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William I. Rose

Researcher at Michigan Technological University

Publications -  242
Citations -  14212

William I. Rose is an academic researcher from Michigan Technological University. The author has contributed to research in topics: Volcano & Volcanic ash. The author has an hindex of 71, co-authored 241 publications receiving 13418 citations. Previous affiliations of William I. Rose include National Center for Atmospheric Research & United States Geological Survey.

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Ice in the 1994 Rabaul eruption cloud : implications for volcano hazard and atmospheric effects

TL;DR: In this article, a satellite-borne infrared sensor was used to detect 2 million tonnes of ice in the cloud produced by the September 1994 eruption of Rabaul volcano, in Papua New Guinea.
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Tephra fallout in the eruption of Soufrière Hills Volcano, Montserrat

TL;DR: In this article, four mechanisms caused tephra fallout at Soufriere Hills Volcano, Montserrat, during the 1995-1999 period: explosive activity (mainly of Vulcanian type), dome collapses, ash-venting and phreatic explosions.
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Ice nucleation and overseeding of ice in volcanic clouds

TL;DR: In this paper, single-particle freezing experiments were carried out to investigate the effect of volcanic ash particle composition and surface area on water drop freezing temperature and found that volcanic clouds are more ice-forming nuclei rich relative to meteorological clouds, and therefore should exhibit distinct microphysics.
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An estimate of gas emissions and magmatic gas content from Kilauea volcano

TL;DR: In this paper, the authors estimate the loading of Kilauean eruptive gases to the atmosphere and suggest that such estimates may be inferred directly from measured lava volumes, using data from the east-rift eruptive plume and CO2 and SO2 measured in the plume from the noneruptive fumaroles in the summit caldera.
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Temporal trends in lava dome extrusion at Santiaguito 1922–2000

TL;DR: Extrusion rates derived from the Landsat data for Santiaguito dome complex (Guatemala) during November 1987 and January 2000 of 072±008 and 048±009 m3 s−1 compare favorably with ground-based estimates of 063±028 and 0 48±017 m−1 as discussed by the authors.