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- W4313596887 abstract "Field-portable Open Path Fourier Transform Infrared (OP-FTIR) spectrometers can be used to remotely measure the composition of volcanic plumes using absorption spectroscopy, providing invaluable data on total gas emissions. Quantifying the temporal evolution of gas compositions during an eruption helps develop models of volcanic processes and aids in eruption forecasting. Absorption measurements require a viewing geometry which aligns infrared source, plume, and instrument, which can be challenging. Here, we present a fast retrieval algorithm to estimate quantities of gas, ash and sulphate aerosols from thermal emission OP-FTIR measurements, and the results from two pilot campaigns on Stromboli volcano in Italy in 2019 and 2021. We validate the method by comparing time series of SO 2 slant column densities retrieved using our method with those obtained from a conventional UV spectrometer, demonstrating that the two methods generally agree to within a factor of 2. The algorithm correctly identifies ash-rich plumes and gas bursts associated with explosions and quantifies the mass column densities and particle sizes of ash and sulphate aerosols (SA) in the plume. We compare the ash sizes retrieved using our method with the particle size distribution (PSD) of an ash sample collected during the period of measurements in 2019 by flying a Remotely Piloted Aircraft System into the path of a drifting ash plume and find that both modes of the bimodal PSD (a fine fraction with diameter around 5–10 μm and a coarse fraction around 65 μm) are identified within our datasets at different times. We measure a decrease in the retrieved ash particle size with distance downwind, consistent with settling of larger particles, which we also observed visually. We measure a decrease in the SO 2 /SA ratio as the plume travels downwind, coupled with an increase in measured SA particle size (range 2–6 μm), suggesting rapid hygroscopic particle growth and/or SO 2 oxidation. We propose that infrared emission spectroscopy can be used to examine physical and chemical changes during plume transport and opens the possibility of remote night-time monitoring of volcanic plume emissions. These ground-based analyses may also aid the refinement of satellite-based aerosol retrievals." @default.
- W4313596887 created "2023-01-06" @default.
- W4313596887 creator A5025108710 @default.
- W4313596887 creator A5028296166 @default.
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- W4313596887 creator A5036902412 @default.
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- W4313596887 creator A5087267796 @default.
- W4313596887 creator A5088853790 @default.
- W4313596887 date "2023-01-06" @default.
- W4313596887 modified "2023-10-14" @default.
- W4313596887 title "Quantification of gas, ash, and sulphate aerosols in volcanic plumes from open path Fourier transform infrared (OP-FTIR) emission measurements at Stromboli volcano, Italy" @default.
- W4313596887 cites W1152347994 @default.
- W4313596887 cites W1503587868 @default.
- W4313596887 cites W1535295956 @default.
- W4313596887 cites W1599143530 @default.
- W4313596887 cites W1604919557 @default.
- W4313596887 cites W1964202260 @default.
- W4313596887 cites W1969919340 @default.
- W4313596887 cites W1978390008 @default.
- W4313596887 cites W1982208526 @default.
- W4313596887 cites W1986402681 @default.
- W4313596887 cites W1987399586 @default.
- W4313596887 cites W1990885281 @default.
- W4313596887 cites W1991138062 @default.
- W4313596887 cites W1998579795 @default.
- W4313596887 cites W2000158228 @default.
- W4313596887 cites W2002652137 @default.
- W4313596887 cites W2004063237 @default.
- W4313596887 cites W2012097073 @default.
- W4313596887 cites W2017390323 @default.
- W4313596887 cites W2022330856 @default.
- W4313596887 cites W2028147785 @default.
- W4313596887 cites W2028637388 @default.
- W4313596887 cites W2034543711 @default.
- W4313596887 cites W2042742770 @default.
- W4313596887 cites W2043442500 @default.
- W4313596887 cites W2044221233 @default.
- W4313596887 cites W2044643221 @default.
- W4313596887 cites W2045585210 @default.
- W4313596887 cites W2050322368 @default.
- W4313596887 cites W2059095941 @default.
- W4313596887 cites W2061593412 @default.
- W4313596887 cites W2062848117 @default.
- W4313596887 cites W2067235826 @default.
- W4313596887 cites W2074725516 @default.
- W4313596887 cites W2074766303 @default.
- W4313596887 cites W2076537805 @default.
- W4313596887 cites W2076811641 @default.
- W4313596887 cites W2091162995 @default.
- W4313596887 cites W2094105589 @default.
- W4313596887 cites W2094339759 @default.
- W4313596887 cites W2095481647 @default.
- W4313596887 cites W2105671256 @default.
- W4313596887 cites W2109103034 @default.
- W4313596887 cites W2117235313 @default.
- W4313596887 cites W2122752600 @default.
- W4313596887 cites W2123817555 @default.
- W4313596887 cites W2123859765 @default.
- W4313596887 cites W2131021676 @default.
- W4313596887 cites W2136473486 @default.
- W4313596887 cites W2144643813 @default.
- W4313596887 cites W2146419431 @default.
- W4313596887 cites W2160890167 @default.
- W4313596887 cites W2170879631 @default.
- W4313596887 cites W2262235569 @default.
- W4313596887 cites W2405339256 @default.
- W4313596887 cites W243376709 @default.
- W4313596887 cites W2471941619 @default.
- W4313596887 cites W2510108218 @default.
- W4313596887 cites W2598114332 @default.
- W4313596887 cites W2613170259 @default.
- W4313596887 cites W2616251295 @default.
- W4313596887 cites W273108663 @default.
- W4313596887 cites W2757093426 @default.
- W4313596887 cites W2766439646 @default.
- W4313596887 cites W2781534587 @default.
- W4313596887 cites W2784008316 @default.
- W4313596887 cites W2902070904 @default.
- W4313596887 cites W2917595964 @default.
- W4313596887 cites W2923867875 @default.
- W4313596887 cites W2948052787 @default.
- W4313596887 cites W2952215413 @default.
- W4313596887 cites W2953867413 @default.
- W4313596887 cites W2981203473 @default.
- W4313596887 cites W3001312438 @default.
- W4313596887 cites W3004015706 @default.
- W4313596887 cites W3033755488 @default.
- W4313596887 cites W3037817234 @default.
- W4313596887 cites W3043215291 @default.
- W4313596887 cites W3093913501 @default.
- W4313596887 cites W3112237765 @default.
- W4313596887 cites W3120130378 @default.
- W4313596887 cites W3146733302 @default.
- W4313596887 cites W3159918571 @default.
- W4313596887 cites W3207929528 @default.
- W4313596887 cites W4205182410 @default.
- W4313596887 cites W4211242048 @default.
- W4313596887 cites W4225771358 @default.