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 |
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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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R. ; Nishi, N. ; Hu, W. ; Liley, J. B. ; Kawakami, S. ; Shirai, T. ; Miyazaki, Y. ; Ikeda, H. ; Russel-Smith, J. ; Ogawa, T.</creator><creatorcontrib>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.</creatorcontrib><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.</description><identifier>ISSN: 0148-0227</identifier><identifier>EISSN: 2156-2202</identifier><identifier>DOI: 10.1029/2002JD002505</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>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</subject><ispartof>Journal of Geophysical Research: Atmospheres, 2003-05, Vol.108 (D10), p.ACH2.1-n/a</ispartof><rights>Copyright 2003 by the American Geophysical Union.</rights><rights>2003 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2002JD002505$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2002JD002505$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,1427,11493,27901,27902,45550,45551,46384,46443,46808,46867</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=14958156$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Takegawa, N.</creatorcontrib><creatorcontrib>Kondo, Y.</creatorcontrib><creatorcontrib>Koike, M.</creatorcontrib><creatorcontrib>Ko, M.</creatorcontrib><creatorcontrib>Kita, K.</creatorcontrib><creatorcontrib>Blake, D. R.</creatorcontrib><creatorcontrib>Nishi, N.</creatorcontrib><creatorcontrib>Hu, W.</creatorcontrib><creatorcontrib>Liley, J. B.</creatorcontrib><creatorcontrib>Kawakami, S.</creatorcontrib><creatorcontrib>Shirai, T.</creatorcontrib><creatorcontrib>Miyazaki, Y.</creatorcontrib><creatorcontrib>Ikeda, H.</creatorcontrib><creatorcontrib>Russel-Smith, J.</creatorcontrib><creatorcontrib>Ogawa, T.</creatorcontrib><title>Removal of NOx and NOy in biomass burning plumes in the boundary layer over northern Australia</title><title>Journal of Geophysical Research: Atmospheres</title><addtitle>J. Geophys. Res</addtitle><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.</description><subject>biomass burning</subject><subject>Chemical composition and interactions. Ionic interactions and processes</subject><subject>dry deposition of NOy</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Meteorology</subject><subject>northern Australia</subject><subject>NOx lifetime</subject><issn>0148-0227</issn><issn>2156-2202</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><recordid>eNpNUMFKAzEUDKJgqb35Abl4XE2yyW72WFqt1tLCongzZDeJRrfZknRr9-9Nqajv8AbezDyGAeASo2uMSHFDECLzaVwMsRMwIJhlCSGInIIBwpQniJD8HIxC-EBxKMsowgPwWup1u5MNbA1crvZQOhWxh9bByrZrGQKsOu-se4ObplvrcGC27xpWbeeU9D1sZK89bHdxudZHyjs47sLWy8bKC3BmZBP06AeH4Pnu9mlynyxWs4fJeJHYNCZOcow4MYyTQrGiIKnBlaQp41grqnmUcMRNkeHaKCUxxpU5nGuqZK2oNDQdgqvj340MtWyMl662QWy8XceMAtMiPmNZ1JGj7ss2uv_jkTh0KP53KOazchrDkGhKjiYbtnr_a5L-U2R5mjPxspyJspxjTpePoky_AWs9dBg</recordid><startdate>20030527</startdate><enddate>20030527</enddate><creator>Takegawa, N.</creator><creator>Kondo, Y.</creator><creator>Koike, M.</creator><creator>Ko, M.</creator><creator>Kita, K.</creator><creator>Blake, D. R.</creator><creator>Nishi, N.</creator><creator>Hu, W.</creator><creator>Liley, J. B.</creator><creator>Kawakami, S.</creator><creator>Shirai, T.</creator><creator>Miyazaki, Y.</creator><creator>Ikeda, H.</creator><creator>Russel-Smith, J.</creator><creator>Ogawa, T.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope></search><sort><creationdate>20030527</creationdate><title>Removal of NOx and NOy in biomass burning plumes in the boundary layer over northern Australia</title><author>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.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-i3002-71082f5829d59923f1ba43581ed4e8300808f961cfdda111bf4e83c4dacd4af43</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><topic>biomass burning</topic><topic>Chemical composition and interactions. Ionic interactions and processes</topic><topic>dry deposition of NOy</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Meteorology</topic><topic>northern Australia</topic><topic>NOx lifetime</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Takegawa, N.</creatorcontrib><creatorcontrib>Kondo, Y.</creatorcontrib><creatorcontrib>Koike, M.</creatorcontrib><creatorcontrib>Ko, M.</creatorcontrib><creatorcontrib>Kita, K.</creatorcontrib><creatorcontrib>Blake, D. R.</creatorcontrib><creatorcontrib>Nishi, N.</creatorcontrib><creatorcontrib>Hu, W.</creatorcontrib><creatorcontrib>Liley, J. B.</creatorcontrib><creatorcontrib>Kawakami, S.</creatorcontrib><creatorcontrib>Shirai, T.</creatorcontrib><creatorcontrib>Miyazaki, Y.</creatorcontrib><creatorcontrib>Ikeda, H.</creatorcontrib><creatorcontrib>Russel-Smith, J.</creatorcontrib><creatorcontrib>Ogawa, T.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><jtitle>Journal of Geophysical Research: Atmospheres</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Takegawa, N.</au><au>Kondo, Y.</au><au>Koike, M.</au><au>Ko, M.</au><au>Kita, K.</au><au>Blake, D. R.</au><au>Nishi, N.</au><au>Hu, W.</au><au>Liley, J. B.</au><au>Kawakami, S.</au><au>Shirai, T.</au><au>Miyazaki, Y.</au><au>Ikeda, H.</au><au>Russel-Smith, J.</au><au>Ogawa, T.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Removal of NOx and NOy in biomass burning plumes in the boundary layer over northern Australia</atitle><jtitle>Journal of Geophysical Research: Atmospheres</jtitle><addtitle>J. Geophys. Res</addtitle><date>2003-05-27</date><risdate>2003</risdate><volume>108</volume><issue>D10</issue><spage>ACH2.1</spage><epage>n/a</epage><pages>ACH2.1-n/a</pages><issn>0148-0227</issn><eissn>2156-2202</eissn><abstract>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.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2002JD002505</doi><tpages>14</tpages><oa>free_for_read</oa></addata></record> |
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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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