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    Comparisons of MIPAS O3 profiles with ground-based measurements

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    Authors
    Blumenstock, T.
    Mikuteit, S.
    Hase, F.
    Boyd, I.
    Calisesi, Y.
    Declercq, C.
    Lambert, J.-C.
    Koopman, R.
    McDermid, S.
    Oltmans, S.
    Swart, D.
    Raffalski, U.
    Schets, H.
    De Muer, D.
    Steinbrecht, W.
    Stubi, R.
    Wood, S.
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    Discipline
    Earth and related Environmental sciences
    Subject
    Computer software
    Data reduction
    Graph theory
    Optical radar
    Project management
    Upper atmosphere
    Error bars
    Ground-based data
    Ground-based measurements
    Sondes
    Ozone
    Audience
    Scientific
    Date
    2004
    Metadata
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    Description
    For the ENVISAT validation different ground-based techniques have been used. MIPAS O3 profiles have been compared with data from different ground-based techniques such as FTIR, LIDAR, O3 sondes, and MWR. All instruments used are operated within the NDSC (Network for the Detection of Stratospheric Change). These comparisons covering different techniques as well as different latitudes show a consistent picture. Within 20 to 40 km MIPAS O3 profiles are in good agreement with ground-based data. Here, the differences are within the combined error bars. Below 20 km and above 50 km the differences are increasing. At these altitudes MIPAS VMR values tends to be a bit too large.
    Citation
    Blumenstock, T.; Mikuteit, S.; Hase, F.; Boyd, I.; Calisesi, Y.; Declercq, C.; Lambert, J.-C.; Koopman, R.; McDermid, S.; Oltmans, S.; Swart, D.; Raffalski, U.; Schets, H.; De Muer, D.; Steinbrecht, W.; Stubi, R.; Wood, S. (2004). Comparisons of MIPAS O3 profiles with ground-based measurements. , ESA-SP 562, Proceedings of the Second Workshop on the Atmospheric Chemistry Validation of ENVISAT (ACVE-2), Issue 562, 151-157,
    Identifiers
    uri: https://orfeo.belnet.be/handle/internal/5097
    scopus: 2-s2.0-20844443994
    Type
    Conference
    Peer-Review
    No
    Language
    eng
    Links
    NewsHelpdeskBELSPO OA Policy

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