Observations of volcanic clouds in their first few days of atmospheric residence: The 1992 eruptions of Crater Peak, Mount Spurr volcano, Alaska

Satellite SO2 and ash measurements of Mount Spurr's three 1992 volcanic clo uds are compared with ground-based observations to develop an understanding of the physical and chemical evolution of volcanic clouds. Each of the thr ee eruptions with ratings of volcanic explosivity index three reached the l ower stratosphere (14 km asl), but the clouds were mainly dispersed at the tropopause by moderate to strong (20-40 m/s) tropospheric winds. Three stag es of cloud evolution were identified. First, heavy fallout of large (>500 mum) pyroclasts occurred close to the volcano (<25 km from the vent) during and immediately after the eruptions, and the cloud resembled an advected g ravity current. Second, a much larger, highly elongated region marked by a secondary-mass maximum occurred 150-350 km downwind in at least two of the three events. This was the result of aggregate fallout of a bimodal size di stribution including fine (<25 mum) ash that quickly depleted the solid fra ction of the volcanic cloud. For the first several hundred kilometers, the cloud spread laterally, first as an intrusive gravity current and then by w ind shear and diffusion as downwind cloud transport occurred at the windspe ed (during the first 18-24 h). Finally, the clouds continued to move throug h the upper troposphere but began decreasing in areal extent, eventually di sappearing as ash and SO2 were removed by meteorological processes. Total S O2 in each eruption cloud increased by the second day of atmospheric reside nce, possibly because of oxidation of coerupted H2S or possibly because of the effects of sequestration by ice followed by subsequent SO2 release duri ng fallout and desiccation of ashy hydrometeors. SO2 and volcanic ash trave lled together in all the Spurr volcanic clouds. The initial (18-24 h) area expansion of the clouds and the subsequent several days of drifting were su ccessfully mapped by both SO2 (ultraviolet) and ash (infrared) satellite im agery.