Simulasi Surge Tsunami Dengan Metode Dam Break Menggunakan Reservoar Terbatas
DOI:
https://doi.org/10.5614/jts.2024.31.2.5Keywords:
Simulation, tsunami surge, dam break, limited reservoirAbstract
Abstract
The dam break method for simulating tsunami surges in the laboratory typically uses a sufficiently long flume, so that the upstream section of the flume, which serves as the reservoir, is also quite long. Using a long reservoir can provide a more extended simulation time for tsunami surge propagation on land, allowing the characteristics of the tsunami surge to be well observed. With a shorter flume, the reservoir space is also limited in length, and the simulation time for tsunami surge propagation is likewise constrained. This study aims to describe the characteristics of the simulated tsunami surge in comparison to the Chanson solution using a limited (short) reservoir. The tsunami surge simulation in a dry channel was conducted under the assumption of a limited reservoir with no bed slope. The water height in the reservoir varied from (d0) = 100 mm, 200 mm, 300 mm, and 400 mm, and the simulation was performed three times for each reservoir height. The tsunami surge simulation with downstream inundation was conducted similarly, but with an initial downstream inundation height of d1 = 100 mm and 150 mm, without initial velocity. The analysis results showed that the height and velocity of the tsunami surge from the simulation for both dry and inundated channels approached the results from Chanson's solution. This indicates that a limited flume length can be used to simulate tsunami surges with the dam break method, and that simulations with initial inundation can simulate the waveforms of undular bore and fully developed bore.
References
Bangguna, D. S. V. L., Triatmadja, R., & Yuwono, N. (2016). Simulation of Tsunami Attack on Seawall Caisson. Poceeding of 20th Congress of IAHR-APD 2016, Colombo, Sri Lanka, 1?6.
Briggs, M. J., Synolakis, C. E., Harkins, G. S., & Hughes, S. T. (1995). Large Scale Three-Dimensional Laboratory Measurements of Tsunami Inundation. Tsunamis: Progress in Prediction, Disaster Prevention and Warning., May 2014, 129?149. https://doi.org/10.1007/978-94-015-8565-1_9
Chanson, H. (2005). Application of the Saint-Venant Equations and Method of Characteristics to the Dam Break Wave Problem (Issue June).
Chanson, H. (2006). Tsunami Surges on Dry Coastal Plains: Application of Dam Break Wave Equations. Coastal Engineering Journal, 48(4), 355?370. https://doi.org/10.1142/S0578563406001477
Kuswandi, Radianta Triatmadja, I. (2016). Velocity Around a Cylinder Plie During Scouring Process Due to Tsunami. Poceeding of 20th Congress of IAHR-APD 2016, Colombo, Sri Lanka, 1?14.
Philip L.-F. Liu, Yong-Sik Cho, Michael J. Briggs, Utku Kanog Lu, C. E. S. (1995). Runup of Solitary Waves on A Circular Island. Journal of Fluid Mechanics, 302, 259?285.
R. Triatmadja, B. (2014). Simulation of Tsunami Force on Rows of Buildings in Aceh Region After Tsunami Disaster in 2004. The International Journal Og the Tsunami Society, 33(3), 156?169.
Raichlen, F. (1970). Tsunamis Some Laboratory and Field Observations. Coastal Engineering, 2103?2122.
Synolakis, C. E., & Raichlen, F. (2007). The Runup of Long Waves (Issue January 1986).
Tiziana Rosetto, William Allsop, Ingrid Charvet, D. I. R. (2016). Physical modelling of tsunami using a new pneumatic wave generator. Coastal Engineering, 6(August), 128.
Warniyati, Radianta Triatmadja, Nur Yuwono, Bangguna, D. (2018). Design of a Facility for Tsunami run up Generation on Study Tsunami and Seawall Interaction. Journal of the Civil Engineering Forum, 4(3), 201. https://doi.org/10.22146/jcef.36857
Yeh, H. (1991). Tsunami Bore Runup. Natural Hazards, 4(2?3), 209?220. https://doi.org/10.1007/BF00162788
Yeh, H., Ghazali, A., & Marton, I. (1989). Experimental Study of Bore Run-up. Journal of Fluid Mechanics, 206, 563?578. https://doi.org/10.1017/S0022112089002417