Numerical Simulation of Morphological Changes due to the 2004 Tsunami Wave around Banda Aceh, Indonesia

The 2004 Indian Ocean tsunami caused massive morphological changes around the coast of Sumatra, Indonesia. This research investigates the coastal morphological changes in the Banda Aceh area via coupling a hydrodynamic model with a sediment transport module. The Cornell Multigrid Coupled Tsunami Mod...

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Main Authors: Teuku Muhammad Rasyif, Shigeru Kato, Syamsidik, Takumi Okabe
Format: Article
Language:English
Published: MDPI AG 2019-03-01
Series:Geosciences
Subjects:
Online Access:http://www.mdpi.com/2076-3263/9/3/125
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spelling doaj-c02ec8c2298149998986f454803461ef2020-11-24T21:20:55ZengMDPI AGGeosciences2076-32632019-03-019312510.3390/geosciences9030125geosciences9030125Numerical Simulation of Morphological Changes due to the 2004 Tsunami Wave around Banda Aceh, IndonesiaTeuku Muhammad Rasyif0Shigeru Kato1Syamsidik2Takumi Okabe3Department of Architecture and Civil Engineering, Toyohashi University of Technology, 1-1 Tempaku Cho, Toyohashi, Aichi 441-8580, JapanDepartment of Architecture and Civil Engineering, Toyohashi University of Technology, 1-1 Tempaku Cho, Toyohashi, Aichi 441-8580, JapanTsunami and Disaster Mitigation Research Center (TDMRC), Universitas Syiah Kuala, Jl. Prof. Dr. Ibrahim Hasan, Gp. Pie, Banda Aceh 23233, IndonesiaDepartment of Architecture and Civil Engineering, Toyohashi University of Technology, 1-1 Tempaku Cho, Toyohashi, Aichi 441-8580, JapanThe 2004 Indian Ocean tsunami caused massive morphological changes around the coast of Sumatra, Indonesia. This research investigates the coastal morphological changes in the Banda Aceh area via coupling a hydrodynamic model with a sediment transport module. The Cornell Multigrid Coupled Tsunami Model (COMCOT) was coupled with the XBeach Model to simultaneously simulate sediment transport and the hydrodynamic process during the tsunami. The coupled model is known as COMCOT-SED. Field bathymetric data measured in 2006 were used to validate the coupled model. This study reveals that the tsunami’s impact was more severe on the eastern part of the coast, where it hit directly. Meanwhile, the western part of the coast suffered a lower impact because of the sheltering effects from a series of small islands and a headland to the north. This study has shown that the model results from COMCOT-SED are consistent with field data and show where the tsunami waves caused offshore erosion.http://www.mdpi.com/2076-3263/9/3/125COMCOT-SEDtsunamicoastal erosionsediment transport
collection DOAJ
language English
format Article
sources DOAJ
author Teuku Muhammad Rasyif
Shigeru Kato
Syamsidik
Takumi Okabe
spellingShingle Teuku Muhammad Rasyif
Shigeru Kato
Syamsidik
Takumi Okabe
Numerical Simulation of Morphological Changes due to the 2004 Tsunami Wave around Banda Aceh, Indonesia
Geosciences
COMCOT-SED
tsunami
coastal erosion
sediment transport
author_facet Teuku Muhammad Rasyif
Shigeru Kato
Syamsidik
Takumi Okabe
author_sort Teuku Muhammad Rasyif
title Numerical Simulation of Morphological Changes due to the 2004 Tsunami Wave around Banda Aceh, Indonesia
title_short Numerical Simulation of Morphological Changes due to the 2004 Tsunami Wave around Banda Aceh, Indonesia
title_full Numerical Simulation of Morphological Changes due to the 2004 Tsunami Wave around Banda Aceh, Indonesia
title_fullStr Numerical Simulation of Morphological Changes due to the 2004 Tsunami Wave around Banda Aceh, Indonesia
title_full_unstemmed Numerical Simulation of Morphological Changes due to the 2004 Tsunami Wave around Banda Aceh, Indonesia
title_sort numerical simulation of morphological changes due to the 2004 tsunami wave around banda aceh, indonesia
publisher MDPI AG
series Geosciences
issn 2076-3263
publishDate 2019-03-01
description The 2004 Indian Ocean tsunami caused massive morphological changes around the coast of Sumatra, Indonesia. This research investigates the coastal morphological changes in the Banda Aceh area via coupling a hydrodynamic model with a sediment transport module. The Cornell Multigrid Coupled Tsunami Model (COMCOT) was coupled with the XBeach Model to simultaneously simulate sediment transport and the hydrodynamic process during the tsunami. The coupled model is known as COMCOT-SED. Field bathymetric data measured in 2006 were used to validate the coupled model. This study reveals that the tsunami’s impact was more severe on the eastern part of the coast, where it hit directly. Meanwhile, the western part of the coast suffered a lower impact because of the sheltering effects from a series of small islands and a headland to the north. This study has shown that the model results from COMCOT-SED are consistent with field data and show where the tsunami waves caused offshore erosion.
topic COMCOT-SED
tsunami
coastal erosion
sediment transport
url http://www.mdpi.com/2076-3263/9/3/125
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