Počet záznamů: 1  

Size dependence of ozone lamina characteristics and their correlations

  1. 1.
    SYSNO ASEP0445956
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevSize dependence of ozone lamina characteristics and their correlations
    Tvůrce(i) Križan, Peter (UFA-U) RID, ORCID
    Laštovička, Jan (UFA-U) RID, ORCID
    Kozubek, Michal (UFA-U) RID, ORCID
    Zdroj.dok.Journal of Atmospheric and Solar-Terrestrial Physics. - : Elsevier - ISSN 1364-6826
    Roč. 132, September (2015), s. 116-123
    Poč.str.8 s.
    Forma vydáníTištěná - P
    Jazyk dok.eng - angličtina
    Země vyd.GB - Velká Británie
    Klíč. slovaozone laminae ; correlations among laminae ; vertical resolution of ozonesonde measurements
    Vědní obor RIVDG - Vědy o atmosféře, meteorologie
    CEPGA15-03909S GA ČR - Grantová agentura ČR
    Institucionální podporaUFA-U - RVO:68378289
    UT WOS000359167500013
    EID SCOPUS84937231593
    DOI10.1016/j.jastp.2015.06.017
    AnotaceOzone 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.
    PracovištěÚstav fyziky atmosféry
    KontaktKateřina Adamovičová, adamovicova@ufa.cas.cz, Tel.: 272 016 012 ; Kateřina Potužníková, kaca@ufa.cas.cz, Tel.: 272 016 019
    Rok sběru2016
Počet záznamů: 1  

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