3D numerical simulation of tsunami generation and propagation, case study: Makran tsunami generation and penetrating in Chabahar Bay

Honarmand, Masih; Shanehsazzadeh, Ahmad; Zandi, Sayed Mahdi

doi:10.1016/j.oceaneng.2020.108109

Cited by 8 publications

(3 citation statements)

References 21 publications

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“…Earthquake events can be triggered by tectonic activity potential to cause a tsunami that can cause harm to people in the coastal areas of Krakal, Drini, Sepanjang, Ngrawe, and Kukup [30,31]. Tsunamis are generally triggered by earthquakes in subduction zones, seafloor landslides, seabed volcanic eruptions, and extraterrestrial forces [32]. Based on the geological setting of Indonesia, earthquakes in subduction zones and seafloor volcanic eruptions are the dominant triggers for tsunamis that occur in Indonesia [30].…”

Section: Tsunamimentioning

confidence: 99%

Identification of coastal typology: potential resources and hazards

Wibowo

Ronggowulan

Fatchurohman

et al. 2022

IOP Conf. Ser.: Earth Environ. Sci.

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Coastal areas are unique ecosystems because of the potential for abundant natural resources and hazards that can cause losses. Therefore, this study aims to identify the typology and coastal dynamics of Kukup, Ngrawe, Sepanjang, Drini, and Krakal, Indonesia, for analyzing the potential of natural resources and hazards. A rapid-integrated assessment was carried out to identify typology, genesis, and dynamics of coastal areas by conducting field surveys at locations that have been determined by purposive sampling. The results showed that wave erosion coast was formed in Ngrawe, Kukup, Drini, and Krakal. The marine deposition coast was formed in Ngrawe, Kukup, Sepanjang, Drini, and Krakal. Moreover, the coast built by organism can be found in Sepanjang, Drini, and Krakal. In contrast, the structurally shaped coast was formed in the western part of the Krakal. The coastal dynamics begin with geodynamic processes that form structurally shaped coast, hydrodynamics that form marine deposition coast, wave erosion coast, and ecodynamics that form coast built by organism typology. The potential of natural resources consists of fishery potential, agriculture, and natural beauty for tourism objects. In contrast, the potential hazards consist of earthquakes, tsunamis, tidal waves, rockfall, rip currents, topographic changes, and land-use changes. The coastal area management planning recommendations were Spatial Planning Regulation, Early Warning System, Evacuation Route and assembly point (shelter), Digital-based Information Dissemination, and building retrofitting.

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Section: Tsunamimentioning

confidence: 99%

Identification of coastal typology: potential resources and hazards

Wibowo

Ronggowulan

Fatchurohman

et al. 2022

IOP Conf. Ser.: Earth Environ. Sci.

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“…It handles the mesh generation, the case simulation and the reading and postprocessing of the outputs. Among others, it was used by Qin et al (2018b) to study the inundation and impact of a tsunami on a coastal city or by Honarmand et al (2020) to propagate the initial elevation generated by the Makran earthquake in 1945. Romano et al (2020) also developed an approach to simulate tsunamis generated by a solid landslide using the Overset mesh technique.…”

Section: Boussinesq Equationsmentioning

confidence: 99%

Landslide tsunamis: Comparison between depth-averaged and Navier–Stokes models

Paris

Heinrich

Abadie

2021

Coastal Engineering

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“…A tsunami is a natural disaster that is directly related to waves in the ocean. It is a natural disaster characterized by waves from the sea to the land with very high destructive power [1]. Rolling ocean waves occur because of a shift in the seabed, which causes seawater to move towards the mainland.…”

Section: Introductionmentioning

confidence: 99%

Implementation of comprehensive school safety: the risk reduction and resilience education pillar in State Senior High School 1 of Pacitan and Islamic State Senior High School 1 of Pacitan, Indonesia

Syahputri

Aris

Hafida

et al. 2022

IOP Conf. Ser.: Earth Environ. Sci.

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Pacitan is vulnerable to earthquakes and tsunamis because it is located near the subduction zone between the Indo-Australian and Eurasian plates. So that it needs Disaster Risk Reduction efforts, one of the best measures is to implement the three pillars of Comprehensive School Safety. This study aims to analyze the implementation of the third pillar of Comprehensive School Safety, namely the Pillar of Risk Reduction and Resilience Education. The study was conducted at State Senior High School 1 of Pacitan and Islamic State Senior High School 1 of Pacitan because they directly face the Indian Ocean. This study used a quantitative approach with primary data obtained from filling out questionnaires by respondents. Respondents in this study were principals, teachers, and students involved in Scouting and Junior Red Cross in these two schools. The instrument was a questionnaire including teacher and education staff training, integration of disaster education into the curriculum, and extracurricular activities indicators. The results indicated that teacher and education staff and curriculum integration were not optimally carried out in these two schools. Furthermore, they have not yet established disaster mitigation extracurricular, but implementing disaster mitigation education was carried out through Scouts and Junior Red Cross.

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3D numerical simulation of tsunami generation and propagation, case study: Makran tsunami generation and penetrating in Chabahar Bay

Cited by 8 publications

References 21 publications

Identification of coastal typology: potential resources and hazards

Identification of coastal typology: potential resources and hazards

Landslide tsunamis: Comparison between depth-averaged and Navier–Stokes models

Implementation of comprehensive school safety: the risk reduction and resilience education pillar in State Senior High School 1 of Pacitan and Islamic State Senior High School 1 of Pacitan, Indonesia

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