scholarly journals SUMBER TSUNAMI GEMPA BUMI IQUIQUE, CHILI 2014 MENGGUNAKAN METODE BACK PROPAGATION TSUNAMI TRAVEL TIME (TTT)

2016 ◽  
Vol 17 (1) ◽  
Author(s):  
Dwi Hartanto
2018 ◽  
Vol 229 ◽  
pp. 04007
Author(s):  
Eko Pradjoko ◽  
Lukita Wardani ◽  
Hartana ◽  
Heri Sulistiyono ◽  
Syamsidik

The past earthquake records in North Lombok show the high level of earthquake hazard in this area. The maximum magnitude of the earthquake was 6.4 Mw on May 30th, 1979. But, there were no tsunami events records due to those earthquakes. Nevertheless, this area is very close to Mataram City (province capital city) and tourism area. Therefore, the assessment of tsunami hazard is very important. The tsunami simulation was conducted by using COMCOT Model, which is based on the North Lombok Earthquake as the initial condition. The simulation result shows the prediction of tsunami travel time is about 18 ~ 20 minutes from the source location to Mataram City. The height of the tsunami wave is 0.13 ~ 0.20 meters due to the earthquake magnitude is about 6 Mw.


2013 ◽  
Vol 13 (11) ◽  
pp. 2863-2870 ◽  
Author(s):  
I. V. Fine ◽  
R. E. Thomson

Abstract. We present a highly accurate and computationally efficient method (herein, the "wavefront orientation method") for determining the travel time of oceanic tsunamis. Based on Huygens' Principle, the method uses an eight-point grid-point pattern and the most recent information on the orientation of the advancing wavefront to determine the time for a tsunami to travel to a specific oceanic location. The method is shown to provide improved accuracy and reduced anisotropy compared with the conventional multiple grid-point method presently in widespread use.


1987 ◽  
Vol 11 (2-3) ◽  
pp. 89-102 ◽  
Author(s):  
T. S. Murty ◽  
N. K. Saxena ◽  
Peter W. Sloss ◽  
Patricia A. Lockridge

2014 ◽  
Vol 38 ◽  
pp. 1-8 ◽  
Author(s):  
M. Péroche ◽  
F. Leone ◽  
R. Gutton

Abstract. The risk of tsunami threatens the whole Caribbean coastline especially the Lesser Antilles. The first available models of tsunami propagation estimate that the travel time from the closest seismic sources would only take few minutes to impact the Martinique Island. Considering this threat, the most effective measure is a planned and organized evacuation of the coastal population. This requires an efficient regional warning system, estimation of the maximum expected tsunami flood height, preparation of the population to evacuate, and drawing up of local and regional emergency plans. In order to produce an efficient evacuation plan, we have to assess the number of people at risk, the potential evacuation routes, the safe areas and the available time to evacuate. However, this essential information is still lacking in the French West Indies emergency plans. This paper proposes a model of tsunami evacuation sites accessibility for Martinique directly addressed to decision makers. It is based on a population database at a local scale, the development of connected graphs of roads, the identification of potential safe areas and the velocity setting for pedestrians. Evacuation routes are calculated using the Dijkstra's algorithm which gives the shortest path between areas at risk and designated evacuation sites. The first results allow us to map the theoretical times and routes to keep the exposed population safe and to compare these results with a tsunami travel time scenario.


2019 ◽  
Vol 32 (14) ◽  
pp. 10435-10449 ◽  
Author(s):  
Chao Chen ◽  
Hui Wang ◽  
Fang Yuan ◽  
Huizhong Jia ◽  
Baozhen Yao

2006 ◽  
pp. 273-291 ◽  
Author(s):  
T Murty ◽  
A Rao ◽  
A Chaudhuri ◽  
A Gangopadhyay ◽  
S Dube ◽  
...  

2006 ◽  
Vol 29 (3) ◽  
pp. 179-199 ◽  
Author(s):  
N. Nirupama ◽  
I. Nistor ◽  
K. Ponnambalam ◽  
T. S. Murty

2018 ◽  
Author(s):  
Martin Wronna ◽  
Maria Ana Baptista ◽  
Jorge Miguel Miranda

Abstract. The tsunami catalogues of the Atlantic include two transatlantic tsunamis in the 18th century the extensively studied 1st November 1755, and 31st March 1761. The latest event struck Portugal, Spain, and Morocco around noontime. Several sources report a tsunami following the earthquake as far as Cornwall (United Kingdom), Cork (Ireland) and Barbados (Caribbean). An earlier analysis of macroseismic information and its compatibility with tsunami travel time information located the epicentre circa 34.5° N 13° W close to the Ampere Seamount at the eastern end of the Gloria Fault (North East Atlantic). The estimated magnitude of the earthquake is 8.5. In this study, we propose a tectonic source for the 31st March 1761 earthquake compatible with the tsunami observations in the Atlantic. We revisit the tsunami observations, reevaluate tsunami travel time data, and include a report from Cadiz not used before. The global plate kinematic model NUVEL 1A computes a convergence rate of 3.8 mm/y in the area of the presumed epicentre. We propose a source mechanism for the parent earthquake compatible with the geodynamic constraints in the region capable of reproducing most of the tsunami observations. The results of our study support the hypothesis that the 1761 event took place in the area of Coral Patch and Ampere seamounts, SW of the 1st November 1755, mega-earthquake source. Finally, this study shows the need to include the 1761 event in all seismic and tsunami hazard assessments in the Atlantic Ocean.


2006 ◽  
Vol 33 (16) ◽  
Author(s):  
Rahul Barman ◽  
B. Prasad Kumar ◽  
P. C. Pandey ◽  
S. K. Dube

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