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Integrated disaster risk reduction

in the Southeast Asian region

Dato’ Ibrahim Bin Komoo, Southeast Asian Disaster Prevention

Research Institute, Universiti Kebangsaan, Malaysia

S

outheast Asia is one of the most vulnerable parts of the

world to natural disaster. The region is frequently exposed

to hazards due to geological processes such as earthquakes,

tsunamis, volcanic eruptions and landslides, and climatic hazards

such as floods, droughts, typhoons and storms. Natural disaster

is the main contributing factor to the high level of casualties and

property damage in many countries, which have yet to implement

appropriate disaster risk reduction (DRR) strategies.

The Southeast Asia Disaster Prevention Research Institute

(SEADPRI), established by Universiti Kebangsaan, Malaysia in 2008,

focuses on initiatives for integrating the management of DRR via

research in the Southeast Asia region. Its aims are to lead innova-

tive knowledge transfer on holistic disaster prevention in the region

and to research issues related to science and governance for DRR.

Multidisciplinary research programmes in disaster management and

DRR are conducted to expand knowledge of climatic, geological and

technological hazards. Training of human capital is also a primary

focus, particularly in addressing disaster issues for both the public

and private sectors through postgraduate programmes.

Information gathered by SEADPRI shows that a

variety of natural disasters have taken a cumulative

toll on countries across the region in recent years.

Significant disasters recorded in the Southeast Asia

region are as follows:

Earthquake and tsunami

Earthquake is the major geological hazard in Southeast

Asia. The region is the most tectonically active zone on

earth as the lithospheric plate is crushed between three

major subducting oceanic plates, namely the eastward-

moving Indian Ocean Crust, the westward-moving

Philippines Sea Plate and Pacific Plate and the north-

ward-moving Australian Plate, squeezed northwards

towards the Eurasian Plate. Collisions along these

boundaries have caused enormous earthquake events.

Several large-scale earthquakes have triggered tsunamis,

which lead to high levels of risk particularly to coastal

areas in Indonesia and the Philippines.

The North Sumatra earthquake that took place in

2004 with a magnitude of 9.3, followed by a tsunami,

was a critical lesson for countries in Southeast Asia,

revealing that most of these countries were still unpre-

pared to face major natural disasters. Deaths due

to the tsunami in the affected countries were very

high: 165,708 in Indonesia, 8,345 in Thailand, 80 in

Malaysia, 61 in Myanmar, 35,222 in Sri Lanka and

12,405 in India. The events highlighted several basic

weaknesses in the region, particularly in terms of the

lack of infrastructure, emergency response, prepared-

ness and public awareness.

Such gigantic seismically triggered tsunamis events

have caused catastrophic consequences in terms of

the number of people killed – for example in 1992 in

Flores, Indonesia (2,200 deaths), in 1990 in Luzon

(1,621 deaths), in 1998 in Papua New Guinea (2,183

deaths), in 2004 in Indonesia (227,898 people killed

and about 1.7 million people displaced), and in 2005

Northern Sumatra (1,000 people killed). Earthquakes

also trigger landslides. On the coast of Padang after

the Sumatra earthquake (2009), several villages slid

into the valley after the quake, killing 1,117 people

and injuring 1,214. There was damage to 181,665

buildings and 451,000 people were displaced in the

Padang-Pariaman area.

2001

Rockfall along the main highway near Kuala Lumpur. Landslides on man-made

slopes are the most common hazards for the Southeast Asia region

Image: SEADPRI