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巻号74
XYtracker ...

XYtracker : a new approach to estimate fault rupture extent in real time for large earthquakes

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XYtracker : a new approach to estimate fault rupture extent in real time for large earthquakes

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info:ndljp/pid/12685364
資料種別
記事
著者
Ying Xiaoほか
出版者
The Society of Geomagnetism and Earth, Planetary and Space Sciences
出版年
2022-05-26
資料形態
デジタル
掲載誌名
EPS : Earth, Planets and Space 74(77)
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要約等:

We present a methodology for estimating fault geometry and utilizing the distance to the fault for the shaking estimation to improve the accuracy of r...

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資料種別
記事
著者・編者
Ying Xiao
Masumi Yamada
出版年月日等
2022-05-26
出版年(W3CDTF)
2022-05-26
タイトル(掲載誌)
EPS : Earth, Planets and Space
巻号年月日等(掲載誌)
74(77)
掲載巻
74(77)
ISSN(掲載誌)
1880-5981
ISSN-L(掲載誌)
1343-8832
本文の言語コード
eng
国立国会図書館永続的識別子
info:ndljp/pid/12685364
コレクション(共通)
コレクション(障害者向け資料:レベル1)
コレクション(個別)
国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
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オンライン資料収集制度
受理日(W3CDTF)
2023-03-07T16:17:01+09:00
保存日(W3CDTF)
2023-03-07
記録形式(IMT)
application/pdf
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図書館・個人送信対象外
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掲載誌(国立国会図書館永続的識別子)
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デジタル

要約等
We present a methodology for estimating fault geometry and utilizing the distance to the fault for the shaking estimation to improve the accuracy of real-time shaking estimates for large earthquakes. Most of the earthquake early warning system currently estimates the seismic intensity with the ground-motion prediction equations (GMPE) as a function of the hypocenter distance. However, using the fault distance computed from a finite source model can improve the accuracy of the shaking intensity estimation for large earthquakes. This study proposes a novel methodology, XYtracker, to estimate the surface projection of the fault extent and real-time seismic intensity. For large earthquakes, high-frequency ground motions tend to saturate over the magnitude range and strongly correlate with fault distance. As a result, this work can achieve the fault extent using seismic intensity and GMPE. We considered three types of fault models: point-source, line-source, and rectangle-source model. We found the most probable model parameters for each model by minimizing the residual sum of squares between the observed and estimated seismic intensities. The Akaike Information Criterion selected the most probable model among them. The strong motion data set of the 2008 Wenchuan, 2011 Tohoku, and 2016 Kumamoto earthquakes was used to test our methodology. The new method for estimating the fault geometry can obtain the ongoing rupture length and direction using the strong motion data. The model selection scheme with the Akaike Information Criterion selected the finite-source model to explain the shaking distribution. Results revealed that this new approach performed well in estimating the fault dimension. The method can promote the accuracy of the seismic intensity estimation for future large earthquakes, including the subduction earthquakes.
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著作権情報
© The Author(s) 2022
This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder.
参照
Performance of the earthquake early warning system for the 2024 Noto Peninsula earthquake
参照
Source rupture processes of the foreshock and mainshock in the 2016 Kumamoto earthquake sequence estimated from the kinematic waveform inversion of strong motion data
Numerical Shake Prediction for Earthquake Early Warning: Data Assimilation, Real‐Time Shake Mapping, and Simulation of Wave Propagation
A new look at the statistical model identification
REAL-TIME SEISMOLOGY AND EARTHQUAKE DAMAGE MITIGATION
Fault Extent Estimation for Near-Real-Time Ground-Shaking Map Computation Purposes
Earthquake early warning: Concepts, methods and physical grounds
The Propagation of Local Undamped Motion (PLUM) Method: A Simple and Robust Seismic Wavefield Estimation Approach for Earthquake Early Warning
Estimating Rupture Dimensions of Three Major Earthquakes in Sichuan, China, for Early Warning and Rapid Loss Estimates
Progress on Development of an Earthquake Early Warning System Using Low-Cost Sensors
Real-Time Estimation of Fault Rupture Extent Using Envelopes of Acceleration
Real-time Finite Fault Rupture Detector (FinDer) for large earthquakes
Peak horizontal acceleration and velocity from strong-motion records including records from the 1979 imperial valley, California, earthquake
Real-Time Estimation of Fault Rupture Extent Using Near-Source versus Far-Source Classification
Regionally Adjustable Generic Ground‐Motion Prediction Equation Based on Equivalent Point‐Source Simulations: Application to Central and Eastern North America
The Status of Earthquake Early Warning around the World: An Introductory Overview
The Potential for Earthquake Early Warning in Southern California
FinDer v.2: Improved real-time ground-motion predictions for M2–M9 with seismic finite-source characterization
On the estimation of seismic intensity in earthquake early warning systems
A New Method of Quickly Estimating Epicentral Distance and Magnitude from a Single Seismic Record
Finite-Fault Rupture Detector (<i>FinDer</i>): Going Real-Time in Californian<i>ShakeAlert</i>Warning System
Earthquake Early Warning Starts Nationwide in Japan
Empirical Response Spectral Attenuation Relations for Shallow Crustal Earthquakes
Optimizing Earthquake Early Warning Performance: ElarmS‐3
震度のリアルタイム演算に用いられる近似フィルタの改良
Fault Length and Direction of Rupture Propagation for the 1993 Kushiro-Oki Earthquake as Derived from Strong Motion Duration.
NIED KiK-net
Focal mechanism and slip history of the 2011 Mw 9.1 off the Pacific coast of Tohoku Earthquake, constrained with teleseismic body and surface waves
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書誌ID(NDLBibID)
12685364