Removal of NOx and NOy in biomass burning plumes in the boundary layer over northern Australia

The Biomass Burning and Lightning Experiment Phase B (BIBLE‐B) aircraft measurement campaign was conducted over the western Pacific and Australia in August and September 1999. In situ aircraft measurements of carbon monoxide (CO), nitric oxide (NO), total reactive nitrogen (NOy), ozone (O3), nonmeth...

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Veröffentlicht in:Journal of Geophysical Research: Atmospheres 2003-05, Vol.108 (D10), p.ACH2.1-n/a
Hauptverfasser: Takegawa, N., Kondo, Y., Koike, M., Ko, M., Kita, K., Blake, D. R., Nishi, N., Hu, W., Liley, J. B., Kawakami, S., Shirai, T., Miyazaki, Y., Ikeda, H., Russel-Smith, J., Ogawa, T.
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container_end_page n/a
container_issue D10
container_start_page ACH2.1
container_title Journal of Geophysical Research: Atmospheres
container_volume 108
creator Takegawa, N.
Kondo, Y.
Koike, M.
Ko, M.
Kita, K.
Blake, D. R.
Nishi, N.
Hu, W.
Liley, J. B.
Kawakami, S.
Shirai, T.
Miyazaki, Y.
Ikeda, H.
Russel-Smith, J.
Ogawa, T.
description The Biomass Burning and Lightning Experiment Phase B (BIBLE‐B) aircraft measurement campaign was conducted over the western Pacific and Australia in August and September 1999. In situ aircraft measurements of carbon monoxide (CO), nitric oxide (NO), total reactive nitrogen (NOy), ozone (O3), nonmethane hydrocarbons (NMHCs), and other species were made during BIBLE‐B. Meteorological analysis shows that the trace gases emitted from biomass burning in northern Australia were mostly confined within the planetary boundary layer (below ∼3 km) by strong subsidence in the free troposphere. Removal processes of NOx (equal to measured NO + calculated NO2) and NOy in biomass burning plumes in the boundary layer are examined on the basis of correlation analysis. The photochemical lifetime of NOx in biomass burning plumes during the daytime is estimated to be 0.1 to 0.3 days using the correlations of NOx with short‐lived NMHCs and hydroxyl radical (OH) concentration calculated from a constrained photochemical model. Correlation of NOy with CO shows that ∼60% of the NOy molecules originating from biomass burning were removed in the boundary layer within 2–3 days. This result is consistent with dry deposition of nitric acid (HNO3) in the plumes. It is likely that only a small fraction of NOy emitted from biomass burning was exported from the boundary layer to the free troposphere during the BIBLE‐B period.
doi_str_mv 10.1029/2002JD002505
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Removal processes of NOx (equal to measured NO + calculated NO2) and NOy in biomass burning plumes in the boundary layer are examined on the basis of correlation analysis. The photochemical lifetime of NOx in biomass burning plumes during the daytime is estimated to be 0.1 to 0.3 days using the correlations of NOx with short‐lived NMHCs and hydroxyl radical (OH) concentration calculated from a constrained photochemical model. Correlation of NOy with CO shows that ∼60% of the NOy molecules originating from biomass burning were removed in the boundary layer within 2–3 days. This result is consistent with dry deposition of nitric acid (HNO3) in the plumes. 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It is likely that only a small fraction of NOy emitted from biomass burning was exported from the boundary layer to the free troposphere during the BIBLE‐B period.</description><subject>biomass burning</subject><subject>Chemical composition and interactions. 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subjects biomass burning
Chemical composition and interactions. Ionic interactions and processes
dry deposition of NOy
Earth, ocean, space
Exact sciences and technology
External geophysics
Meteorology
northern Australia
NOx lifetime
title Removal of NOx and NOy in biomass burning plumes in the boundary layer over northern Australia
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