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Horizontal velocities and propagation directions of gravity waves in the ionosphere over the Czech Republic

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    SYSNO ASEP0350501
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleHorizontal velocities and propagation directions of gravity waves in the ionosphere over the Czech Republic
    Author(s) Chum, Jaroslav (UFA-U) RID, ORCID
    Šindelářová, Tereza (UFA-U) RID, ORCID
    Laštovička, Jan (UFA-U) RID, ORCID
    Hruška, František (UFA-U) RID
    Burešová, Dalia (UFA-U) RID, ORCID
    Baše, Jiří (UFA-U) RID, ORCID
    Source TitleJournal of Geophysical Research - ISSN 0148-0227
    Roč. 115, - (2010), A11322/1-A11322/13
    Number of pages13 s.
    Languageeng - English
    CountryUS - United States
    KeywordsIonosphere ; gravity waves ; wave propagation ; remote sensing
    Subject RIVBL - Plasma and Gas Discharge Physics
    R&D ProjectsGA205/07/1367 GA ČR - Czech Science Foundation (CSF)
    GA205/09/1253 GA ČR - Czech Science Foundation (CSF)
    CEZAV0Z30420517 - UFA-U, BC-A (2005-2011)
    UT WOS000284708300005
    DOI10.1029/2010JA015821
    AnnotationUsing a five-point continuous Doppler sounding system operating at 3.59 MHz we investigate propagation directions and velocities of gravity waves (GWs) at altitudes from ~150 to ~250 km over the western part of the Czech Republic. The velocities and directions are computed from the time delays between the observations of corresponding GWs at different reflection points that correspond to various sounding paths. We focused on the GWs that produce an S-shaped trace in Doppler shift spectrograms and are observed close to sunrise and sunset. We have selected about 100 of such events. Our results show that the analyzed GWs propagate with typical horizontal velocities from ~100 to ~200 m/s. The north-south component of GW velocities depends on the season, it is directed northward in the summer and southward in the winter. At the same time, the north-south component of the neutral winds calculated by the horizontal wind model HWM07 has the opposite sign.
    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 Publishing2011
Number of the records: 1  

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