Number of the records: 1  

Signatures of storm Opheliain microbarom measurements in the Czech Republicon 15-18 October 2017

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    SYSNO ASEP0490237
    Document TypeA - Abstract
    R&D Document TypeThe record was not marked in the RIV
    R&D Document TypeNení vybrán druh dokumentu
    TitleSignatures of storm Opheliain microbarom measurements in the Czech Republicon 15-18 October 2017
    Author(s) Šindelářová, Tereza (UFA-U) RID, ORCID
    Kozubek, Michal (UFA-U) RID, ORCID
    Chum, Jaroslav (UFA-U) RID, ORCID
    Baše, Jiří (UFA-U) RID, ORCID
    Potužníková, Kateřina (UFA-U) RID, ORCID
    Source TitleGeophysical Research Abstracts, EGU General Assembly 2018, Vol. 20. - Göttingen : European Geosciences Union, 2018
    EGU2018-4367-1
    Number of pages1 s.
    Publication formOnline - E
    ActionEGU General Assembly 2018
    Event date08.04.2018 - 13.04.2018
    VEvent locationVienna
    CountryAT - Austria
    Event typeWRD
    Languageeng - English
    CountryDE - Germany
    Keywordsmicrobarom ; hurricane
    Subject RIVDG - Athmosphere Sciences, Meteorology
    OECD categoryMeteorology and atmospheric sciences
    Institutional supportUFA-U - RVO:68378289
    AnnotationA change in microbarom arrivals was observed at Panska Ves array (50◦32’W 14◦34‘E) between 15 October 2017, 21:07 UTC and 16 October 2017, 04:22 UTC. The azimuth of arrival turned from the usually observed direction of 310◦ to 260◦. Then, during 16-18 October 2017, the back-azimuth gradually returned to the values around 300-310◦. The observed microbarom back-azimuths followed the track of the storm Ophelia. The signal elevation increased from 26◦ to 36◦ between 21:07 and 00:39 UTC on 15/16 October 2017. By way of contrast, on 14 October and 17 October 2017 elevations between 20◦ and 30◦ prevailed. The increase of RMS signal amplitudes was observed during the event, particularly at frequencies around 0.2 Hz. The storm Ophelia (former hurricane Ophelia) travelled above the eastern Atlantic along western coast of Europe to the North East between 15 and 17 October 2017. It was accompanied by winds of speed 20-40 m/s (from www.nhc.noaa.gov). We assume that the storm was able to shift the microbarom source region transitorily from the Northern Atlantic to localities along the Ophelia trajectory above the Eastern Atlantic.
    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 Publishing2019
Number of the records: 1  

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