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dc.contributor.authorDeWitt, H. Langley
dc.contributor.authorGasore, Jimmy
dc.contributor.authorRupakheti, Maheswar
dc.contributor.authorPotter, Katherine E.
dc.contributor.authorPrinn, Ronald G.
dc.contributor.authorNdikubwimana, Jean de Dieu
dc.contributor.authorNkusi, Julius
dc.contributor.authorSafari, Bonfils
dc.date.accessioned2020-04-17T18:27:44Z
dc.date.available2020-04-17T18:27:44Z
dc.date.issued2019-02
dc.date.submitted2018-12
dc.identifier.issn1680-7324
dc.identifier.issn1680-7316
dc.identifier.urihttps://hdl.handle.net/1721.1/124730
dc.description.abstractAir pollution is understudied in sub-Saharan Africa, resulting in a gap in the scientific understanding of emissions, atmospheric processes, and impacts of air pollutants in this region. The Rwanda Climate Observatory, a joint partnership between MIT and the government of Rwanda, has been measuring ambient concentrations of key long-lived greenhouse gases and the short-lived climateforcing pollutants CO2, CO, CH4, black carbon (BC), and O3 with state-of-the-art instruments on the summit of Mt. Mugogo (1.586◦ S, 29.566◦ E; 2590 m above sea level) since May 2015. Rwanda is a small, mountainous, and densely populated country in equatorial East Africa, currently undergoing rapid development but still at less than 20 % urbanization. Black carbon concentrations during Rwanda’s two dry seasons (December–January–February, DJF, and June–July– August, JJA), which coincide with the two regional biomass burning seasons, are higher at Mt. Mugogo than in major European cities with daily values (24 h) during the dry season of around 5 µgm−3 (daily average concentrations ranging from less than 0.1 to over 17 µgm−3 for the entire measurement period). BC baseline concentrations during biomass burning seasons are loosely correlated with fire radiative power data for the region acquired with a MODIS satellite instrument. The position and meteorology of Rwanda is such that the emissions transported from both the northern and southern African biomass burning seasons affect BC, CO, and O3 concentrations in Rwanda. Spectral aerosol absorption measured with a dual-spot Aethalometer varies seasonally due to changes in types of fuel burned and the direction of pollution transport to the site. Ozone concentrations peaked during Rwanda’s dry seasons (daily measured maximum of 70 ppbv). The understanding and quantification of the percent contributions of regional and local (beyond large-scale biomass) emissions is essential to guide policy in the region. During the rainy seasons, local emitting activities (e.g., cooking, transportation, trash burning) remain steady, regional biomass burning is low, and transport distances are shorter as rainout of pollution occurs regularly. Thus, local pollution at Mugogo can be estimated during this time period and was found to account for up to 35% of annual average BC measured. Our measurements indicate that air pollution is a current and growing problem in equatorial East Africa. ©2019en_US
dc.language.isoen
dc.publisherCopernicus GmbHen_US
dc.relation.isversionof10.5194/ACP-19-2063-2019en_US
dc.rightsCreative Commons Attribution 4.0 International licenseen_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_US
dc.sourceCopernicus Publicationsen_US
dc.titleSeasonal and diurnal variability in O3, black carbon, and CO measured at the Rwanda Climate Observatoryen_US
dc.typeArticleen_US
dc.identifier.citationDeWitt, H. Langley, et al., "Seasonal and diurnal variability in O3, black carbon, and CO measured at the Rwanda Climate Observatory." Atmospheric chemistry and physics 19, 3 (February 2019): p. 2063-78 doi 10.5194/ACP-19-2063-2019 ©2019 Author(s)en_US
dc.contributor.departmentMassachusetts Institute of Technology. Center for Global Change Scienceen_US
dc.relation.journalAtmospheric chemistry and physicsen_US
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dc.date.updated2020-04-07T15:22:51Z
dspace.date.submission2020-04-07T15:22:56Z
mit.journal.volume19en_US
mit.journal.issue3en_US
mit.licensePUBLISHER_CC
mit.metadata.statusComplete


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