author_facet Zannoni, Nora
Gros, Valerie
Sarda Esteve, Roland
Kalogridis, Cerise
Michoud, Vincent
Dusanter, Sebastien
Sauvage, Stephane
Locoge, Nadine
Colomb, Aurelie
Bonsang, Bernard
Zannoni, Nora
Gros, Valerie
Sarda Esteve, Roland
Kalogridis, Cerise
Michoud, Vincent
Dusanter, Sebastien
Sauvage, Stephane
Locoge, Nadine
Colomb, Aurelie
Bonsang, Bernard
author Zannoni, Nora
Gros, Valerie
Sarda Esteve, Roland
Kalogridis, Cerise
Michoud, Vincent
Dusanter, Sebastien
Sauvage, Stephane
Locoge, Nadine
Colomb, Aurelie
Bonsang, Bernard
spellingShingle Zannoni, Nora
Gros, Valerie
Sarda Esteve, Roland
Kalogridis, Cerise
Michoud, Vincent
Dusanter, Sebastien
Sauvage, Stephane
Locoge, Nadine
Colomb, Aurelie
Bonsang, Bernard
Atmospheric Chemistry and Physics
Summertime OH reactivity from a receptor coastal site in the Mediterranean Basin
Atmospheric Science
author_sort zannoni, nora
spelling Zannoni, Nora Gros, Valerie Sarda Esteve, Roland Kalogridis, Cerise Michoud, Vincent Dusanter, Sebastien Sauvage, Stephane Locoge, Nadine Colomb, Aurelie Bonsang, Bernard 1680-7324 Copernicus GmbH Atmospheric Science http://dx.doi.org/10.5194/acp-17-12645-2017 <jats:p>Abstract. Total hydroxyl radical (OH) reactivity, the total loss frequency of the hydroxyl radical in ambient air, provides the total loading of OH reactants in air. We measured the total OH reactivity for the first time during summertime at a coastal receptor site located in the western Mediterranean Basin. Measurements were performed at a temporary field site located in the northern cape of Corsica (France), during summer 2013 for the project CARBOSOR (CARBOn within continental pollution plumes: SOurces and Reactivity)–ChArMEx (Chemistry and Aerosols Mediterranean Experiment). Here, we compare the measured total OH reactivity with the OH reactivity calculated from the measured reactive gases. The difference between these two parameters is termed missing OH reactivity, i.e., the fraction of OH reactivity not explained by the measured compounds. The total OH reactivity at the site varied between the instrumental LoD (limit of detection = 3 s−1) to a maximum of 17 ± 6 s−1 (35 % uncertainty) and was 5 ± 4 s−1 (1σ SD – standard deviation) on average. It varied with air temperature exhibiting a diurnal profile comparable to the reactivity calculated from the concentration of the biogenic volatile organic compounds measured at the site. For part of the campaign, 56 % of OH reactivity was unexplained by the measured OH reactants (missing reactivity). We suggest that oxidation products of biogenic gas precursors were among the contributors to missing OH reactivity. </jats:p> Summertime OH reactivity from a receptor coastal site in the Mediterranean Basin Atmospheric Chemistry and Physics
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title Summertime OH reactivity from a receptor coastal site in the Mediterranean Basin
title_unstemmed Summertime OH reactivity from a receptor coastal site in the Mediterranean Basin
title_full Summertime OH reactivity from a receptor coastal site in the Mediterranean Basin
title_fullStr Summertime OH reactivity from a receptor coastal site in the Mediterranean Basin
title_full_unstemmed Summertime OH reactivity from a receptor coastal site in the Mediterranean Basin
title_short Summertime OH reactivity from a receptor coastal site in the Mediterranean Basin
title_sort summertime oh reactivity from a receptor coastal site in the mediterranean basin
topic Atmospheric Science
url http://dx.doi.org/10.5194/acp-17-12645-2017
publishDate 2017
physical 12645-12658
description <jats:p>Abstract. Total hydroxyl radical (OH) reactivity, the total loss frequency of the hydroxyl radical in ambient air, provides the total loading of OH reactants in air. We measured the total OH reactivity for the first time during summertime at a coastal receptor site located in the western Mediterranean Basin. Measurements were performed at a temporary field site located in the northern cape of Corsica (France), during summer 2013 for the project CARBOSOR (CARBOn within continental pollution plumes: SOurces and Reactivity)–ChArMEx (Chemistry and Aerosols Mediterranean Experiment). Here, we compare the measured total OH reactivity with the OH reactivity calculated from the measured reactive gases. The difference between these two parameters is termed missing OH reactivity, i.e., the fraction of OH reactivity not explained by the measured compounds. The total OH reactivity at the site varied between the instrumental LoD (limit of detection  =  3 s−1) to a maximum of 17 ± 6 s−1 (35 % uncertainty) and was 5 ± 4 s−1 (1σ SD – standard deviation) on average. It varied with air temperature exhibiting a diurnal profile comparable to the reactivity calculated from the concentration of the biogenic volatile organic compounds measured at the site. For part of the campaign, 56 % of OH reactivity was unexplained by the measured OH reactants (missing reactivity). We suggest that oxidation products of biogenic gas precursors were among the contributors to missing OH reactivity. </jats:p>
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author Zannoni, Nora, Gros, Valerie, Sarda Esteve, Roland, Kalogridis, Cerise, Michoud, Vincent, Dusanter, Sebastien, Sauvage, Stephane, Locoge, Nadine, Colomb, Aurelie, Bonsang, Bernard
author_facet Zannoni, Nora, Gros, Valerie, Sarda Esteve, Roland, Kalogridis, Cerise, Michoud, Vincent, Dusanter, Sebastien, Sauvage, Stephane, Locoge, Nadine, Colomb, Aurelie, Bonsang, Bernard, Zannoni, Nora, Gros, Valerie, Sarda Esteve, Roland, Kalogridis, Cerise, Michoud, Vincent, Dusanter, Sebastien, Sauvage, Stephane, Locoge, Nadine, Colomb, Aurelie, Bonsang, Bernard
author_sort zannoni, nora
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container_title Atmospheric Chemistry and Physics
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description <jats:p>Abstract. Total hydroxyl radical (OH) reactivity, the total loss frequency of the hydroxyl radical in ambient air, provides the total loading of OH reactants in air. We measured the total OH reactivity for the first time during summertime at a coastal receptor site located in the western Mediterranean Basin. Measurements were performed at a temporary field site located in the northern cape of Corsica (France), during summer 2013 for the project CARBOSOR (CARBOn within continental pollution plumes: SOurces and Reactivity)–ChArMEx (Chemistry and Aerosols Mediterranean Experiment). Here, we compare the measured total OH reactivity with the OH reactivity calculated from the measured reactive gases. The difference between these two parameters is termed missing OH reactivity, i.e., the fraction of OH reactivity not explained by the measured compounds. The total OH reactivity at the site varied between the instrumental LoD (limit of detection  =  3 s−1) to a maximum of 17 ± 6 s−1 (35 % uncertainty) and was 5 ± 4 s−1 (1σ SD – standard deviation) on average. It varied with air temperature exhibiting a diurnal profile comparable to the reactivity calculated from the concentration of the biogenic volatile organic compounds measured at the site. For part of the campaign, 56 % of OH reactivity was unexplained by the measured OH reactants (missing reactivity). We suggest that oxidation products of biogenic gas precursors were among the contributors to missing OH reactivity. </jats:p>
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spelling Zannoni, Nora Gros, Valerie Sarda Esteve, Roland Kalogridis, Cerise Michoud, Vincent Dusanter, Sebastien Sauvage, Stephane Locoge, Nadine Colomb, Aurelie Bonsang, Bernard 1680-7324 Copernicus GmbH Atmospheric Science http://dx.doi.org/10.5194/acp-17-12645-2017 <jats:p>Abstract. Total hydroxyl radical (OH) reactivity, the total loss frequency of the hydroxyl radical in ambient air, provides the total loading of OH reactants in air. We measured the total OH reactivity for the first time during summertime at a coastal receptor site located in the western Mediterranean Basin. Measurements were performed at a temporary field site located in the northern cape of Corsica (France), during summer 2013 for the project CARBOSOR (CARBOn within continental pollution plumes: SOurces and Reactivity)–ChArMEx (Chemistry and Aerosols Mediterranean Experiment). Here, we compare the measured total OH reactivity with the OH reactivity calculated from the measured reactive gases. The difference between these two parameters is termed missing OH reactivity, i.e., the fraction of OH reactivity not explained by the measured compounds. The total OH reactivity at the site varied between the instrumental LoD (limit of detection = 3 s−1) to a maximum of 17 ± 6 s−1 (35 % uncertainty) and was 5 ± 4 s−1 (1σ SD – standard deviation) on average. It varied with air temperature exhibiting a diurnal profile comparable to the reactivity calculated from the concentration of the biogenic volatile organic compounds measured at the site. For part of the campaign, 56 % of OH reactivity was unexplained by the measured OH reactants (missing reactivity). We suggest that oxidation products of biogenic gas precursors were among the contributors to missing OH reactivity. </jats:p> Summertime OH reactivity from a receptor coastal site in the Mediterranean Basin Atmospheric Chemistry and Physics
spellingShingle Zannoni, Nora, Gros, Valerie, Sarda Esteve, Roland, Kalogridis, Cerise, Michoud, Vincent, Dusanter, Sebastien, Sauvage, Stephane, Locoge, Nadine, Colomb, Aurelie, Bonsang, Bernard, Atmospheric Chemistry and Physics, Summertime OH reactivity from a receptor coastal site in the Mediterranean Basin, Atmospheric Science
title Summertime OH reactivity from a receptor coastal site in the Mediterranean Basin
title_full Summertime OH reactivity from a receptor coastal site in the Mediterranean Basin
title_fullStr Summertime OH reactivity from a receptor coastal site in the Mediterranean Basin
title_full_unstemmed Summertime OH reactivity from a receptor coastal site in the Mediterranean Basin
title_short Summertime OH reactivity from a receptor coastal site in the Mediterranean Basin
title_sort summertime oh reactivity from a receptor coastal site in the mediterranean basin
title_unstemmed Summertime OH reactivity from a receptor coastal site in the Mediterranean Basin
topic Atmospheric Science
url http://dx.doi.org/10.5194/acp-17-12645-2017