The Propagation of Local Undamped Motion (PLUM) Method: A Simple and Robust Seismic Wavefield Estimation Approach for Earthquake Early Warning

被引:81
作者
Kodera, Yuki [1 ]
Yamada, Yasuyuki [2 ]
Hirano, Kazuyuki [3 ]
Tamaribuchi, Koji [1 ]
Adachi, Shimpei [2 ]
Hayashimoto, Naoki [2 ]
Morimoto, Masahiko [2 ]
Nakamura, Masaki [4 ]
Hoshiba, Mitsuyuki [1 ]
机构
[1] Japan Meteorol Agcy, Meteorol Res Inst, 1-1 Nagamine, Tsukuba, Ibaraki 3050052, Japan
[2] Japan Meteorol Agcy, Seismol & Volcanol Dept, Chiyoda Ku, 1-3-4 Otemachi, Tokyo 1008122, Japan
[3] Japan Meteorol Agcy, Osaka Reg Headquarter, Chuo Ku, 4-1-76 Otemae, Osaka 5400008, Japan
[4] Minist Educ Culture Sports Sci & Technol, Res & Dev Bur, Chiyoda Ku, 3-2-2 Kasumigaseki, Tokyo 1008959, Japan
关键词
REAL-TIME; GROUND-MOTION; SOUTHERN CALIFORNIA; TOHOKU EARTHQUAKE; BAYESIAN-APPROACH; SOURCE MODEL; SYSTEM; ALGORITHM; GENERATION; MAGNITUDE;
D O I
10.1785/0120170085
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
A basic methodology for earthquake early warning is the use of point-source models fed with observational data from triggered stations. The 2011 Off the Pacific Coast of Tohoku earthquake in Japan (M-w 9.0) (the Tohoku-Oki earthquake) and its aftershock and induced earthquake activity, however, highlighted the following technical challenges of point-source models: (1) underprediction of the strong motion of large earthquakes with finite faults, (2) missing earthquakes during intense seismic activities, and (3) overprediction of the strong motion of multiple simultaneous earthquakes. We propose the propagation of local undamped motion (PLUM) method to address these technical challenges. The PLUM method is a simple wavefield-estimation approach that predicts seismic intensities directly from observed real-time seismic intensities near target sites. The PLUM method can outperform point-source-model approaches in terms of (a) accurate ground-motion prediction for large earthquakes with finite faults and (b) robust event declaration for complex earthquake sequences. On the other hand, available warning times provided by the PLUM method are not expected to be very long. We also introduce a hybrid method that uses both the PLUM method and a point-source-model approach to maximize the total available warning times and avoid missing strong motion. When applied to the Tohoku-Oki earthquake (M-w 9.0), the PLUM and hybrid methods predicted accurate strong motion without underestimation and provided sufficient warning times in most areas. For the subsequent earthquake sequence after the M-w 9.0 earthquake, the PLUM method robustly detected and processed large earthquakes despite considerable intense seismicity. A statistical analysis using large aftershocks and induced earthquakes demonstrated that the PLUM and hybrid methods predicted strong motion more accurately than the point-source-model approach of the Japan Meteorological Agency. These findings indicate that the PLUM and hybrid methods can be effective countermeasures to address the technical challenges faced by point-source models. Electronic Supplement: A detailed description of the event-construction (EC) process in the propagation of local undamped motion (PLUM) method with related figures, figures of available warning times for the Tohoku-Oki earthquake (Mw 9.0) when the threshold of the observed real-time seismic intensity was changed to 4 on IJMA (JMA, Japan Meteorological Agency), available warning times for the largest aftershock (M 7.6) of the Tohoku-Oki earthquake at 15: 15: 34 in application 2, and available warning times for events 2, 7, 19, 21, and 26 in application 3.
引用
收藏
页码:983 / 1003
页数:21
相关论文
共 55 条
[1]  
Aketagawa T., 2010, Q J SEISMOL, V73, P123
[2]   Application of real-time GPS to earthquake early warning [J].
Allen, Richard M. ;
Ziv, Alon .
GEOPHYSICAL RESEARCH LETTERS, 2011, 38
[3]   The potential for earthquake early warning in southern California [J].
Allen, RM ;
Kanamori, H .
SCIENCE, 2003, 300 (5620) :786-789
[4]  
ALLEN RV, 1978, B SEISMOL SOC AM, V68, P1521
[5]  
[Anonymous], 2008, Eos Trans. AGU, DOI DOI 10.1029/2008EO080001
[6]  
[Anonymous], 2001, Seismology
[7]  
[Anonymous], 2009, Introduction to seismology
[8]   Source model for strong ground motion generation in the frequency range 0.1-10 Hz during the 2011 Tohoku earthquake [J].
Asano, Kimiyuki ;
Iwata, Tomotaka .
EARTH PLANETS AND SPACE, 2012, 64 (12) :1111-1123
[9]   PreSEIS:: A neural network-based approach to earthquake early warning, for finite faults [J].
Boese, Maren ;
Wenzel, Friedemann ;
Erdik, Mustafa .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2008, 98 (01) :366-382
[10]   Real-time Finite Fault Rupture Detector (FinDer) for large earthquakes [J].
Boese, Maren ;
Heaton, Thomas H. ;
Hauksson, Egill .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2012, 191 (02) :803-812