Journal
ATMOSPHERIC CHEMISTRY AND PHYSICS
Volume 21, Issue 21, Pages 16277-16291Publisher
COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/acp-21-16277-2021
Keywords
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Funding
- NASA
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This study analyzed the changes in atmospheric NH3 concentrations over Africa from 2008 to 2018 using satellite observations. The results showed an increase in NH3 concentrations in some regions, such as Nigeria and the Lake Victoria basin, while a decrease was observed in the Sudd wetlands in South Sudan. The changes in NH3 concentrations were closely related to factors such as burned area, CO trends, and drying of wetland soils.
Atmospheric ammonia (NH3) is a precursor to fine particulate matter and a source of nitrogen (N) deposition that can adversely affect ecosystem health. The main sources of NH3 - agriculture and biomass burning - are undergoing are or expected to undergo substantial changes in Africa. Although evidence of increasing NH3 over parts of Africa has been observed, the mechanisms behind these trends are not well understood. Here we use observations of atmospheric NH3 vertical column densities (VCDs) from the Infrared Atmospheric Sounding Interferometer (IASI) along with other satellite observations of the land surface and atmosphere to evaluate how NH3 concentrations have changed over Africa from 2008 through 2018, and what has caused those changes. In West Africa NH3 VCDs are observed to increase during the late dry season, with increases of over 6% yr(-1) in Nigeria during February and March ( p<0 :01). These positive trends are associated with increasing burned area and CO trends during these months, likely related to agricultural preparation. Increases are also observed in the Lake Victoria basin region, where they are associated with expanding agricultural area. In contrast, NH3 VCDs declined over the Sudd wetlands in South Sudan by over 1.5% yr(-1), though not significantly (p D 0:28). Annual maxima in NH3 VCDs in South Sudan occur during February through May and are associated with the drying of temporarily flooded wetland soils, which favor emissions of NH3. The change in mean NH3 VCDs over the Sudd is strongly correlated with variation in wetland extent in the Sudd: in years when more area remained flooded during the dry season, NH3 VCDs were lower (r D 0:64, p<0:05). Relationships between biomass burning and NH3 may be observed when evaluating nationalscale statistics: countries with the highest rates of increasing NH3 VCDs also had high rates of growth in CO VCDs; burned area displayed a similar pattern, though not significantly. Livestock numbers were also higher in countries with intermediate or high rates of NH3 VCD growth. Fertilizer use in Africa is currently low but growing; implementing practices that can limit NH3 losses from fertilizer as agriculture is intensified may help mitigate impacts on health and ecosystems.
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