Enhanced Role of Transition Metal Ion Catalysis During In-Cloud Oxidation of SO2

dc.contributor.authorSinha, B.
dc.date.accessioned2020-12-11T06:57:46Z
dc.date.available2020-12-11T06:57:46Z
dc.date.issued2013
dc.descriptionOnly IISERM authors are available in the record.
dc.description.abstractGlobal sulfate production plays a key role in aerosol radiative forcing; more than half of this production occurs in clouds. We found that sulfur dioxide oxidation catalyzed by natural transition metal ions is the dominant in-cloud oxidation pathway. The pathway was observed to occur primarily on coarse mineral dust, so the sulfate produced will have a short lifetime and little direct or indirect climatic effect. Taking this into account will lead to large changes in estimates of the magnitude and spatial distribution of aerosol forcing. Therefore, this oxidation pathway—which is currently included in only one of the 12 major global climate models—will have a significant impact on assessments of current and future climate.en_US
dc.identifier.citationScience, 340(6133), pp.727-730.en_US
dc.identifier.other10.1126/science.1230911
dc.identifier.urihttps://science.sciencemag.org/content/340/6133/727
dc.identifier.urihttp://hdl.handle.net/123456789/3039
dc.language.isoenen_US
dc.publisherAmerican Association for the Advancement of Science.en_US
dc.subjectGlobal sulfateen_US
dc.subjectOxidationen_US
dc.subjectCloudsen_US
dc.titleEnhanced Role of Transition Metal Ion Catalysis During In-Cloud Oxidation of SO2en_US
dc.typeArticleen_US

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