Flaring emissions in Africa: Distribution, evolution and comparison with current inventories

El Hadji Thierno Doumbia (1) , Catherine Liousse (2) , Sekou Keita (3) , Louise Granier (4) , Claire Granier (2) , Christopher Elvidge (5) , Nellie Elguindi (2) , Kathy S. Law (6)

1 CNRM - Centre national de recherches météorologiques
2 LAERO - Laboratoire d'aérologie
3 Laboratoire de Physique de l’Atmosphère [Abidjan]
4 LATMOS - Laboratoire Atmosphères, Milieux, Observations Spatiales
5 ESRL - NOAA Earth System Research Laboratory
6 TROPO - LATMOS

Flaring emissions are a major concern due to large uncertainties in the amount of chemical compounds released into the atmosphere and their evolution with time. A methodology based on DMSP (Defense Meteorological Satellite Program) nighttime light data combined with regional gas flaring volumes from National Oceanic and Atmospheric Administration's National Centers for Environmental Information (NOAA-NCEI) has been developed to estimate flaring emissions. This method is validated in Nigeria where individual field company data are available. The spatial distribution of CO2, CH4, NMVOCs, CO, OC, BC, SO2 and NOx is derived for the African continent for the period 1995–2010. A range of the emissions due to flaring is estimated based on the range of emission factors (EFs) for each chemical species. An average decrease in CO2 emissions of about 30% is found over Africa from 1995 to 2010, with Nigeria being the largest contributor to this reduction (up to 50%). Changes in the spatial distribution with time indicate local increases, particularly at offshore platforms, which are attributed to a lack of regulations as well as aging infrastructures in oil and gas fields. Comparisons with current inventories reveal differences in the location and magnitude of point source emissions. For chemical compounds such as NMVOCs and CH4, the ECLIPSE and EDGAR country-level values are considerably higher than the highest flaring emission estimated in this study for 2005. For species such as CO, OC, BC, SO2 and NOx, the emissions provided by the ECLIPSE and EDGAR inventories are generally within the same order of magnitude as the average values found in this study, with the exception of OC, BC and SO2 in which EDGAR provides much lower emissions. These discrepancies are likely due to either differences in the methodologies used to estimate the emissions, in the values of the emission factors considered, or in the definition of flaring sector. Our current estimations suggest that BC, CH4 and CO2 flaring emissions in Africa account for 1–15% (on average 7%), 0.5–8% (on average 2%) and 8–13% (on average 11%) of African total anthropogenic emissions, respectively. The contribution of flaring to African anthropogenic emissions varies widely among countries. For example, in Nigeria the average emissions due to flaring are estimated to be as high as 18% for BC, 10% for CH4 and 50% for CO2, which is significantly greater than the continental average and highlights the importance of emissions in flaring areas.

Mots clés: Flare; Chemical compounds; Africa; Emission factor; Defense meteorological satellite program (DMSP); Nighttime light

Domaines: Planète et Univers [physics]; Océan, Atmosphère

El Hadji Thierno Doumbia, Catherine Liousse, Sekou Keita, Louise Granier, Claire Granier, et al.. Flaring emissions in Africa: Distribution, evolution and comparison with current inventories. Atmospheric Environment, 2019, 199, pp.423-434. ⟨10.1016/j.atmosenv.2018.11.006⟩. ⟨hal-02116054⟩