P-Alert earthquake early warning system: case study of the 2022 Chishang earthquake at Taitung, Taiwan

被引:0
|
作者
Yang, Benjamin M. [1 ]
Mittal, Himanshu [2 ]
Wu, Yih-Min [1 ,3 ,4 ]
机构
[1] Natl Taiwan Univ, Dept Geosci, Taipei 10617, Taiwan
[2] Govt India, Minist Earth Sci, Natl Ctr Seismol, New Delhi 110003, India
[3] Acad Sinica, Inst Earth Sci, Taipei 11529, Taiwan
[4] Natl Taiwan Univ, Res Ctr Future Earth, Taipei 10617, Taiwan
来源
关键词
Earthquake early warning; On-site; Shake maps; Regional; PGA; PGV; SEISMIC NETWORK; HUALIEN; INVERSION; MAPS;
D O I
10.1007/s44195-023-00057-z
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
A series of earthquakes that struck Taiwan's southern Longitudinal Valley on September 17 and 18, 2022 severely damaged several buildings in Taitung and Hualien. The Chishang earthquake, which had a magnitude of M-L 6.8 and a large foreshock with a magnitude of M-L 6.6 the day before, was the mainshock in this sequence. The strongest intensity reported in the epicentral region during this earthquake sequence, which was 6 + , is the highest ever recorded since the Central Weather Bureau (CWB, renamed as the Central Weather Administration since September 15, 2023) revised its seismic intensity scale. National Taiwan University (NTU) has operated a low-cost earthquake early warning (EEW) system known as the P-Alert for a decade. In this study, we demonstrate the performance of the P-Alert network during the 2022 Chishang earthquake and the largest foreshock. The P-Alert network plotted shake maps during these earthquakes that displayed various values within 5 min. The high shaking areas on these maps were in good agreement with observed damages during this earthquake, providing valuable insights into rupture directivity, a crucial component of earthquake engineering. Individual P-Alert stations acted as on-site EEW systems and provided a lead time of 3-10 s within the blind zone of CWB. For the M-L 6.8 mainshock, there was a lead time of at least 5 s, even up to 10 s, demonstrating their effectiveness in the blind zone. The P-Alert regional EEW system provided the first report about 9 s and 7 s after the mainshock and the largest foreshock occurrence, respectively, with estimated magnitudes of 5.74 and 5.67. The CWB system estimated magnitudes of 6.72 and 6.16 in the first report, respectively, about 7 s and 9 s after the earthquake occurrence. The timeliness of the two systems were not significantly different. Despite the effectiveness of the P-Alert network, data loss due to connection interruptions prompted us to develop a new compact data logger for improved data availability.
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页数:14
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