Opportunistic validation of sulfur dioxide in the Sarychev Peak volcanic eruption cloud

We report attempted validation of Ozone Monitoring Instrument (OMI) sulfur dioxide (SO<sub>2</sub>) retrievals in the stratospheric volcanic cloud from Sarychev Peak (Kurile Islands) in June 2009, through opportunistic deployment of a ground-based ultraviolet (UV) spectro...

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Main Authors: T. M. Lopez, S. A. Carn
Format: Article
Language:English
Published: Copernicus Publications 2011-09-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/4/1705/2011/amt-4-1705-2011.pdf
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spelling doaj-2e607a4f235d43398d13c3907eacd2e92020-11-24T23:27:14ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482011-09-01491705171210.5194/amt-4-1705-2011Opportunistic validation of sulfur dioxide in the Sarychev Peak volcanic eruption cloudT. M. LopezS. A. CarnWe report attempted validation of Ozone Monitoring Instrument (OMI) sulfur dioxide (SO<sub>2</sub>) retrievals in the stratospheric volcanic cloud from Sarychev Peak (Kurile Islands) in June 2009, through opportunistic deployment of a ground-based ultraviolet (UV) spectrometer (FLYSPEC) as the volcanic cloud drifted over central Alaska. The volcanic cloud altitude (~12–14 km) was constrained using coincident CALIPSO lidar observations. By invoking some assumptions about the spatial distribution of SO<sub>2</sub>, we derive averages of FLYSPEC vertical SO<sub>2</sub> columns for comparison with OMI SO<sub>2</sub> measurements. Despite limited data, we find minimum OMI-FLYSPEC differences within measurement uncertainties, which support the validity of the operational OMI SO<sub>2</sub> algorithm. However, our analysis also highlights the challenges involved in comparing datasets representing markedly different spatial and temporal scales. This effort represents the first attempt to validate SO<sub>2</sub> in a stratospheric volcanic cloud using a mobile ground-based instrument, and demonstrates the need for a network of rapidly deployable instruments for validation of space-based volcanic SO<sub>2</sub> measurements.http://www.atmos-meas-tech.net/4/1705/2011/amt-4-1705-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author T. M. Lopez
S. A. Carn
spellingShingle T. M. Lopez
S. A. Carn
Opportunistic validation of sulfur dioxide in the Sarychev Peak volcanic eruption cloud
Atmospheric Measurement Techniques
author_facet T. M. Lopez
S. A. Carn
author_sort T. M. Lopez
title Opportunistic validation of sulfur dioxide in the Sarychev Peak volcanic eruption cloud
title_short Opportunistic validation of sulfur dioxide in the Sarychev Peak volcanic eruption cloud
title_full Opportunistic validation of sulfur dioxide in the Sarychev Peak volcanic eruption cloud
title_fullStr Opportunistic validation of sulfur dioxide in the Sarychev Peak volcanic eruption cloud
title_full_unstemmed Opportunistic validation of sulfur dioxide in the Sarychev Peak volcanic eruption cloud
title_sort opportunistic validation of sulfur dioxide in the sarychev peak volcanic eruption cloud
publisher Copernicus Publications
series Atmospheric Measurement Techniques
issn 1867-1381
1867-8548
publishDate 2011-09-01
description We report attempted validation of Ozone Monitoring Instrument (OMI) sulfur dioxide (SO<sub>2</sub>) retrievals in the stratospheric volcanic cloud from Sarychev Peak (Kurile Islands) in June 2009, through opportunistic deployment of a ground-based ultraviolet (UV) spectrometer (FLYSPEC) as the volcanic cloud drifted over central Alaska. The volcanic cloud altitude (~12–14 km) was constrained using coincident CALIPSO lidar observations. By invoking some assumptions about the spatial distribution of SO<sub>2</sub>, we derive averages of FLYSPEC vertical SO<sub>2</sub> columns for comparison with OMI SO<sub>2</sub> measurements. Despite limited data, we find minimum OMI-FLYSPEC differences within measurement uncertainties, which support the validity of the operational OMI SO<sub>2</sub> algorithm. However, our analysis also highlights the challenges involved in comparing datasets representing markedly different spatial and temporal scales. This effort represents the first attempt to validate SO<sub>2</sub> in a stratospheric volcanic cloud using a mobile ground-based instrument, and demonstrates the need for a network of rapidly deployable instruments for validation of space-based volcanic SO<sub>2</sub> measurements.
url http://www.atmos-meas-tech.net/4/1705/2011/amt-4-1705-2011.pdf
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