Mo. Andreae et al., METHYL HALIDE EMISSIONS FROM SAVANNA FIRES IN SOUTHERN AFRICA, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 101(D19), 1996, pp. 23603-23613
The methyl halides, methyl chloride (CH3Cl), methyl bromide (CH3Br), a
nd methyl iodide (CH3I), were measured in regional air samples and smo
ke from savanna fires in southern Africa during the Southern Africa Fi
re-Atmosphere Research Initiative-92 (SAFARI-92) experiment (August-Oc
tober 1992). All three species were significantly enhanced in the smok
e plumes relative to the regional background. Good correlations were f
ound between the methyl halides and carbon monoxide, suggesting that e
mission was predominantly associated with the smoldering phase of the
fires. About 90% of the halogen content of the fuel burned was release
d to the atmosphere, mostly as halide species, but a significant fract
ion (3-38%) was emitted in methylated form. On the basis of comparison
with the composition of the regional background atmosphere, emission
ratios to carbon dioxide and carbon monoxide were determined for the m
ethyl halide species. The emission ratios decreased in the sequence CH
3Cl > CH3Br > CH3I. Extrapolation of these results in combination with
data from other types of biomass burning, e.g. forest fires, suggests
that vegetation fires make a significant contribution to the atmosphe
ric budget of CH3Cl and CH3Br. For tropospheric CH3I, on the other han
d, fires appear to be a minor source. Our results suggest that pyrogen
ic emissions of CH3Cl and CH3Br need to be considered as significant c
ontributors to stratospheric ozone destruction.