Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/97321
Title: Tsunami hazard from the subduction megathrust of the South China Sea : Part II. Hydrodynamic modeling and possible impact on Singapore
Authors: Huang, Zhenhua
Wu, Tso-Ren
Tan, Soon Keat
Megawati, Kusnowidjaja
Shaw, Felicia
Liu, Xiaozhen
Pan, Tso-Chien
Keywords: DRNTU::Science::Geology::Volcanoes and earthquakes
Issue Date: 2008
Source: Huang, Z., Wu, T. R., Tan, S. K., Megawati, K., Shaw, F., Liu, X., et al. (2009). Tsunami hazard from the subduction Megathrust of the South China Sea: Part II. Hydrodynamic modeling and possible impact on Singapore. Journal of Asian Earth Sciences, 36(1), 93-97.
Series/Report no.: Journal of Asian earth sciences
Abstract: USGS has identified certain section of the Manila (Luzon) trench as a high-risk earthquake zone. This zone is where the Eurasian plate is actively subducting eastward underneath the Luzon volcanic arc on the Philippine Sea plate. An earthquake of magnitude 9.0 could be generated based on the worst case scenario rupture of Manila Trench. In this paper, the possible impact of this worst case scenario rupture on Singapore is investigated using a numerical model. It is found that (1) it takes about 12 h for the tsunami waves generated at Manila Trench to arrive at Singapore coastal waters; (2) the wave period of the tsunami wave, i.e., time interval between two peaks, is about 5 h; (3) the maximum water level rise in Singapore water is about 0.8 m; and (4) the maximum velocity associated with the tsunami waves is about 0.5 m/s, which is not likely to have significant impact on the port operations in Singapore.
URI: https://hdl.handle.net/10356/97321
http://hdl.handle.net/10220/10525
ISSN: 1367-9120
DOI: http://dx.doi.org/10.1016/j.jseaes.2008.08.007
Rights: © 2008 Elsevier Ltd.
Fulltext Permission: none
Fulltext Availability: No Fulltext
Appears in Collections:CEE Journal Articles

Google ScholarTM

Check

Altmetric

Items in DR-NTU are protected by copyright, with all rights reserved, unless otherwise indicated.