Nyamuragira (Virunga chain, D.R. Congo) is among Africa's most active volcanoes, but direct observations of its eruptions are rare. From 1978–2002 the Total Ozone Mapping Spectrometer (TOMS) instruments measured SO 2 emissions during each of Nyamuragira's 13 most recent eruptions. Due to continuous co‐eruptive SO 2 degassing, estimating the total atmospheric SO 2 loading resulting from eruptions of Nyamuragira is not straightforward. Using TOMS SO 2 plume cross‐sections and model wind profiles we derive eruptive SO 2 fluxes and SO 2 loss rates for emissions on 19 October 1998 and 6 February 2001, giving peak SO 2 fluxes of 0.21 and 0.74 Tg day −1 respectively and loss rates of ∼10 −6 –10 −5 s −1 . Based on current data, time‐averaged SO 2 emission rates at Nyamuragira are comparable to persistent emitters (Etna, Kilauea), but eruptive fluxes at Nyamuragira are much higher. Considering the alkaline composition of Virunga lavas, eruptive CO 2 fluxes could be seven times the SO 2 flux.
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Carn et al. (2003) studied this question.
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