Aircraft and ground-based measurements of hydroperoxides during the 2006 MILAGRO field campaign
Mixing ratios of hydrogen peroxide and hydroxymethyl hydroperoxide were determined aboard the US Department of Energy G-1 Research Aircraft during the March, 2006 MILAGRO field campaign in Mexico. Ground measurements of total hydroperoxide were made at Tecámac University, about 35 km NW of Mexico Ci...
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2008-12-01
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Series: | Atmospheric Chemistry and Physics |
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doaj-a1631f90ceae4e5fb316c7e761d8bf5c2020-11-25T00:19:42ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242008-12-0182476197636Aircraft and ground-based measurements of hydroperoxides during the 2006 MILAGRO field campaignL. J. NunnermackerJ. B. Weinstein-LloydB. HilleryB. GiebelL. I. KleinmanS. R. SpringstonP. H. DaumJ. GaffneyN. MarleyG. HueyMixing ratios of hydrogen peroxide and hydroxymethyl hydroperoxide were determined aboard the US Department of Energy G-1 Research Aircraft during the March, 2006 MILAGRO field campaign in Mexico. Ground measurements of total hydroperoxide were made at Tecámac University, about 35 km NW of Mexico City. In the air and on the ground, peroxide mixing ratios near the source region were generally near 1 ppbv. Strong southerly flow resulted in transport of pollutants from Mexico City to two downwind surface sites on several flight days. On these days, it was observed that peroxide concentrations slightly decreased as the G-1 flew progressively downwind. This observation is consistent with low or negative net peroxide production rates calculated for the source region and is due to the very high NO<sub>x</sub> concentrations in the Mexico City plateau. However, relatively high values of peroxide were observed at takeoff and landing near Veracruz, a site with much higher humidity and lower NO<sub>x</sub> concentrations. http://www.atmos-chem-phys.net/8/7619/2008/acp-8-7619-2008.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
L. J. Nunnermacker J. B. Weinstein-Lloyd B. Hillery B. Giebel L. I. Kleinman S. R. Springston P. H. Daum J. Gaffney N. Marley G. Huey |
spellingShingle |
L. J. Nunnermacker J. B. Weinstein-Lloyd B. Hillery B. Giebel L. I. Kleinman S. R. Springston P. H. Daum J. Gaffney N. Marley G. Huey Aircraft and ground-based measurements of hydroperoxides during the 2006 MILAGRO field campaign Atmospheric Chemistry and Physics |
author_facet |
L. J. Nunnermacker J. B. Weinstein-Lloyd B. Hillery B. Giebel L. I. Kleinman S. R. Springston P. H. Daum J. Gaffney N. Marley G. Huey |
author_sort |
L. J. Nunnermacker |
title |
Aircraft and ground-based measurements of hydroperoxides during the 2006 MILAGRO field campaign |
title_short |
Aircraft and ground-based measurements of hydroperoxides during the 2006 MILAGRO field campaign |
title_full |
Aircraft and ground-based measurements of hydroperoxides during the 2006 MILAGRO field campaign |
title_fullStr |
Aircraft and ground-based measurements of hydroperoxides during the 2006 MILAGRO field campaign |
title_full_unstemmed |
Aircraft and ground-based measurements of hydroperoxides during the 2006 MILAGRO field campaign |
title_sort |
aircraft and ground-based measurements of hydroperoxides during the 2006 milagro field campaign |
publisher |
Copernicus Publications |
series |
Atmospheric Chemistry and Physics |
issn |
1680-7316 1680-7324 |
publishDate |
2008-12-01 |
description |
Mixing ratios of hydrogen peroxide and hydroxymethyl hydroperoxide were determined aboard the US Department of Energy G-1 Research Aircraft during the March, 2006 MILAGRO field campaign in Mexico. Ground measurements of total hydroperoxide were made at Tecámac University, about 35 km NW of Mexico City. In the air and on the ground, peroxide mixing ratios near the source region were generally near 1 ppbv. Strong southerly flow resulted in transport of pollutants from Mexico City to two downwind surface sites on several flight days. On these days, it was observed that peroxide concentrations slightly decreased as the G-1 flew progressively downwind. This observation is consistent with low or negative net peroxide production rates calculated for the source region and is due to the very high NO<sub>x</sub> concentrations in the Mexico City plateau. However, relatively high values of peroxide were observed at takeoff and landing near Veracruz, a site with much higher humidity and lower NO<sub>x</sub> concentrations. |
url |
http://www.atmos-chem-phys.net/8/7619/2008/acp-8-7619-2008.pdf |
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