Počet záznamů: 1  

Long-term trends in the northern extratropical ozone laminae with focus on European stations

  1. 1.
    0431929 - ÚFA 2015 RIV GB eng J - Článek v odborném periodiku
    Laštovička, Jan - Križan, Peter - Kozubek, Michal
    Long-term trends in the northern extratropical ozone laminae with focus on European stations.
    Journal of Atmospheric and Solar-Terrestrial Physics. Roč. 120, December (2014), s. 88-95. ISSN 1364-6826. E-ISSN 1879-1824
    Grant CEP: GA MŠMT LD12070; GA ČR GAP209/10/1792
    Institucionální podpora: RVO:68378289
    Klíčová slova: ozone laminae * long-term trends * atmospheric dynamics
    Kód oboru RIV: DG - Vědy o atmosféře, meteorologie
    Impakt faktor: 1.474, rok: 2014
    http://www.sciencedirect.com/science/article/pii/S1364682614002119

    Narrow layers of substantially enhanced ozone concentration in ozonesonde-observed ozone profiles, called positive ozone laminae, reveal much stronger trend than the stratospheric and total ozone itself. They seem to be sensitive to both the ozone concentration and even more to changes in the stratospheric dynamics. We are studying long-term trends of strong positive laminae based on balloon-borne ozone sounding in Europe, Japan, North America and Arctic over 1970–2011 with focus on European stations due to their highest frequency of ozone sounding. Laminae characteristics exhibit strong negative trend till the mid-1990s (decrease by 50% or more). In more recent years this negative trend reverses to a positive trend. According to regression analysis, several factors play a role in the trend in laminae in Europe, namely NAO, EESC and the behavior of the winter polar stratospheric vortex represented here by the 10 hPa polar temperature. On the other hand, several factors are found not to play a significant role in the long-term trend in laminae.
    Trvalý link: http://hdl.handle.net/11104/0236451

     
     
Počet záznamů: 1  

  Tyto stránky využívají soubory cookies, které usnadňují jejich prohlížení. Další informace o tom jak používáme cookies.