Aj. Krueger et al., THE DECEMBER 1981 ERUPTION OF NYAMURAGIRA VOLCANO (ZAIRE), AND THE ORIGIN OF THE MYSTERY CLOUD OF EARLY 1982, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 101(D10), 1996, pp. 15191-15196
The ''mystery'' volcanic aerosols observed in early 1982 were produced
by the eruption of Nyamuragira in eastern Zaire. Large sulfur dioxide
clouds associated with this volcano were found in the total ozone map
ping spectrometer data beginning on December 26, 1981, continuing into
early January 1982. This fissure eruption produced 3 million tons of
sulfur dioxide in clouds that rose only to the tropopause level on the
basis of winds and inferred chemical loss rates (about 20%/day), whic
h are faster than stratospheric loss rates. Two thirds of the SO2 was
produced in the first 3 days of the eruption. In the 1980 this eruptio
n was exceeded in sulfur dioxide output only by the April 1982 eruptio
n of El Chichon.