首页> 外文期刊>Bulletin of the Seismological Society of America >The Propagation of Local Undamped Motion (PLUM) Method: A Simple and Robust Seismic Wavefield Estimation Approach for Earthquake Early Warning
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The Propagation of Local Undamped Motion (PLUM) Method: A Simple and Robust Seismic Wavefield Estimation Approach for Earthquake Early Warning

机译:局部透明运动(PLUM)方法的传播:一种简单且坚固的地震波场估计地震预警

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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
机译:地震预警的基本方法是使用从触发站中馈出具有观测数据的点源模型。 2011年从日本的东北地震(MW 9.0)(Tohoku-oki地震)及其余震和诱发地震活动的2011年突出了下列情点源模型的技术挑战:(1)强大的欠款大地震的运动与有限断层,(2)在激烈的地震活动期间缺失地震,(3)对多同质地震的强烈运动的过度估计。我们提出了局部无拆除运动(PLUM)方法的传播来解决这些技术挑战。梅花方法是一种简单的波场估计方法,可直接从目标位点附近的观察到的实时地震强度预测地震强度。梅花方法可以在大地震的准确地面运动预测方面优于偏好点源模型方法,具有用于复杂地震序列的有限故障的大地震和(B)强大的事件声明。另一方面,梅花方法提供的可用警告时间不会很长。我们还介绍了一种混合方法,使用梅花方法和点源模型方法来最大化总可用警告时间,并避免缺少强烈的运动。当应用于Tohoku-OKI地震(M-W 9.0)时,李子和混合方法预测了准确的强烈运动,而不会低估,并且在大多数区域提供足够的警告时间。对于在M-W 9.0的地震后随后的地震序列,李子法稳健地检测到并加工大地震,尽管存在相当大的地震性。使用大余震和诱导地震的统计分析证明了梅和混合方法比日本气象学局的点源模型方法更准确地预测强运动。这些发现表明李子和

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    Japan Meteorol Agcy Meteorol Res Inst 1-1 Nagamine Tsukuba Ibaraki 3050052 Japan;

    Japan Meteorol Agcy Seismol &

    Volcanol Dept Chiyoda Ku 1-3-4 Otemachi Tokyo 1008122 Japan;

    Japan Meteorol Agcy Osaka Reg Headquarter Chuo Ku 4-1-76 Otemae Osaka 5400008 Japan;

    Japan Meteorol Agcy Meteorol Res Inst 1-1 Nagamine Tsukuba Ibaraki 3050052 Japan;

    Japan Meteorol Agcy Seismol &

    Volcanol Dept Chiyoda Ku 1-3-4 Otemachi Tokyo 1008122 Japan;

    Japan Meteorol Agcy Seismol &

    Volcanol Dept Chiyoda Ku 1-3-4 Otemachi Tokyo 1008122 Japan;

    Japan Meteorol Agcy Seismol &

    Volcanol Dept Chiyoda Ku 1-3-4 Otemachi Tokyo 1008122 Japan;

    Minist Educ Culture Sports Sci &

    Technol Res &

    Dev Bur Chiyoda Ku 3-2-2 Kasumigaseki Tokyo 1008959 Japan;

    Japan Meteorol Agcy Meteorol Res Inst 1-1 Nagamine Tsukuba Ibaraki 3050052 Japan;

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  • 正文语种 eng
  • 中图分类 地震学;
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