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Scott D. Doiron

Researcher at STX Corporation

Publications -  11
Citations -  786

Scott D. Doiron is an academic researcher from STX Corporation. The author has contributed to research in topics: Total Ozone Mapping Spectrometer & Ozone depletion. The author has an hindex of 7, co-authored 11 publications receiving 762 citations. Previous affiliations of Scott D. Doiron include Goddard Space Flight Center.

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Global tracking of the SO2 clouds from the June, 1991 Mount Pinatubo eruptions

TL;DR: The explosive June 1991 eruptions of Pinatubo produced the largest sulfur dioxide cloud detected by the Total Ozone Mapping Spectrometer (TOMS) during its 13 years of operation: approximately 20 million tons of SO2, predominantly from the cataclysmic June 15th eruption.
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A simulation of the Cerro Hudson SO2 cloud

TL;DR: In this article, an isentropic trajectory model is used to simulate the evolution of the southern hemisphere SO2 cloud associated with the eruption of Cerro Hudson, which was still clearly observed 19 days after the eruption.
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TOMS measurement of the sulfur dioxide emitted during the 1985 Nevado del Ruiz eruptions

TL;DR: In this paper, the Nimbus 7 Total Ozone Mapping Spectrometer (TOMS) was used to quantitatively map volcanic sulfur dioxide plumes on a global scale, and the results showed that the ratio of sulfur dioxide to erupted magma from Ruiz was an order of magnitude greater than in the 1982 eruption of El Chichon or the 1980 eruption of Mount St. Helens.
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Transport of Cerro Hudson SO2 clouds

TL;DR: In this paper, the authors used the Total Ozone Mapping Spectrometer (TOMS) to measure the ratio of backscattered Earth radiance to incoming solar irradiance in the ultraviolet spectrum.
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Evaluation of sulfur dioxide emissions from explosive volcanism: the 1982–1983 eruptions of Galunggung, Java, Indonesia

TL;DR: Galunggung volcano, Java, awoke from a 63-year quiescence in April 1982, and erupted sporadically through January 1983, and an estimated 1730 kilotons (kt) of SO2 were outgassed by these explosive eruptions as mentioned in this paper.