over the Atlantic using Aircraft and Satellites (BORTAS) experiment was conducted in two phases: July–August 2010 (phase A) and 2011 (phase B) (Palmer et al, 2013). A number of previous measurement campaigns have made in situ observations of photochemistry within boreal biomass burning outflow and evaluated the associated O3 production and loss. Mauzerall et al (1996) performed 1-D model simulations to calculate in situ production and loss of O3 based on the ABLE 3B measurements in the summer of 1990 They found biomass burning emissions to be a relatively negligible, contributing less than 2 % to the calculated O3 budget. Pfister et al (2006) utilised the MOZART-4 CTM to evaluate O3 production in the outflow from fires in Alaska during summer of 2004 with measurements made from aircraft during the ICARTT campaign and at the Pico Mountain Observatory Peroxy radicals are subject to reaction with NO and can follow two different pathways: RO2 + NO → RO + NO2

Plume photochemistry
BORTAS measurements
Observed O3 distribution over eastern Canada
Observed boreal biomass burning outflow
O3 enhancements in biomass burning plumes
O3 photochemistry in boreal biomass burning outflow
Ozone production efficiency
Comparison of O3 photochemistry from BORTAS and previous campaigns
Findings
Conclusions
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