Abstract. 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
climate-forcing 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 µg m−3
(daily average concentrations ranging from less than
0.1 to over 17 µg m−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.