Number of the records: 1  

Size dependence of ozone lamina characteristics and their correlations

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    SYSNO ASEP0445956
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleSize dependence of ozone lamina characteristics and their correlations
    Author(s) Križan, Peter (UFA-U) RID, ORCID
    Laštovička, Jan (UFA-U) RID, ORCID
    Kozubek, Michal (UFA-U) RID, ORCID
    Source TitleJournal of Atmospheric and Solar-Terrestrial Physics. - : Elsevier - ISSN 1364-6826
    Roč. 132, September (2015), s. 116-123
    Number of pages8 s.
    Publication formPrint - P
    Languageeng - English
    CountryGB - United Kingdom
    Keywordsozone laminae ; correlations among laminae ; vertical resolution of ozonesonde measurements
    Subject RIVDG - Athmosphere Sciences, Meteorology
    R&D ProjectsGA15-03909S GA ČR - Czech Science Foundation (CSF)
    Institutional supportUFA-U - RVO:68378289
    UT WOS000359167500013
    EID SCOPUS84937231593
    DOI10.1016/j.jastp.2015.06.017
    AnnotationOzone profiles contain narrow layers of substantially enhanced or reduced ozone, called positive and negative laminae, respectively. They reflect both evolutions of stratospheric ozone content and stratospheric dynamics. Here we deal only with positive laminae. The following lamina characteristics are investigated in dependence on lamina size: the number of laminae per profile, the overall ozone amount in laminae per profile and the ozone amount in one lamina at the European ozonosonde stations. An important role of the vertical resolution of ozonesonde measurements is specified. Lamina characteristics for Legionowo and Lindenberg, and small lamina (o2 mPa) characteristics for all stations suffer with effects of vertical resolution of measurements. For this reason they are not used here for long-term trend investigations. The long-term evolution of the ozone amount in one lamina does not display a trend. The results for the three remaining stations, Hohenpeissenberg, Payerne and Uccle, are largely consistent with our previous results on lamina behaviour, which means that our previous results on trends in laminae (e.g., Križan and Laštovička, 2005; Laštovička et al., 2014) are basically correct.
    WorkplaceInstitute of Atmospheric Physics
    ContactKateřina Adamovičová, adamovicova@ufa.cas.cz, Tel.: 272 016 012 ; Kateřina Potužníková, kaca@ufa.cas.cz, Tel.: 272 016 019
    Year of Publishing2016
Number of the records: 1  

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