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Doppler Frequency Shifts Associated With the 18 September 2022 M6.8 Taitung Earthquake Observed by Local CW-HF Doppler Sounding Systems in Taiwan

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F25%3A00638497" target="_blank" >RIV/68378289:_____/25:00638497 - isvavai.cz</a>

  • Výsledek na webu

    <a href="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025JA033876" target="_blank" >https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025JA033876</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1029/2025JA033876" target="_blank" >10.1029/2025JA033876</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Doppler Frequency Shifts Associated With the 18 September 2022 M6.8 Taitung Earthquake Observed by Local CW-HF Doppler Sounding Systems in Taiwan

  • Popis výsledku v původním jazyce

    Doppler frequency shifts (DFSs) recorded by local continuous wave-high frequency (CW-HF) Doppler sounding systems have been used to study seismo-traveling ionospheric disturbances (STIDs) triggered by seismic waves of M ≥ 5.5 earthquakes in the Taiwan vicinity during 2000–2022. We observed the first significant STID in DFSs induced by the 18 September 2022 M6.8 Taitung earthquake. To investigate this significant STID in more detail, DFSs of five sounding frequencies recorded by a network of nine receiving stations of the CW-HF Doppler sounding systems, together with the total electron content (TEC) derived by 35 ground-based GPS receivers, ionograms, and seismograms, are examined. Results show that horizontal speeds of the significant STID in DFSs of the 6.1 MHz sounding frequency and in TECs are 1.4 and 1.3 km/s, respectively. Upward propagation with a speed of sound of 0.72 km/s is estimated through DFSs of the five sounding frequencies, where the reflection heights are about 160–225 km altitude. We further examine DFSs associated with the top nine earthquakes in the Taiwan vicinity during 2022–2023. Results show that for near field observations, in addition to the earthquake magnitude, the total earthquake intensity plays an important role in triggering significant STIDs.

  • Název v anglickém jazyce

    Doppler Frequency Shifts Associated With the 18 September 2022 M6.8 Taitung Earthquake Observed by Local CW-HF Doppler Sounding Systems in Taiwan

  • Popis výsledku anglicky

    Doppler frequency shifts (DFSs) recorded by local continuous wave-high frequency (CW-HF) Doppler sounding systems have been used to study seismo-traveling ionospheric disturbances (STIDs) triggered by seismic waves of M ≥ 5.5 earthquakes in the Taiwan vicinity during 2000–2022. We observed the first significant STID in DFSs induced by the 18 September 2022 M6.8 Taitung earthquake. To investigate this significant STID in more detail, DFSs of five sounding frequencies recorded by a network of nine receiving stations of the CW-HF Doppler sounding systems, together with the total electron content (TEC) derived by 35 ground-based GPS receivers, ionograms, and seismograms, are examined. Results show that horizontal speeds of the significant STID in DFSs of the 6.1 MHz sounding frequency and in TECs are 1.4 and 1.3 km/s, respectively. Upward propagation with a speed of sound of 0.72 km/s is estimated through DFSs of the five sounding frequencies, where the reflection heights are about 160–225 km altitude. We further examine DFSs associated with the top nine earthquakes in the Taiwan vicinity during 2022–2023. Results show that for near field observations, in addition to the earthquake magnitude, the total earthquake intensity plays an important role in triggering significant STIDs.

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    10509 - Meteorology and atmospheric sciences

Návaznosti výsledku

  • Projekt

  • Návaznosti

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Ostatní

  • Rok uplatnění

    2025

  • Kód důvěrnosti údajů

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Údaje specifické pro druh výsledku

  • Název periodika

    Journal of Geophysical Research-Space Physics

  • ISSN

    2169-9380

  • e-ISSN

    2169-9402

  • Svazek periodika

    130

  • Číslo periodika v rámci svazku

    9

  • Stát vydavatele periodika

    US - Spojené státy americké

  • Počet stran výsledku

    9

  • Strana od-do

    e2025JA033876

  • Kód UT WoS článku

    001563162800001

  • EID výsledku v databázi Scopus

    2-s2.0-105014618756