Skip to main content
Log in

Modeling of inundation dynamics on Banda Aceh, Indonesia during the great Sumatra tsunamis December 26, 2004

  • Original Paper
  • Published:
Natural Hazards Aims and scope Submit manuscript

Abstract

The tsunami inundation flows on Banda Aceh, Indonesia reached 5 km inland during the December 26, 2004, event and devastated most of the houses, buildings, and infrastructure along the coast and killed more than 167,000 people. The overland flows from the northwest coast and the west coast collided at Lampisang village approximately 3.7 km from Ulee Lheue (northwest coast) and 6.8 km from Lhok Nga (west coast) as reported by survivors. Inundation modeling based on the nonlinear shallow-water wave equations reproduces the inundation pattern and demonstrates a colliding of the overland flows. The model suggests that wave characteristics on the northwest coast of Banda Aceh were different from those on the waves that impacted upon the west coast. The areas, which experienced higher inundation levels, did not always experience greatest overland flow speeds, and the damage areas mostly coincide with the flow speed distribution rather than the runup and inundation depth.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11
Fig. 12
Fig. 13
Fig. 14
Fig. 15
Fig. 16
Fig. 17
Fig. 18
Fig. 19
Fig. 20
Fig. 21

Similar content being viewed by others

References

  • Aida I (1978) Reliability of a tsunami source model derived from fault parameters. J Phys Earth 26:57–73

    Article  Google Scholar 

  • Banerjee P, Pollitz F, Nagarajan B, Burgmann R (2007) Coseismic slip distribution of the 26 December 2004 Sumatra-Andaman and 28 March 2005 Nias Earthquake from GPS static offsets. Bull Seismol Soc Am 97(1A):S86–S102. doi:10.1785/01200506091

    Article  Google Scholar 

  • Black KP (1983) Sediment transport and tidal inlet hydraulics. PhD thesis, University of Waikato, New Zealand, p 331

  • Black KP (2001) The 3DD suite of numerical process models. ASR Ltd., PO Box 67, Raglan, p 90

  • Black KP, Barnett AG (1988) Sediment transport modelling under tidal flows with application in Natural Estuary, IAHR Symposium on mathematical modeling of sediment transport in the Coastal Zone, Copenhagen, p 9

  • Black KP, Gay SL (1987) Eddy formation in unsteady flows. J Geophys Res 92(C9):9514–9522

    Article  Google Scholar 

  • Black KP, Gay SL (1989) Reef-scale numerical hydrodynamic modelling developed to investigate crown-of-thorns starfish outbreaks. In: Bradbury R (ed) Acanthaster and the coral reef: a theoretical perspective. Lecture notes in Biomathematics, Springer, pp 120–150

    Google Scholar 

  • Black KP, Healy TR, Hunter M (1989) Sediment dynamics in the lower section of a mixed sand and shell–lagged tidal estuary. J Coast Res 5(3):503–521

    Google Scholar 

  • Borrero JC (2005) Field data and satellite imagery of tsunami effects in Banda Aceh. Science 308:1596

    Article  Google Scholar 

  • Borrero JC, Synolakis CE, Fritz H (2006) Northern Sumatra field survey after the December 2004 great Sumatra earthquake and Indian Ocean tsunami. Earthquake Spectra 22(3):93–104

    Article  Google Scholar 

  • Borrero JC, Bosserelle C, Prasetya G, Black KP (2007) Using 3DD to model tsunami inundation. In: Proceedings of the Australasian coast and port conference, July 2007. Melbourne, Paper 96, p 6

  • BRR (Reconstruction and Rehabilitation Agency of Aceh and Nias) (2006) Progress Report Aceh & Nias, two years after the tsunamis, December 2006, p 110

  • Fritz H, Borrero JC, Synolakis CE, Yoo J (2006) 2004 Indian Ocean tsunami flow velocity measurements from survivors videos. Geophy Res Lett 33:1–5

    Article  Google Scholar 

  • Fujii Y, Satake K (2007) Tsunami source of the 2004 Sumatra-Andaman earthquake inferred from tide gauge and satellite data. Bull Seismol Soc Am 97(1A):S192–S207. doi:10.1785/0120050613

    Article  Google Scholar 

  • Grilli ST, Loualalen M, Asavanant J, Shi F, Kirby J, Watts P (2007) Source constraints and model simulation of the December 26, 2004, Indian Ocean Tsunami. J Waterw, Port, Coast Ocean Eng 133:414–429. doi:10.1061/(ASCE)0733-950X(2007)133:6(414)

    Article  Google Scholar 

  • Jaffe BE, C. Borrero JC, Prasetya GS, Peters P, McAdoo B, Gelfenbaum G, Morton R, Ruggiero P, Higman B, Dengler L, Hidayat R, Kingsley E, Widjo Kongko, Lukijanto, Moore A, Titov V, Yulianto E (2006) The December 26, 2004 Indian Ocean tsunami in Northwest Sumatra and Offshore Islands. Earthquake Spectra 22(3):105–135

  • Liu PLF, Yeh H, Synolakis CE (2008) Benchmark problems in advance numerical models for simulating tsunami waves and runup. In: Liu PLF, Yeh H, Synolakis CE (eds) Advance in Coastal and Ocean Engineering, Vol 10. pp 223–230

  • Lundquist CJ, Thrush F, Oldman JW, Senior AK (2004) Limited transport and recolonization potential in shallow tidal estuaries. J Limnol Oceanogr 49(2):386–395

    Article  Google Scholar 

  • Matsutomi H, Sakakiyama T, Nugroho S, Matsuyama M (2006) Aspects of inundated flow due to the 2004 Indian Ocean tsunami. Coast Eng J 48(2):167–195

    Article  Google Scholar 

  • Okada Y (1985) Surface deformation due to shear and tensile faults in a half space. Bull Seismol Soc Am 5(4):1135–1154

    Google Scholar 

  • Paris R, Lavigne F, Wassmer P, Sartohadi J (2007) Coastal sedimentation associated with the December 26 2004 tsunami in Lhok Nga, west Banda Aceh (Sumatra, Indonesia). Mar Geol 238:97–106

    Article  Google Scholar 

  • Rhie J, Dreger D, Burgmann R, Romanowicz B (2007) Slip of the 2004 Sumatra-Andaman earthquake from joint inversion of long-period global seismic waveforms and GPS static offsets. Bull Seismol Soc Am 97(1A):S115–S127. doi:10.1785/0120050620

    Article  Google Scholar 

  • Shuterland J, Peet AH, Soulsby RL (2004) Evaluating the performance of morphological models. Coast Eng 51:917–939

    Article  Google Scholar 

  • Stein S, Okal EA (2005) Speed and size of the Sumatra earthquake. Nature 434(7033):581–582

    Article  Google Scholar 

  • Subarya C, Clieh M, Prawirodirdjo L, Avouac J, Bock Y, Sieh K, Meltzner A, Natawidjaja D, McCaffrey R (2006) Plate-boundary deformation associated with the great Sumatra-Andaman earthquake. Nature 440:46–51

    Article  Google Scholar 

  • Synolakis CE (1987) The runup of solitary waves. J Fluid Mech 185:523–545

    Article  Google Scholar 

  • Synolakis CE, Bernard E (2006) Tsunami science before and beyond Boxing Day 2004. Philos Trans R Soc Lond A 364:2231–2265

    Article  Google Scholar 

  • Synolakis CE, Kong L (2006) Runup measurements of the December 2004 Indian Ocean Tsunami. Earthquake Spectra 22(3):67–91

    Article  Google Scholar 

  • Synolakis CE, Okal EA (2005) 1992–2002: perspective on a decade of post tsunami surveys. Adv Nat Technol Hazards 23:1–30

    Article  Google Scholar 

  • Tadepalli S, Synolakis CE (1994) The runup of N-waves. Proc R Soc Lond A 445:99–112

    Article  Google Scholar 

  • Tadepalli S, Synolakis CE (1996) Model for the leading waves of tsunamis. Phys Rev Lett 77:2141–2144

    Article  Google Scholar 

  • Tanioka Y, Kasusose T, Kathiroli S, Nishimura Y, Iwasaki S, Satake K (2006) Rupture process of the 2004 great Sumatra-Andaman earthquake estimated from tsunami waveforms. Earth Planet Space 58:203–209

    Google Scholar 

  • Titov VV, Synolakis CE (1997) Extreme inundation flows during the Hokkaido-Nansei-Oki tsunami. Geophys Res Lett 24(11):1315–1318

    Article  Google Scholar 

  • Titov VV, Rabinovich AB, Mofjeld HO, Thomson RE, Gonzalez FI (2005) The global reach of the 24 December 2004 Sumatra tsunami. Science 309:2045

    Article  Google Scholar 

  • Umitsu M, Tanavud C, Patanakanog B (2007) Effects of landforms on tsunami flow in the plains of Banda Aceh, Indonesia, and Nam Khem, Thailand. Mar Geol 242:141–153

    Article  Google Scholar 

  • Valee M (2007) Rupture properties of the giant Sumatra earthquake imaged by empirical Green’s function analysis. Bull Seismol Soc Am 97(1A):S103–S114. doi:10.1785/0120050616

    Article  Google Scholar 

  • Yalciner AC, Perincek D, Ersoy S, Prasetya G, Hidayat R, McAdoo BG (2005) Report on December 26, 2004, Indian Ocean Tsunami, Field Survey on Jan 21–31 at North of Sumatra, ITST of UNESCO IOC, p 18

Download references

Acknowledgments

The authors wish to thank anonymous reviewer for a critical review and valuable inputs and comments that improved the manuscript considerably. The numerical model research work had been funded through NZIDRS, New Zealand and the fieldwork funded partly by Tsunami Research Foundation––Indonesia, USGS––NOAA on ITST 1–2. Thanks to Drs. Rahman Hidayat, Dinar C Istiyanto, Widjo Kongko, Lukianto and all ITST Sumatra 2004 team for providing the fieldwork data.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Gegar Prasetya.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Prasetya, G., Borrero, J., de Lange, W. et al. Modeling of inundation dynamics on Banda Aceh, Indonesia during the great Sumatra tsunamis December 26, 2004. Nat Hazards 58, 1029–1055 (2011). https://doi.org/10.1007/s11069-010-9710-7

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11069-010-9710-7

Keywords

Navigation