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dc.contributor.authorMüller, J.-F.
dc.contributor.authorBrasseur, G.
dc.date1999
dc.date.accessioned2017-05-09T11:58:43Z
dc.date.available2017-05-09T11:58:43Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/5370
dc.descriptionThe sources of odd hydrogen radicals (HOx=OH+HO2>) in the upper troposphere are investigated and quantified using a three-dimensional model. While the reaction of O(1D) with water vapor constitutes the single major source of HOx in the lower and middle troposphere, the model calculations suggest that acetone photooxidation represents a large, almost ubiquitous source of HOx in the upper troposphere (around 20-40% of the total primary source in the main aircraft corridors, poleward of 40°N), while the convective injections of peroxides and aldehydes are the dominant sources in the tropics, above the oceans and the continents, respectively. The consequences for ozone photochemical production in the upper troposphere are discussed, in particular, in the perspective of the aircraft impact. The role of acetone on ozone photochemical production is estimated and discussed. It is calculated that the presence of acetone might enhance by about 20% the sensitivity of upper tropospheric ozone to the current aircraft emissions of NOx.
dc.languageeng
dc.titleSources of upper tropospheric HOx: A three-dimensional study
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeacetone
dc.subject.freeaircraft emission
dc.subject.freepollutant source
dc.subject.freeradical
dc.subject.freetroposphere
dc.source.titleJournal of Geophysical Research Atmospheres
dc.source.volume104
dc.source.issueD1
dc.source.page1705-1715
Orfeo.peerreviewedYes
dc.identifier.doi10.1029/1998JD100005
dc.identifier.scopus2-s2.0-0033585575


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