ANALISIS ARTIFICIAL NEURAL NETWORK DALAM PENENTUAN ARRIVAL TIME GELOMBANG P DAN S

Earthquake Earthquake Early Warning (EEW) is a system for sending early warning of earthquake events, with the stages of detecting and determining the location of earthquakes. The selection of the arrival time of the P waves and S waves is the parameter used to determine the location of an earthq...

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Main Author: Ilyasa Rachmanditya, Bima
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/76745
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:76745
spelling id-itb.:767452023-08-18T09:57:36ZANALISIS ARTIFICIAL NEURAL NETWORK DALAM PENENTUAN ARRIVAL TIME GELOMBANG P DAN S Ilyasa Rachmanditya, Bima Indonesia Final Project DNN; gempa bumi; artificial intelligence; NonLinLoc; PhaseNet, GaMMA; Deep Learning INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/76745 Earthquake Earthquake Early Warning (EEW) is a system for sending early warning of earthquake events, with the stages of detecting and determining the location of earthquakes. The selection of the arrival time of the P waves and S waves is the parameter used to determine the location of an earthquake. For this reason, the time required to determine the arrival time of P waves and S waves has an important role in EEW. Generally, determining the location of earthquakes is done manually, with artificial intelligence being one of the methods for determining the arrival time of an earthquake automatically. Deep learning is part of artificial intelligence that can process data quickly, has high scalability, and has a high level of accuracy. PhaseNet is a deep neural network (DNN) program, which is a further classification of deep learning with the aim of determining the arrival time of P waves and S waves. In this study, the authors used waveform data from 89 BMKG stations located on the island of Java, Indonesia during the recording time range from April 2020 to September 2020. The duration of the waveform used was five minutes and then PhaseNet was applied to obtain the arrival times of the P waves and S waves. The results of determining the arrival time of the P wave and S wave were compared with the GaMMA program to obtain a consistent distribution pattern of the wave phase selection results. Earthquake locations were determined using the NonLinLoc program. The arrival time results based on PhaseNet obtained 312 out of 333 arrival times of P waves and S waves, these results have a difference of less than one second. The results of determining the location with PhaseNet data have a difference with BMKG with an average longitude of -0.0071o, latitude of 0.39369o and depth of 3.17981 km. text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description Earthquake Earthquake Early Warning (EEW) is a system for sending early warning of earthquake events, with the stages of detecting and determining the location of earthquakes. The selection of the arrival time of the P waves and S waves is the parameter used to determine the location of an earthquake. For this reason, the time required to determine the arrival time of P waves and S waves has an important role in EEW. Generally, determining the location of earthquakes is done manually, with artificial intelligence being one of the methods for determining the arrival time of an earthquake automatically. Deep learning is part of artificial intelligence that can process data quickly, has high scalability, and has a high level of accuracy. PhaseNet is a deep neural network (DNN) program, which is a further classification of deep learning with the aim of determining the arrival time of P waves and S waves. In this study, the authors used waveform data from 89 BMKG stations located on the island of Java, Indonesia during the recording time range from April 2020 to September 2020. The duration of the waveform used was five minutes and then PhaseNet was applied to obtain the arrival times of the P waves and S waves. The results of determining the arrival time of the P wave and S wave were compared with the GaMMA program to obtain a consistent distribution pattern of the wave phase selection results. Earthquake locations were determined using the NonLinLoc program. The arrival time results based on PhaseNet obtained 312 out of 333 arrival times of P waves and S waves, these results have a difference of less than one second. The results of determining the location with PhaseNet data have a difference with BMKG with an average longitude of -0.0071o, latitude of 0.39369o and depth of 3.17981 km.
format Final Project
author Ilyasa Rachmanditya, Bima
spellingShingle Ilyasa Rachmanditya, Bima
ANALISIS ARTIFICIAL NEURAL NETWORK DALAM PENENTUAN ARRIVAL TIME GELOMBANG P DAN S
author_facet Ilyasa Rachmanditya, Bima
author_sort Ilyasa Rachmanditya, Bima
title ANALISIS ARTIFICIAL NEURAL NETWORK DALAM PENENTUAN ARRIVAL TIME GELOMBANG P DAN S
title_short ANALISIS ARTIFICIAL NEURAL NETWORK DALAM PENENTUAN ARRIVAL TIME GELOMBANG P DAN S
title_full ANALISIS ARTIFICIAL NEURAL NETWORK DALAM PENENTUAN ARRIVAL TIME GELOMBANG P DAN S
title_fullStr ANALISIS ARTIFICIAL NEURAL NETWORK DALAM PENENTUAN ARRIVAL TIME GELOMBANG P DAN S
title_full_unstemmed ANALISIS ARTIFICIAL NEURAL NETWORK DALAM PENENTUAN ARRIVAL TIME GELOMBANG P DAN S
title_sort analisis artificial neural network dalam penentuan arrival time gelombang p dan s
url https://digilib.itb.ac.id/gdl/view/76745
_version_ 1822995039931858944