Seasonal and diurnal variability in O3, black carbon, and CO measured at the Rwanda Climate Observatory
Author(s)
DeWitt, H. Langley; Gasore, Jimmy; Rupakheti, Maheswar; Potter, Katherine E.; Prinn, Ronald G.; Ndikubwimana, Jean de Dieu; Nkusi, Julius; Safari, Bonfils; ... Show more Show less
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Air 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. ©2019
Date issued
2019-02Department
Massachusetts Institute of Technology. Center for Global Change ScienceJournal
Atmospheric chemistry and physics
Publisher
Copernicus GmbH
Citation
DeWitt, 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)
Version: Final published version
ISSN
1680-7324
1680-7316