• Login
     
    View Item 
    •   ORFEO Home
    • Royal Belgian Institute for Space Aeronomy
    • BIRA-IASB publications
    • View Item
    •   ORFEO Home
    • Royal Belgian Institute for Space Aeronomy
    • BIRA-IASB publications
    • View Item
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Volcanic SO2 by UV-TIR satellite retrievals: Validation by using ground-based network at Mt. Etna

    Thumbnail
    View/Open
    Spinetti(2014).pdf (398.0Kb)
    Authors
    Spinetti, C.
    Salerno, G.G.
    Caltabiano, T.
    Carboni, E.
    Clarisse, L.
    Corradini, S.
    Grainger, R.G.
    Hedelt, P.A.
    Koukouli, M.E.
    Merucci, L.
    Siddans, R.
    Tampellini, L.
    Theys, N.
    Valks, P.
    Zehner, C.
    Show allShow less
    Discipline
    Earth and related Environmental sciences
    Subject
    degassing
    error analysis
    GOME
    ground-based measurement
    IASI
    MODIS
    satellite data
    sulfur dioxide
    volcanic gas
    volcanology
    Catania [Sicily]
    Etna
    Italy
    Sicily
    Audience
    Scientific
    Date
    2014
    Metadata
    Show full item record
    Description
    Mt. Etna volcano in Italy is one of the most active degassing volcanoes worldwide, emitting a mean of 1.7 Mt/year of Sulphur Dioxide (SO2) in quiescent periods. In this work, SO2 measurements retrieved by Moderate Resolution Imaging Spectroradiometer (MODIS), hyper-spectral Infrared Atmospheric Sounding Interferometer (IASI) and the second Global Ozone Monitoring Experiment (GOME-2) data are compared with the ground-based data from the FLux Automatic MEasurement monitoring network (FLAME). Among the eighteen lava fountain episodes occurring at Mt. Etna in 2011, the 10 April paroxysmal event has been selected as a case-study for the simultaneous observation of the SO2 cloud by satellite and ground-based sensors. For each data-set two retrieval techniques were adopted and the measurements of SO2 mass and flux with their respective uncertainty were obtained. With respect to the FLAME SO2 mass of 4.5 Gg, MODIS, IASI and GOME-2 differ by about 10%, 15% and 30%, respectively. The SO2 flux correlation coefficient between MODIS and FLAME is 0.84. All the retrievals within the respective errors are in agreement with the ground-based measurements supporting the validity of these space measurements.
    Citation
    Spinetti, C.; Salerno, G.G.; Caltabiano, T.; Carboni, E.; Clarisse, L.; Corradini, S.; Grainger, R.G.; Hedelt, P.A.; Koukouli, M.E.; Merucci, L.; Siddans, R.; Tampellini, L.; Theys, N.; Valks, P.; Zehner, C. (2014). Volcanic SO2 by UV-TIR satellite retrievals: Validation by using ground-based network at Mt. Etna. , Annals of Geophysics, Vol. 57, Issue FastTrack2, DOI: 10.4401/ag-6641.
    Identifiers
    uri: https://orfeo.belnet.be/handle/internal/4277
    doi: http://dx.doi.org/10.4401/ag-6641
    scopus: 2-s2.0-84940882368
    Type
    Article
    Peer-Review
    Yes
    Language
    eng
    Links
    NewsHelpdeskBELSPO OA Policy

    Browse

    All of ORFEOCommunities & CollectionsBy Issue DateAuthorsTitlesDisciplinesThis CollectionBy Issue DateAuthorsTitlesDisciplines
     

    DSpace software copyright © 2002-2016  DuraSpace
    Send Feedback | Cookie Information
    Theme by 
    Atmire NV