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Airborne measurement of OH reactivity during INTEX-B

TLDR
In the second phase of the International Chemical Transport Experiment-B (INTEX-B) campaign as discussed by the authors, a new airborne OH reactivity instrument was designed and deployed for the first time on the NASA DC-8 aircraft, which was focused on the Asian pollution outflow over Pacific Ocean and was based in Hawaii and Alaska.
Abstract
. The measurement of OH reactivity, the inverse of the OH lifetime, provides a powerful tool to investigate atmospheric photochemistry. A new airborne OH reactivity instrument was designed and deployed for the first time on the NASA DC-8 aircraft during the second phase of Intercontinental Chemical Transport Experiment-B (INTEX-B) campaign, which was focused on the Asian pollution outflow over Pacific Ocean and was based in Hawaii and Alaska. The OH reactivity was measured by adding OH, generated by photolyzing water vapor with 185 nm UV light in a moveable wand, to the flow of ambient air in a flow tube and measuring the OH signal with laser induced fluorescence. As the wand was pulled back away from the OH detector, the OH signal decay was recorded; the slope of −Δln(signal)/Δ time was the OH reactivity. The overall absolute uncertainty at the 2σ confidence levels is about 1 s−1 at low altitudes (for decay about 6 s−1), and 0.7 s−1 at high altitudes (for decay about 2 s−1). From the median vertical profile obtained in the second phase of INTEX-B, the measured OH reactivity (4.0±1.0 s−1) is higher than the OH reactivity calculated from assuming that OH was in steady state (3.3&plusmn0.8 s−1), and even higher than the OH reactivity that was calculated from the total measurements of all OH reactants (1.6±0.4 s−1). Model calculations show that the missing OH reactivity is consistent with the over-predicted OH and under-predicted HCHO in the boundary layer and lower troposphere. The over-predicted OH and under-predicted HCHO suggest that the missing OH sinks are most likely related to some highly reactive VOCs that have HCHO as an oxidation product.

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Atmospheric composition change – global and regional air quality

Paul S. Monks, +68 more
TL;DR: A review of the state of scientific understanding in relation to global and regional air quality is outlined in this article, in terms of emissions, processing and transport of trace gases and aerosols.
Journal ArticleDOI

Tropospheric OH and HO2 radicals: field measurements and model comparisons.

TL;DR: This critical review discusses field measurements of local concentrations of OH and HO(2) radicals in the troposphere, and in particular the comparisons that have been made with numerical model calculations containing a detailed chemical mechanism.

An Overview of MILAGRO 2006 Campaign: Mexico City Emissions and their Transport and Transformation

Luisa Molina
TL;DR: The Mexico City Metropolitan Area (MCMA) was selected as the case study to characterize the sources, concentrations, transport, and transformation processes of the gases and fine particles emitted to the MCMA atmosphere and to evaluate the regional and global impacts of these emissions.
Journal ArticleDOI

Laboratory studies of the chemical composition and cloud condensation nuclei (CCN) activity of secondary organic aerosol (SOA) and oxidized primary organic aerosol (OPOA)

TL;DR: In this paper, secondary organic aerosol (SOA) and oxidized OPOA were generated via controlled exposure of precursors to OH radicals and/or O 3 in a potential aerosol mass (PAM) flow reactor over timescales equivalent to 1-20 days of atmospheric aging.
References
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Journal ArticleDOI

Evaluated kinetic and photochemical data for atmospheric chemistry

TL;DR: A critical evaluation of the kinetics and photochemistry of gas phase chemical reactions of neutral species involved in middle atmosphere chemistry (10-55 km altitude) was carried out by the authors under the auspices of the CODATA Task Group on Chemical Kinetics.
Journal ArticleDOI

Missing OH reactivity in a forest: evidence for unknown reactive biogenic VOCs.

TL;DR: In a northern Michigan forest, the direct measurement of total OH reactivity, which is the inverse of the OH lifetime, was significantly greater than expected, consistent with the hypothesis that unknown reactive BVOCs, perhaps terpenes, provide the missingOH reactivity.
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