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The high-resolution images in this
Envirocast®
Bulletin
were captured by Space Imaging's
IKONOS satellite. They show the northwestern tip of Sumatra
(Indonesia)
before and after the moment of tsunami impact.
Image processed by StormCenter
Communications, Inc. |
New:
Envirocast
Special Edition -- South Asia Tsunami
NOTE:
Credit to
Space Imaging / CRISP -
Singapore must appear on-screen throughout the entire
air-time.
Before and After
the Tsunami - Aceh, NW Sumatra, Indonesia

Note: The animations
above shows how you can use the images to your right in your
broadcast to show how the coast was affected. Save each of the
still images to your right at the appropriate resolution for your
system (either 720x486 or 640x480) and dissolve from one to
another in sequence to achieve the above effect.
All the areas to your right include a corresponding
'before' and 'after' image that can be overlapped.
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.
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Environmental Impact:
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The
world's biggest earthquake in 40 years hit southern Asia on December 26, 2004,
unleashing a tsunami that crashed into eight countries around the Indian
Ocean.
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Just before the killer waves
struck, sea level fell rapidly, appearing like an extreme low tide and
exposing the seafloor - one of the definite warning signs of an approaching
tsunami. Then water surges onshore and powerful currents sweep
everything back out to sea.
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'After' imagery show the effects
of the water
surging onshore and the powerful currents sweeping everything back out to
sea.
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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."
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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)
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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.
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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.
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