The Impact of Uncertainties in African Biomass Burning Emission Estimates on Modeling Global Air Quality, Long Range Transport and Tropospheric Chemical Lifetimes

• Published in: Atmosphere 2012-03, Vol.3 (1), p.132-163
• Main Authors: Williams, Jason E., Weele, Michiel van, Velthoven, Peter F. J. van, Scheele, Marinus P., Liousse, Catherine, Werf, Guido R. van der
• Format: Article
• Language: English
• Subjects: African biomass burning; Air quality; air quality; Annual variations; Atmospheric chemistry; Carbon monoxide; emission inventories; Emissions; long range transport; Methane; methane lifetimes; Pollution dispersion; Temporal distribution; Tropical environments; Troposphere
• ISSN: 2073-4433; 2073-4433
• DOI: 10.3390/atmos3010132

The chemical composition of the troposphere in the tropics and Southern Hemisphere (SH) is significantly influenced by gaseous emissions released from African biomass burning (BB). Here we investigate how various emission estimates given in bottom-up BB inventories (GFEDv2, GFEDv3, AMMABB) affect simulations of global tropospheric composition using the TM4 chemistry transport model. The application of various model parameterizations for introducing such emissions is also investigated. There are perturbations in near-surface ozone (O3) and carbon monoxide (CO) of ~60–90% in the tropics and ~5–10% in the SH between different inventories. Increasing the update frequency of the temporal distribution to eight days generally results in decreases of between ~5 and 10% in near-surface mixing ratios throughout the tropics, which is larger than the influence of increasing the injection heights at which BB emissions are introduced. There are also associated differences in the long range transport of pollutants throughout the SH, where the composition of the free troposphere in the SH is sensitive to the chosen BB inventory. Analysis of the chemical budget terms reveals that the influence of increasing the tropospheric CO burden due to BB on oxidative capacity of the troposphere is mitigated by the associated increase in NOx emissions (and thus O3) with the variations in the CO/N ratio between inventories being low. For all inventories there is a decrease in the tropospheric chemical lifetime of methane of between 0.4 and 0.8% regardless of the CO emitted from African BB. This has implications for assessing the effect of inter-annual variability in BB on the annual growth rate of methane.