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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Main Authors: 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
Format: Article
Language:English
Published: Copernicus Publications 2008-12-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/8/7619/2008/acp-8-7619-2008.pdf
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spelling 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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