Modest volcanic SO2 emissions from the Indonesian archipelago
Philipson Bani, Clive Oppenheimer, V. I. Tsanev, Bruno Scaillet, Sofyan Primulyana, Ugan B. Saing, Hilma Alfianti, Mita Marlia
Abstract
Abstract Indonesia hosts the largest number of active volcanoes, several of which are renowned for climate-changing historical eruptions. This pedigree might suggest a substantial fraction of global volcanic sulfur emissions from Indonesia and are intrinsically driven by sulfur-rich magmas. However, a paucity of observations has hampered evaluation of these points—many volcanoes have hitherto not been subject to emissions measurements. Here we report new gas measurements from Indonesian volcanoes. The combined SO 2 output amounts to 1.15 ± 0.48 Tg/yr. We estimate an additional time-averaged SO 2 yield of 0.12-0.54 Tg/yr for explosive eruptions, indicating a total SO 2 inventory of 1.27-1.69 Tg/yr for Indonesian. This is comparatively modest—individual volcanoes such as Etna have sustained higher fluxes. To understand this paradox, we compare the geodynamic, petrologic, magma dynamical and shallow magmatic-hydrothermal processes that influence the sulfur transfer to the atmosphere. Results reinforce the idea that sulfur-rich eruptions reflect long-term accumulation of volatiles in the reservoirs.