Dear Visitor.
Thank you very much for your
visit our site. We have renewed our simulation by comparing the tsunami
amplitudes along the coasts with the measurements taken by us other tsunami
survey teams. The results of our new simulations
will be available after
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Our field survey in |
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Our new simulation results will be ready
in the following link http://yalciner.ce.metu.edu.tr/sumatra/survey/simulation/index.htm |
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Best wishes and kind regards. Dr. Ahmet Cevdet Yalciner yalciner@metu.edu.tr
__________________
The following part of this page
has been prepared two weeks after Indian Ocean Tsunami in order to provide data
based on model studies for identification of level of tsunami inundation and
run up along Indian ocean coasts for the teams to go to sites for tsunami
survey and reconnaissance.
__________________
Our web site (dated on
We announce
our deep condolences to the people from all countries who suffered from the
devastating December 26, 2004 tsunami disaster directly and/or indirectly We
also dedicate all our knowledge/efforts/works and share all our results with
all scientists, officials, managers, decision makers and governors for the
better understanding of the this disaster and better development in
preparedness and mitigation for future events.
THE MODEL
STUDIES ON
Ahmet Cevdet Yalciner, Tuncay
Taymaz,, Ugur Kuran, Efim
Pelinovsky, Andrey Zaitsev.
Research Assistants Ceren
Ozer, Hulya Karakus, Gulizar Ozyurt, Ilgar Safak
in
Onur Tan, Seda Yolsal in
Our closest collaborators Nobuo Shuto,
Costas Synolakis, Fumihiko Imamura, Emile Okal are acknowledged for their endless
scientific support and cooperation
Tsunami Propagation Model for
The generation, propagation and
coastal amplification of tsunami waves are modeled using TUNAMI N2 software
which was originally authored by Fumihiko Imamura in
Tsunami event by Res. Assists. Ceren Ozer, Hulya Karakus, Gulizar Ozyurt and Ilgar Safak in Middle East Technical University (METU), Ankara-Turkey, and Efim Pelinovsky and Andrey Zaitsev from Institute of Applied Physics, Russian Academy of Sciences, Nizhny Novgorod, Russia
We have made simulations.
*******************
SIMULATION 1:
*******************
Our first estimate of the tsunami source on the date of earthquake and tsunami
(
Fault Length and Width are 666km and 90 km respectively.
Strike Angle 340
Dip Angle 13
Slip Angle 55
Displacement 20 m
Focal Depth 7 km.
The initial wave has
The maximum positive amplitude : 7.18 m
The maximum negative amplitude : 3.42 m.
Shown in the figures (links) below
http://yalciner.ce.metu.edu.tr/sumatra/0001/faultwave.jpg
http://yalciner.ce.metu.edu.tr/sumatra/0001/a000.jpg
The sea state and propagation of the wave at different time steps
in
http://yalciner.ce.metu.edu.tr/sumatra/0001/a000.jpg
http://yalciner.ce.metu.edu.tr/sumatra/0001/a060.jpg
http://yalciner.ce.metu.edu.tr/sumatra/0001/a120.jpg
http://yalciner.ce.metu.edu.tr/sumatra/0001/a180.jpg
http://yalciner.ce.metu.edu.tr/sumatra/0001/a240.jpg
http://yalciner.ce.metu.edu.tr/sumatra/0001/a300.jpg
http://yalciner.ce.metu.edu.tr/sumatra/0001/a360.jpg
The distribution of maximum amplitude in the Ocean throughout
simulation duration
http://yalciner.ce.metu.edu.tr/sumatra/0001/azmax-600dpi.jpg
http://yalciner.ce.metu.edu.tr/sumatra/0001/azmax.jpg
The run up distributions along the Coast of
http://yalciner.ce.metu.edu.tr/sumatra/0001/indoneziya.jpg
The run up distributions along the Coast of
http://yalciner.ce.metu.edu.tr/sumatra/0001/thailand_N.jpg
The run up distributions along the Coast of
http://yalciner.ce.metu.edu.tr/sumatra/0001/thailand_S.jpg
The run up distributions along the North Coast of Indian Ocean
http://yalciner.ce.metu.edu.tr/sumatra/0001/north.jpg
The coastlines where run up distributions are computed
http://yalciner.ce.metu.edu.tr/sumatra/0001/runup_area.jpg
********************
SIMULATION 2
BY USING SPHERICAL
COORDINATE
SYSTEM WITH CORIOLIS
FORCE EFFECT
********************
By Andrey Zaitsev and Efim Pelinovsky from the Institute of Applied Physics,
Russian
The same fault data given above has also been used in simulation
Initial wave
http://yalciner.ce.metu.edu.tr/sumatra/spherical/t0.jpg
After 2 hours
http://yalciner.ce.metu.edu.tr/sumatra/sphericalt2hours.jpg
Run up Distribution
http://yalciner.ce.metu.edu.tr/sumatra/spherical/ruup_area_lable.jpg
http://yalciner.ce.metu.edu.tr/sumatra/spherical/ruups_area.jpg
***********************
SIMULATION 7:
***********************
New version of simulation: Simulation 7.
Animation
http://yalciner.ce.metu.edu.tr/sumatra/0007/sim-7-b-60dpi-600min.gif
Fault Length and Width are 419km and 190km respectively.
Strike Angle 329
Dip Angle 8
Slip Angle 110
Displacement 20 m
Focal Depth 25 km.
The initial wave has
The maximum positive amplitude : 7.18 m
The maximum negative amplitude : -3.36 m
It is based on the fault parameters and initial wave shown in the figure with its link below:
http://yalciner.ce.metu.edu.tr/sumatra/0007/0000-data.jpg
In this simulation we have used shorter length of the fault by using the fault plane solutions (by Prof. Tuncay Taymaz) and historical earthquakes (Geophysicist Ugur Kuran) of the fault zones at West of Sumatra.
We have put the animation of several files in the following link
about the results of recent Simulation 7.
http://yalciner.ce.metu.edu.tr/sumatra/0007/sim-7-b-60dpi-600min.gif
The jpeg files showing the sea state at different time steps are also shown in the following links. (The file name represents the time in minutes)
http://yalciner.ce.metu.edu.tr/sumatra/0007/0000.jpg
http://yalciner.ce.metu.edu.tr/sumatra/0007/010.jpg
http://yalciner.ce.metu.edu.tr/sumatra/0007/060.jpg
http://yalciner.ce.metu.edu.tr/sumatra/0007/120.jpg
http://yalciner.ce.metu.edu.tr/sumatra/0007/240.jpg
http://yalciner.ce.metu.edu.tr/sumatra/0007/360.jpg
The distribution of maximum positive amplitudes in
http://yalciner.ce.metu.edu.tr/sumatra/0007/max-0007.jpg
The time histories of water surface fluctuations at some gauge locations near West of Sumatra
http://yalciner.ce.metu.edu.tr/sumatra/0007/sumatrawest.jpg
The time histories of water surface fluctuations at some gauge locations near East of Sumatra
http://yalciner.ce.metu.edu.tr/sumatra/0007/sumatraeast.jpg
The time histories of water surface fluctuations at some
gauge locations near
http://yalciner.ce.metu.edu.tr/sumatra/0007/thailand.jpg
The time histories of water surface fluctuations at some
gauge locations near
http://yalciner.ce.metu.edu.tr/sumatra/0007/burma.jpg
The time histories of water surface fluctuations at some
gauge locations near
http://yalciner.ce.metu.edu.tr/sumatra/0007/bangladesh.jpg
The time histories of water surface fluctuations at some
gauge locations near the border of
http://yalciner.ce.metu.edu.tr/sumatra/0007/bangladeshindia.jpg
The time histories of water surface fluctuations at some
gauge locations near
http://yalciner.ce.metu.edu.tr/sumatra/0007/india.jpg
The time histories of water surface fluctuations at some gauge locations near India East Coast
http://yalciner.ce.metu.edu.tr/sumatra/0007/indiaeast.jpg
The time histories of water surface fluctuations at some
gauge locations near
http://yalciner.ce.metu.edu.tr/sumatra/0007/indiasouth.jpg
The time histories of water surface fluctuations at some
gauge locations near
http://yalciner.ce.metu.edu.tr/sumatra/0007/srilanka.jpg
The time histories of water surface fluctuations at some
gauge locations near
http://yalciner.ce.metu.edu.tr/sumatra/0007/maldives.jpg
The time histories of water surface fluctuations at some gauge locations near Maldives-2
http://yalciner.ce.metu.edu.tr/sumatra/0007/maldives2.jpg
The time histories of water surface fluctuations at some
gauge locations near
http://yalciner.ce.metu.edu.tr/sumatra/0007/westocean.jpg
The time histories of water surface fluctuations at some
gauge locations near
http://yalciner.ce.metu.edu.tr/sumatra/0007/umman.jpg
The time histories of water surface fluctuations at some
gauge locations near
http://yalciner.ce.metu.edu.tr/sumatra/0007/aden.jpg
Figure of Tidal Wave measurements for
http://yalciner.ce.metu.edu.tr/sumatra/0007/mareg-11-aden.jpg
We acknowledge
Kassim Mohamed & Jalludin Mohamed
Observatoire
Geophysique d'Arta /CERD
BP1888 Djibouti-
R. of Djibouti
for providing the source of tidal
gauge data for
The time histories of water surface fluctuations at some gauge locations near Somali
http://yalciner.ce.metu.edu.tr/sumatra/0007/somali.jpg
The time histories of water surface fluctuations at some
gauge locations near
http://yalciner.ce.metu.edu.tr/sumatra/0007/kenya.jpg
The time histories of water surface fluctuations at some
gauge locations near
http://yalciner.ce.metu.edu.tr/sumatra/0007/tanzanya.jpg
The time histories of water surface fluctuations at some
gauge locations near