Abstract:
Two-third of the coastal belt of Sri Lanka suffered massive loss of life and damage to
property due to the tsunami generated by the great earthquake of 26 December 2004 in the
Andaman-Sumatran subduction zone. The extension of tsunami inundation and consequent
damage were not uniform over the tsunami affected coastal areas. Therefore, a detailed
assessment of the onshore distance within which significant inundation can be caused by
potential tsunami may provide useful information to identify low-hazard site areas to
^ c a te evacuation centers and to prepare evacuation routes.
The MOST (Method of Splitting Tsunami) model, developed by National Oceanic and
Atmospheric Administration (NOAA) is one of only two fully .validated hydrodynamic
models for operational tsunami propagation and inundation. Inundation Phase modeling
performs on three distinct, nested, but overlapping DEM ( Digital Elevation Model) finite
difference data sets and model outputs are Tsunami arrival time, Maximum wave height
and inundation level.
MOST model is simulated for Sumatra 2004 Tsunami with 8.8 magnitude to see the
impact on different coastal areas. Inundation studies are conducted taking a probabilistic
approach in which multiple tsunami scenarios are considered. For this study two
tsunamigenic fault rupture scenarios are investigated for Makran subduction zone located
in the north of the Arabian Sea and Arakan subduction zone located in the north east of
the Bay of Bengal.
