Počet záznamů: 1  

Simultaneous infrasonic, seismic, magnetic and ionospheric observations in an earthquake epicentre

  1. 1.
    SYSNO ASEP0348450
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevSimultaneous infrasonic, seismic, magnetic and ionospheric observations in an earthquake epicentre
    Tvůrce(i) Laštovička, Jan (UFA-U) RID, ORCID
    Baše, Jiří (UFA-U) RID, ORCID
    Hruška, František (UFA-U) RID
    Chum, Jaroslav (UFA-U) RID, ORCID
    Šindelářová, Tereza (UFA-U) RID, ORCID
    Horálek, Josef (GFU-E) ORCID, RID
    Zedník, Jan (GFU-E) ORCID, RID
    Krasnov, V. (RU)
    Zdroj.dok.Journal of Atmospheric and Solar-Terrestrial Physics. - : Elsevier - ISSN 1364-6826
    Roč. 72, č. 16 (2010), s. 1231-1240
    Poč.str.10 s.
    Jazyk dok.eng - angličtina
    Země vyd.GB - Velká Británie
    Klíč. slovaEarthquake ; Infrasonic effects ; Ionospheric effects ; Magnetic effects
    Vědní obor RIVDG - Vědy o atmosféře, meteorologie
    CEPGA205/07/1367 GA ČR - Grantová agentura ČR
    CEZAV0Z30420517 - UFA-U, BC-A (2005-2011)
    AV0Z30120515 - GFU-E (2005-2011)
    UT WOS000283410100012
    DOI10.1016/j.jastp.2010.08.005
    AnotaceWe analyze the co-seismic effects of a relatively weak earthquake of 28 October 2008, which was a part of an earthquake swarm in the westernmost region of the Czech Republic. Special attention is paid to unique measurements of infrasonic phenomena. As far as we know, these have been the first infrasonic measurements during earthquake in the epicentre zone. Infrasonic oscillations (~1–12 Hz) in the epicentre region appear to be excited essentially by the vertical seismic oscillations. The observed oscillations are real epicentral infrasound not caused by seismic shaking of the instruments or by meteorological phenomena. Seismo-infrasonic oscillations observed 155 km apart from the epicentre were excited in situ by seismic waves. No earthquake-related infrasonic effects have been observed in the ionosphere. Necessity to make vibration tests of instruments is pointed out in order to be sure that observed effects are not effects of mechanical shaking of the instrument.
    PracovištěÚstav fyziky atmosféry
    KontaktKateřina Adamovičová, adamovicova@ufa.cas.cz, Tel.: 272 016 012 ; Kateřina Potužníková, kaca@ufa.cas.cz, Tel.: 272 016 019
    Rok sběru2011
Počet záznamů: 1  

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