2017
DOI: 10.35799/jm.6.1.2017.16176
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Simulasi Penjalaran Gelombang Tsunami di Sofifi– Tidore Kepulauan Maluku Utara sebagai Upaya Mitigasi Bencana

Abstract: Telah dilakukan simulasi penjalaran gelombang tsunami di Sofifi – Tidore Kepulauan Maluku Utara untuk mengetahui waktu tiba dan tinggi gelombang tsunami yang menerjang pantai apabila gempa yang diikuti tsunami kembali terjadi. Simulasi menggunakan perangkat lunak WinITDB dengan memasukkan koordinat sumber tsunami, koordinat daerah yang akan diterjang tsunami, panjang patahan, lebar patahan dan deformasi dasar laut dari data gempa yang pernah menimbulkan tsunami. Hasil simulasi menunjukkan bahwa daerah Sofifi t… Show more

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Cited by 4 publications
(3 citation statements)
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“…Tsunamis generally occur after a large earthquake on the oceanic plate with a strength above 7 on the Richter Scale. Tsunami waves are able to ravage land areas because of its speed reaching 500 km/hour while reached the land [16]. To minimize the impact of the disaster, it is necessary to increase the buffer zone in coastal areas and settlements to responsive the tsunami hazard.…”
Section: Methodsmentioning
confidence: 99%
“…Tsunamis generally occur after a large earthquake on the oceanic plate with a strength above 7 on the Richter Scale. Tsunami waves are able to ravage land areas because of its speed reaching 500 km/hour while reached the land [16]. To minimize the impact of the disaster, it is necessary to increase the buffer zone in coastal areas and settlements to responsive the tsunami hazard.…”
Section: Methodsmentioning
confidence: 99%
“…Large magnitudes have large deformation areas. One way to calculate the area is using the Well and Coppersmith equation (1994) [5] After the tsunami height is defined, the wave simulation of the tsunami is generated with the Gaussian hump equation [6] and then it is solved by the Shallow Water equation and Partial Differential Equation [7] that can be seen in (2.a) and (2.b) as the general equations. Gaussian hump is effective to make the distribution data of the parameter with mean and standard deviation factor and the Partial Differential Equation will simulate the tsunami in a couple times as the Shallow Water method as the simple one [11].…”
Section: Methodsmentioning
confidence: 99%
“…Areas right by the sea will bear the brunt of a tsunami, making communities near the coast more susceptible than those further inland. Tsunami waves, capable of reaching speeds up to 500 km/h, can severely damage structures and even push ships from the Meuraxa District port inland, as seen with the National Electricity Company's (PLN) generator ship during the last disaster [23].…”
Section: Study Of Areamentioning
confidence: 99%