Towards Automated Real-Time Detection and Location of Large-Scale Landslides through Seismic Waveform Back Projection

Rainfall-triggered landslides are one of the most deadly natural hazards in many regions. Seismic recordings have been used to examine source mechanisms and to develop monitoring systems of landslides. We present a semiautomatic algorithm for detecting and locating landslide events using both broadb...

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Main Authors: En-Jui Lee, Wu-Yu Liao, Guan-Wei Lin, Po Chen, Dawei Mu, Ching-Weei Lin
Format: Article
Language:English
Published: Wiley 2019-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2019/1426019
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author En-Jui Lee
Wu-Yu Liao
Guan-Wei Lin
Po Chen
Dawei Mu
Ching-Weei Lin
author_facet En-Jui Lee
Wu-Yu Liao
Guan-Wei Lin
Po Chen
Dawei Mu
Ching-Weei Lin
author_sort En-Jui Lee
collection DOAJ
description Rainfall-triggered landslides are one of the most deadly natural hazards in many regions. Seismic recordings have been used to examine source mechanisms and to develop monitoring systems of landslides. We present a semiautomatic algorithm for detecting and locating landslide events using both broadband and short-period recordings and have successfully applied our system to landslides in Taiwan. Compared to local earthquake recordings, the recordings of landslides usually show longer durations and lack distinctive P and S wave arrivals; therefore, the back projection method is adopted for the landslide detection and location. To identify the potential landslide events, the seismic recordings are band-passed from 1 to 3 Hz and the spectrum pattern in the time-frequency domain is used to distinguish landslides from other types of seismic sources based upon carefully selected empirical criteria. Satellite images before and after the detected and located landslide events are used for final confirmation. Our landslide detection and spatial-temporal location system could potentially benefit the establishment of rainfall-triggered landslide forecast models and provide more reliable constraints for physics-based landslide modeling. The accumulating seismic recordings of landslide events could be used as a training dataset for machine learning techniques, which will allow us to fully automate our system in the near future.
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issn 1468-8115
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publishDate 2019-01-01
publisher Wiley
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series Geofluids
spelling doaj-art-9993a2a97a2a4f4da3d75b975227e7582025-08-20T02:18:24ZengWileyGeofluids1468-81151468-81232019-01-01201910.1155/2019/14260191426019Towards Automated Real-Time Detection and Location of Large-Scale Landslides through Seismic Waveform Back ProjectionEn-Jui Lee0Wu-Yu Liao1Guan-Wei Lin2Po Chen3Dawei Mu4Ching-Weei Lin5Department of Earth Sciences, National Cheng-Kung University, No. 1, University Rd., East Dist., Tainan City 70101, TaiwanDepartment of Earth Sciences, National Cheng-Kung University, No. 1, University Rd., East Dist., Tainan City 70101, TaiwanDepartment of Earth Sciences, National Cheng-Kung University, No. 1, University Rd., East Dist., Tainan City 70101, TaiwanDepartment of Geology and Geophysics, University of Wyoming, Dept. 3006, 1000 E University Ave, Laramie, WY 82071, USASan Diego Supercomputer Center, University of California, San Diego, 10100 Hopkins Drive, La Jolla, CA 92093, USADepartment of Earth Sciences, National Cheng-Kung University, No. 1, University Rd., East Dist., Tainan City 70101, TaiwanRainfall-triggered landslides are one of the most deadly natural hazards in many regions. Seismic recordings have been used to examine source mechanisms and to develop monitoring systems of landslides. We present a semiautomatic algorithm for detecting and locating landslide events using both broadband and short-period recordings and have successfully applied our system to landslides in Taiwan. Compared to local earthquake recordings, the recordings of landslides usually show longer durations and lack distinctive P and S wave arrivals; therefore, the back projection method is adopted for the landslide detection and location. To identify the potential landslide events, the seismic recordings are band-passed from 1 to 3 Hz and the spectrum pattern in the time-frequency domain is used to distinguish landslides from other types of seismic sources based upon carefully selected empirical criteria. Satellite images before and after the detected and located landslide events are used for final confirmation. Our landslide detection and spatial-temporal location system could potentially benefit the establishment of rainfall-triggered landslide forecast models and provide more reliable constraints for physics-based landslide modeling. The accumulating seismic recordings of landslide events could be used as a training dataset for machine learning techniques, which will allow us to fully automate our system in the near future.http://dx.doi.org/10.1155/2019/1426019
spellingShingle En-Jui Lee
Wu-Yu Liao
Guan-Wei Lin
Po Chen
Dawei Mu
Ching-Weei Lin
Towards Automated Real-Time Detection and Location of Large-Scale Landslides through Seismic Waveform Back Projection
Geofluids
title Towards Automated Real-Time Detection and Location of Large-Scale Landslides through Seismic Waveform Back Projection
title_full Towards Automated Real-Time Detection and Location of Large-Scale Landslides through Seismic Waveform Back Projection
title_fullStr Towards Automated Real-Time Detection and Location of Large-Scale Landslides through Seismic Waveform Back Projection
title_full_unstemmed Towards Automated Real-Time Detection and Location of Large-Scale Landslides through Seismic Waveform Back Projection
title_short Towards Automated Real-Time Detection and Location of Large-Scale Landslides through Seismic Waveform Back Projection
title_sort towards automated real time detection and location of large scale landslides through seismic waveform back projection
url http://dx.doi.org/10.1155/2019/1426019
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