Hydrogen peroxide, methyl hydroperoxide, and formaldehdye over North America and the North Atlantic
Hydrogen peroxide (HâO), methyl hydroperoxide (CHâOOH), and formaldehyde (CHâO) were measured over North America and the North Atlantic during the INTEX-NA, TOPSE, and SONEX aircraft campaigns. An overview of HâOâ, CHâOOH, and CHâO across the geographic and temporal range of these campaigns is presented. HâOâ, CHâOOH, and CHâO mixing ratios and variability were larger during INTEX-NA compared to TOPSE and SONEX. Mean HâOâ, CHâOOH, and CHâO were 1390, 440, and 480 pptv, respectively, more than two times higher than TOPSE measurements and an order of magnitude higher than SONEX measurements. This is attributed to higher solar radiation levels and the more polluted conditions of INTEX-NA. Mixing ratios and variability decreased with altitude for all three gases and on all three campaigns, except for CHâOOH during TOPSE. The impact of convection on HâOâ, CHâOOH, and CHâO is also discussed. Using the ratio HâOâ/CHâOOH, convectively influenced air parcels were found to be enhanced in CHâOOH, CHâO, CO, NO, and NOâ while HâOâ and HNO3 were depleted by wet removal. Biomass burning was also shown to increase HâOâ, CHâOOH, and CHâO mixing ratios up to 1.5, 2, and 1 ppbv, respectively, even after 4-5 days of transit. Results from this study show considerable variability in HâOâ, CHâOOH, and CHâO throughout the North American and North Atlantic troposphere. The variability in the upper troposphere is driven by local photochemical production and transport via regional convection and long-range pathways, suggesting transport mechanisms are important factors to include in photochemical models simulating HâOâ, CHâOOH, CHâO, and HOx.
document
https://n2t.org/ark:/85065/d7t43t92
eng
geoscientificInformation
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publication
2016-01-01T00:00:00Z
publication
2007-05-03T00:00:00Z
Copyright 2007 American Geophysical Union.
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