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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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 |
work_keys_str_mv |
AT teukumuhammadrasyif numericalsimulationofmorphologicalchangesduetothe2004tsunamiwavearoundbandaacehindonesia AT shigerukato numericalsimulationofmorphologicalchangesduetothe2004tsunamiwavearoundbandaacehindonesia AT syamsidik numericalsimulationofmorphologicalchangesduetothe2004tsunamiwavearoundbandaacehindonesia AT takumiokabe numericalsimulationofmorphologicalchangesduetothe2004tsunamiwavearoundbandaacehindonesia |
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1726002211038691328 |