Envirocast® On-Line Special Edition

South Asia Tsunami

On December 26, 2004, a powerful earthquake occurred on the seafloor just off the coast of northern Indonesia. The earthquake measured at a magnitude of 9.0 and led to the worst tsunami that occurred in the past 40 years. The tsunami raced across the ocean at speeds up to 500 mph and reached some shores in just a matter of minutes. Some locations, including those on the other side of the Indian Ocean, anticipated the arrival of the tsunami for over 8 hours. The huge wave crashed onto the coasts of Indonesia, Malaysia, Thailand, Myanmar, India, Sri Lanka and other Asian and African countries.

Total devastation occurred in just minutes as the enormous wave, measuring between 10 and 40 feet, crashed onto the shores. Beaches and coastlines were washed away and modified in shape due to the speed and force of the intense waves and retreating water. Towns were flattened completely, trees and other vegetation were ruined, and as of January 5, 2005, the tsunami led to over 155,000 deaths of those who were unprepared. Water and airborne diseases were responsible for even more deaths after the water receded.

India Sri Lanka Maldives Indonesia Thailand


The maximum wave height that likely occurred when the wave came ashore

(Credit:  Dr. Vasily Titov, NOAA Tsunami Research Program, Pacific Marine Environmental Laboratory)

The coastline of Sumatra, near the fault boundary, received waves over 10 meters (33 feet) tall, while those farther away (Sri Lanka and Thailand) were caught by waves over 4 meters (13 feet). On the other side of the Indian Ocean, Somalia and the Seychelles were struck by waves approaching 4 meters in height (13 feet).

 

Wave Travel Time

(Credit:  Dr. Vasily Titov, NOAA Tsunami Research Program, Pacific Marine Environmental Laboratory)

Although the epicenter of the earthquake that triggered the tsunami was near the northern tip of Sumatra, the sea floor shifted along an arc stretching about 1200 km to the north. This shifting pushes a mass of water across the Indian Ocean. Wave travel times ranged from minutes (Sumatra) to 8 hours (Somalia) or more.

 

How the wave moved towards the surrounding coasts.

Click on the image to see an animation (650 KB)

(Animation provided by Kenji Satake,
National Institute of Advanced Industrial Science and Technology, Japan)

 



Before and After the Tsunami - Aceh, NW Sumatra, Indonesia

The 'before' image was taken by Space Imaging's IKONOS satellite on January 10, 2003 and the 'after' image was taken on December 29, 2004, 3 days after the tsunami event.

These IKONOS images are of Aceh, on the northwestern tip of Sumatra, Indonesia.

The effects of coastline flooding and strong coastal erosion can be observed.

Area 1 : Before Tsunami

Area 1 : After Tsunami


Area 2 : Before Tsunami

Area 2 : After Tsunami


Area 3 : Before Tsunami

Area 3 : After Tsunami


Area 4 : Before Tsunami

Area 4 : After Tsunami


Area 5 : Before Tsunami

Area 5 : After Tsunami


Hi-res Images of Tsunami Aftermath: Banda Aceh, Indonesia

Banda Aceh: After the Tsunami (Area 1)

Banda Aceh: After the Tsunami (Area 2)

Banda Aceh: Grand Mosque


Before and After Images Showing Coastal Changes in Northwest Sumatra

The 'before' image was taken by NASA's Terra satellite on December 17, 2004 and the 'after' image was taken on Dec. 29, 2004.

On December 17, the green vegetation along the west coast appears to reach all the way to the sea, with only an occasional thin stretch of white that is likely sand. After the earthquake and tsunamis, the entire western coast is lined with a noticeable purplish-brown border.

The brownish border could be deposited sand, or perhaps exposed soil that was stripped bare of vegetation when the large waves rushed ashore and then raced away. Another possibility is that parts of the coastline may have sunk as the sea floor near the plate boundary rose.

On a moderate-resolution image such as this, the affected area may seem small, but each pixel in the full resolution image is 250 by 250 meters (820 by 820 feet). In places the brown strip reaches inland roughly 13 pixels, equal to a distance of 3.25 kilometers, or about 2 miles.


Tsunami Destroys Lhoknga, Indonesia

Lhoknga before and after the moment of tsunami impact

On December 26, 2004, the Indonesian province of Aceh was hit the hardest by the earthquake and tsunamis that followed.  Sumatra, an island where Aceh is located, received the largest waves leading to the flattening of towns and devastating fatalities.

Zoom-in: Lhoknga before and after the moment of tsunami impact

The town of Lhoknga, on the west coast of Sumatra near the capital of Aceh, Banda Aceh, was completely destroyed by the tsunami. The only building that was not destroyed was the mosque, the large white feature, in the center of the city.

 

Most of the vegetation was wiped out as the tsunami flattened buildings, trees, and everything else in its path.  Beaches and coastlines were washed away and modified in shape due to the speed and force of the intense waves and retreating water.  Lakes and streams were flooded and piers were submerged in water. 

 

The low-lying agricultural areas remained covered with water and debris several days after the tsunamis


Tsunami Destroys Gleebruk Village, South Banda Aceh

 

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Before and After the Tsunami - Kalutara beach, SW Sri Lanka

The 'before' image was taken by DigitalGlobe's QuickBird satellite on January 1, 2004 and the 'after' image was taken on Dec. 26, 2004, 10:20 a.m. local time, slightly less than four hours after the 6:28 a.m. earthquake (local Sri Lanka time) and shortly after the moment of tsunami impact.

This QuickBird image of the southwestern coast of Sri Lanka--just south of the city of Colombo in a resort area called Kalutara--was collected shortly after the moment of tsunami impact. --10:20 local time; slightly less than four hours after the earthquake.

Coastline flooding was observed

-- High water evident at least a kilometer inland

--Churning ocean noted from the receding water

Area 1 : Before Tsunami

Area 1 : During Tsunami


Area 2 : Before Tsunami

Area 2 : During Tsunami


Area 3 : Before Tsunami

Area 3 : During Tsunami


Area 4 : Before Tsunami

Area 4 : During Tsunami

 

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The high-resolution images, acquired by the IKONOS satellite, show before and after views of the Male Intl' Airport in the Maldives Islands.

Male is the capital of the Maldives. The airport is located in the center of a small island called Hulule and is the first point of contact for every visitor coming from overseas.

This image was taken from 423 miles in space as IKONOS moved from north to south over the Indian Ocean.

Maldives's Male International Airport Before and After the Tsunami

The 'before' image was taken by Space Imaging's IKONOS satellite on Dec. 3, 2003 and the 'after' image was taken on Dec. 27, 2004.  The 'after' image is cloudy and hazy so the level of detail is not as good as in the 'before' image.

The imagery shows sand and debris on the runway, debris and damage to the coastline and damage to structures on the sand jetties. Other changes visible in the images may have been produced by human development along the coast (like the sand bar in the lagoon).

 

Damaged Docks and Sand Pushed Onshore

Sand on the Runway

 

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Before and After the Tsunami - Khao Lak, SW Thailand

The 'before' image was taken by Space Imaging's IKONOS satellite on January 13, 2003 and the 'after' image was taken on December 29, 2004, 3 days after the tsunami event.

These IKONOS images are of Khao Lak, on the southwestern coast of Thailand, south of the city of Takua Pa and north of Phuket.

The effects of coastline flooding can be observed and strong coastal erosion.

Area 1 : Before Tsunami

Area 1 : After Tsunami


Area 2 : Before Tsunami

Area 2 : After Tsunami

 

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This image from the Ikonos satellite shows the city of Chennai, a harbor city on the southeastern Indian coast, located about 350 kilometers (220 miles) north of the Palk Strait, which separates Sri Lanka and India. The "After" image was captured on December 29, 2004, after the waves' arrival. Although the devastation captured in this image may not seem as obvious as the damage to Sri Lanka, parts of Thailand, or northern Sumatra, a careful eye can see the impacts

Before and After Images Showing Damages to Chennai, Southeast India

Area 1 : Destroyed / Damaged Structures

A stretch of houses or other structures has been wiped out. Where the houses used to be is an open expanse of beach

Area 2 : Boats Piled on Pier

Boats that were neatly lined up in their moorings along three piers in the August 14 image are piled on top of the piers in the image from December 29.

 

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Supplementary Material:

  • Sunday 26 December 2004: at 0100 GMT, an 9.0 magnitude earthquake occurs on the seafloor near Aceh in northern Indonesia. This earthquake generated a huge tsunami wave, hitting the coasts of Indonesia, Malaysia, Thailand, Myanmar, India, Sri Lanka, Maldives and even Somalia.

  • StormCenter's Earth and Oceans expert, Dr. Ellen Prager describes the tsunami as follows:

    "
    Tsunamis can be highly variable in the way they strike, some coasts may have been struck by a towering wall of water while others may have experienced a tremendous surge of water. Much of this variability depends on the configuration of the coastline and changes in bathymetry as the waves approach. The destruction from the tsunamis comes from the onslaught of the water, the power of the waves and surge, and then the swiftly flowing currents as the water returns to the sea.

    If you live or visit the coast and you feel the earth shaking, see the ocean's level lower rapidly, or hear a loud rushing noise or bang from offshore, your immediate reaction should be to run inland and up as far as possible. Do not go to the shore to investigate and if a warning is issued, take heed and go to a safe location inland preferably on higher ground."

  • A tsunami (pronounced soo-nahm'ee) is a series of waves generated by the sudden movement or disturbance of the seafloor. Tsunamis are fast-moving, low, long waves that radiate out from a triggering event, such as an undersea earthquake, volcanic eruption, landslide or asteroid impact.  Once one of these waves reaches shallow water, they change…becoming towering, powerful walls of water that slam ashore. 

Hypothetical Tsunami along the Pacific Northwest Coast (QuickTime 2.2Mb, Courtesy: USGS )

  • Tsunamis or seismic sea waves differ markedly from typical waves generated by the wind.  Imagine blowing over the surface of a coffee cup…the top surface of the liquid inside moves in small waves.  Now shake the cup and all the water sloshes back and forth and over the lip – this is a tsunami.  In wind waves only a relatively small portion of the water is in motion…near the surface.  In contrast in a tsunami the entire water column, from the surface to the sea floor, begins to move and transfer energy.

  • Although tsunamis travel as low, very fast waves, often over 500 mph, once they reach shallow water, they slow down and bunch up.  It is here that the true danger lay.  Sometimes the water along the beach will recede right before a tsunami hits.  Seconds later, one or more towering walls of water will crash ashore.  And not only is the direct hit of the waves extremely dangerous, but also the currents created as the water piled onshore swiftly flows back out to sea.

  • The tsunami waves can travel inland along river beds and can pollute the fresh water rivers and streams with salt water from the ocean. 

    Trees, shrubs, and other vegetation were washed away polluting the cities, destroying food for animals and adding to the debris that created more destruction around the towns. Drifting materials, oil and other substances can also lead to the environmental pollution.

    Diseases infect areas where tsunamis strike as people and animals drink water tainted by sewage.  Other respiratory illnesses occur when people are forced to cram together in refugee camps.

    Other water-carrying diseases such as dysentery and cholera are also possible to occur as the water supplies are contaminated. 

  • Tsunami’s occur most commonly in Indonesia and other coastal regions around the Pacific where triggering events are more likely due to the region’s seismic activity.

 

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