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First comparison of measurements of Ka-band cloud radar with lightning in Central Europe

  1. 1.
    SYSNO ASEP0508141
    Document TypeC - Proceedings Paper (int. conf.)
    R&D Document TypeConference Paper
    TitleFirst comparison of measurements of Ka-band cloud radar with lightning in Central Europe
    Author(s) Minářová, Jana (UFA-U) RID, ORCID
    Sokol, Zbyněk (UFA-U) RID, ORCID
    Pešice, Petr (UFA-U) RID, ORCID
    Number of authors3
    Article number8815957
    Source Title2019 11th Asia-Pacific International Conference on Lightning (APL). - Piscataway : IEEE, 2019 - ISBN 978-1-7281-1694-5
    Pagess. 1-6
    Number of pages6 s.
    Publication formOnline - E
    ActionAsia-Pacific International Conference on Lightning (APL2019) /11./
    Event date12.06.2019 - 14.06.2019
    VEvent locationHong Kong
    CountryCN - China
    Event typeWRD
    Languageeng - English
    CountryUS - United States
    Keywordscloud radar ; lightning ; hydrometeor ; vertical air velocity ; convection ; Ka-band
    Subject RIVDG - Athmosphere Sciences, Meteorology
    OECD categoryMeteorology and atmospheric sciences
    Institutional supportUFA-U - RVO:68378289
    EID SCOPUS85072324572
    DOI10.1109/APL.2019.8815957
    AnnotationSituated in Central Europe, the Milešovka observatory was equipped with a vertically oriented Ka-band cloud radar (35 GHz) in spring 2018. We analysed strong convective events that were observed in summer 2018 at the observatory and were detected by the cloud radar, which read high reflectivity values. We applied our algorithm treating the radar data to retrieve vertical air velocity and five types of hydrometeors and we conducted a comparative study of the results with ground-based measurements of lightning. The study showed that hail and rain are the two hydrometeors, which clearly tend to be more frequent in convective clouds that are situated above the cloud radar, when a lightning is recorded in the vicinity of the Milešovka observatory. Similarly, in case of nearby lightning downdrafts are observed at lower altitudes (up to 4 km above the radar), whereas slight updrafts are more typical for higher altitudes above the radar.
    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 Publishing2020
    Electronic addresshttps://ieeexplore.ieee.org/document/8815957
Number of the records: 1  

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