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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/509

Authors: McGonigle, A. J. S.*
Inguaggiato, S.*
Aiuppa, A.*
Hayes, A.R.*
Oppenheimer, C.*
Title: Accurate measurement of volcanic SO2 flux: Determination of plume transport speed and integrated SO2 concentration with a single device
Title of journal: Geochemistry, Geophysics, Geosystems
Series/Report no.: 1/6(2005)
Publisher: American Geophysical Union
Issue Date: 9-Feb-2005
DOI: 10.1029/2004GC000845
URL: http://www.agu.org/
Keywords: DOAS
volcanic SO2 emissions.
Abstract: Ground-based measurements of volcanic sulfur dioxide fluxes are important indicators of volcanic activity, with application in hazard assessment, and understanding the impacts of volcanic emissions upon the environment and climate. These data are obtained by making traverses underneath the volcanic plume a few kilometers from source with an ultraviolet spectrometer, measuring integrated SO2 concentrations across the plume’s cross section, and multiplying by the plume’s transport speed. However, plume velocities are usually derived from ground-based anemometers, located many kilometers from the traverse route and hundreds of meters below plume altitude, complicating the experimental design and introducing large flux (can be >100%) errors. Here we present the first report of a single instrument capable of (accurate) volcanic SO2 flux measurements. This device records integrated SO2 concentrations and plume heights during traverses. Between traverses, two in-plume SO2 time series are measured from underneath the plume with the instrument, corresponding to zenith and inclined (user-specified angle from vertical in the direction of the volcano) fields of view, respectively. The distance between the points of intersection of the two views with the plume is found on the basis of the determined plume height, and the two signals are cross-correlated to determine the lag between them, enabling accurate derivation of the wind speed. We present flux data (with errors ±12%) obtained in this way at Mt. Etna during July 2004.
Appears in Collections:04.08.07. Instruments and techniques
04.08.01. Gases
04.08.08. Volcanic risk
04.08.06. Volcano monitoring
01.01.07. Volcanic effects
Papers Published / Papers in press

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