Počet záznamů: 1  

The vertical propagation of disturbances triggered by seismic waves of the 11 March 2011 M9.0 Tohoku earthquake over Taiwan

  1. 1.
    SYSNO ASEP0458523
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevThe vertical propagation of disturbances triggered by seismic waves of the 11 March 2011 M9.0 Tohoku earthquake over Taiwan
    Tvůrce(i) Liu, J. Y. (TW)
    Chen, C. H. (TW)
    Sun, Y. Y. (TW)
    Chen, C. (TW)
    Tsai, H. F. (TW)
    Yen, H. Y. (TW)
    Chum, Jaroslav (UFA-U) RID, ORCID
    Laštovička, Jan (UFA-U) RID, ORCID
    Yang, Q. S. (TW)
    Chen, W. S. (CN)
    Wen, S. (TW)
    Celkový počet autorů11
    Zdroj.dok.Geophysical Research Letters. - : Wiley - ISSN 0094-8276
    Roč. 43, č. 4 (2016), s. 1759-1765
    Poč.str.7 s.
    Jazyk dok.eng - angličtina
    Země vyd.US - Spojené státy americké
    Klíč. slovaionospheric disturbances ; Pacific Coast ; surface-waves ; Tohoku-oki earthquake ; ionograms
    Vědní obor RIVDG - Vědy o atmosféře, meteorologie
    CEPGC15-07281J GA ČR - Grantová agentura ČR
    Institucionální podporaUFA-U - RVO:68378289
    UT WOS000373109000045
    EID SCOPUS84977856310
    DOI10.1002/2015GL067487
    AnotaceIn this paper, concurrent/colocated measurements of seismometers, infrasonic systems, magnetometers, HF-CW (high frequency-continuous wave) Doppler sounding systems, and GPS receivers are employed to detect disturbances triggered by seismic waves of the 11 March 2011M9.0 Tohoku earthquake. No time delay between colocated infrasonic (i.e., super long acoustic) waves and seismic waves indicates that the triggered acoustic and/or gravity waves in the atmosphere (or seismo-traveling atmospheric disturbances, STADs) near the Earth's surface can be immediately activated by vertical ground motions. The circle method is used to find the origin and compute the observed horizontal traveling speed of the triggered infrasonic waves. The speed of about 3.3km/s computed from the arrival time versus the epicentral distance suggests that the infrasonic waves (i.e., STADs) are mainly induced by the Rayleigh waves. The agreements in the travel time at various heights between the observation and theoretical calculation suggest that the STADs triggered by the vertical motion of ground surface caused by the Tohoku earthquake traveled vertically from the ground to the ionosphere with speed of the sound in the atmosphere over Taiwan.
    PracovištěÚstav fyziky atmosféry
    KontaktKateřina Adamovičová, adamovicova@ufa.cas.cz, Tel.: 272 016 012 ; Kateřina Potužníková, kaca@ufa.cas.cz, Tel.: 272 016 019
    Rok sběru2017
Počet záznamů: 1  

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