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dc.contributor.authorFredrickson, C.D.
dc.contributor.authorTheys, N.
dc.contributor.authorThornton, J.A.
dc.date2023
dc.date.accessioned2023-09-08T08:37:57Z
dc.date.available2023-09-08T08:37:57Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/11064
dc.descriptionWildfires are important sources of atmospheric reactive nitrogen. The reactive nitrogen species partitioning generally depends on fire characteristics. One reactive nitrogen compound, nitrous acid (HONO), is a source of hydroxyl radicals and nitric oxide, which can impact the oxidizing capacity of the atmosphere and fire plume chemistry and composition. We study the Australian wildfire season of 2019–2020, known as Black Summer, where numerous large and intense wildfires burned throughout the continent. We use HONO and nitrogen dioxide (NO2) from the TROPOspheric Monitoring Instrument (TROPOMI) and fire radiative power (FRP) from the Visible Infrared Imaging Radiometer Suite to investigate HONO and NO2 relationships with fire characteristics. The ratio of HONO to NO2 increases linearly with FRP both in Australia and globally. Both Australian and global fire relationships depend strongly on land cover type. These relationships can be applied to emission inventories to improve wildfire emission representation in models.
dc.languageeng
dc.titleSatellite Evidence of HONO/NO2 Increase with Fire Radiative Power
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freefire emissions
dc.subject.freeTROPOMI
dc.subject.freesatellite FRP
dc.subject.freereactive nitrogen
dc.subject.freenitrous acid
dc.source.titleGeophysical Research Letters
dc.source.volume50
dc.source.issue17
dc.source.pagee2023GL103836
Orfeo.peerreviewedYes
dc.identifier.doi10.1029/2023GL103836
dc.identifier.scopus


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