Natural Hazards: Causes and Effects - Disaster Management Center ...
Natural Hazards: Causes and Effects - Disaster Management Center ... Natural Hazards: Causes and Effects - Disaster Management Center ...
In order to function effectively, these regional systems generally have data from a number of seismic and tide stations telemetered to a central headquarters. Nearby earthquakes are located, usually in 15 minutes or less, and a warning based on seismological evidence is released to the population of the area. Since the warning is issued on the basis of seismic data alone, it is to be anticipated that warnings will occasionally be issued when tsunamis have not been generated. Since the warnings are issued only to a restricted area and confirmation of the existence or nonexistence of a tsunami is rapidly obtained, dislocations due to the higher level of protection are minimized. Thanks to this international warning system, civil defense organizations in most of the countries bordering the Pacific Ocean now receive warnings of tsunamis several hours before they reach the coasts of their respective countries. They are thus able to put into action previously prepared plans for the evacuation of people from the endangered coastal areas. 7 However, despite the development of the ocean-wide warning system, which uses the most advanced techniques of detection, measurement and communication, in many countries there are still obstacles to the rapid diffusion of warnings in thinly-populated areas or in regions where modern communication networks do not yet exist. In such areas, it is essential that the local population be informed about tsunamis. The population must be educated to recognize the signs that portend an approaching tsunami and to take appropriate action on their own initiative. The following “Tsunami Safety Rules,” issued by the United States Department of Commerce, provide an example of information that is useful in such situations: • All earthquakes do not cause tsunamis, but many do. When you hear that an earthquake has occurred, stand by for a tsunami emergency. • An earthquake in your area is a natural tsunami warning. Do not stay in low-lying coastal areas after a local earthquake. • A tsunami is not a single wave but a series of waves. Stay out of danger areas until an “allclear” is issued by competent authority. • Approaching tsunamis are sometimes heralded by a noticeable rise or fall of coastal water. This is nature’s tsunami warning and should be heeded. • A small tsunami at one beach can be a giant a few kilometers away. Don’t let the modest size of one make you lose respect for all. The Tsunami Warning Center does not issue false alarms. When a warning is issued, a tsunami exists. The tsunami of May 1960 killed 61 in Hilo, Hawaii, who thought it was “just another false alarm.” • All tsunamis—like hurricanes—are potentially dangerous, even though they may not damage every coastline they strike. • Never go down to the beach to watch for a tsunami. When you can see the wave, you are too close to escape it. • Sooner or later, tsunamis visit every coastline in the Pacific. Warnings apply to you if you live in any Pacific coastal area. • During a tsunami emergency, your local civil defense, police and other emergency organizations will try to save your life. Give them your fullest cooperation. • Unless otherwise determined by competent scientists: – for tsunamis of distant origin, potential danger areas are those less than 15 meters (50 feet) above sea level and within 1 1/2 kilometers (one mile) of the coast
– for tsunamis of local origin, potential danger areas are those less than 30 meters (100 feet) above sea level and within 1 1/2 kilometers of the coast Conclusion The impact of tsunamis is very limited geographically, affecting only land mass at the edge of some of the world’s oceans. However, where they do strike, it can be with a destructive force greater than the other types of disasters. Protecting lives and property from such losses begins with good land planning, placing high economic investments out of reach of a potential tsunami and implementing a warning/evacuation system that will maximize the safety of persons living and working near the coastlines. Notes 1 Bolt, Horn, McDonald, Scott, Geological Hazards, Springer-Verlag, New York, 1977, p. 145-146. 2 Ibid. 3 Disaster Prevention and Mitigation, A Compendium of Current Knowledge, Vol. 3 Seismological Aspects, UNDRO, p.113-114. 4 Office of Emergency Preparedness, Disaster Preparedness, U.S. Government Printing Office, 1972, p. 1011-103. 5 Frederick C. Cuny, Disasters and Development, Oxford University Press, 1983, p. 58-59. 6 UNDRO, Disaster Prevention and Mitigation, A Compendium of Current Knowledge, Vol. 3: Seismological Aspects, UNDRO, 1978, p. 114-116. 7 Ibid. p. 117. References Adams. W.M., Editor, Tsunamis in the Pacific Ocean, Honolulu: East-West Center Press, 1970. Bolt, Horn, McDonald and Scott, Geological Hazards, Springer-Verlag, New York, 1977. Cuny, Frederick C., Disasters and Development, Oxford University Press, 1983. Disaster Prevention and Mitigation, A Compendium of Current Knowledge, Vol. 3 Seismological Aspects, UNDRO, 1978. Eskite, Wilbur H., Jr., “Analysis of ESSA Activities Related to Tsunami Warnings,” A Report Prepared for NOAA Office of Plans and Programs, June 30, 1970. Iida, K., “Magnitude, Energy and Generation Mechanisms of Tsunamis and a Catalog of Earthquakes Associated with Tsunamis,” Proc. Tenth Pacific Science Congress, IUGG Monograph 24, 7-18, 1963. Office of Emergency Preparedness, Disaster Preparedness, U.S. Government Printing Office, 1972. Van Dorn, W.G., “Tsunamis, Advances in Hydroscience,” 2, p. 1-48. New York: Academic Press, 1965. Weigel, R.L., “Tsunamis,” Chapter 11 in Earthquake Engineering, New Jersey: Prentice-Hall, 1970.
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In order to function effectively, these regional systems generally have data from a number of<br />
seismic <strong>and</strong> tide stations telemetered to a central headquarters. Nearby earthquakes are<br />
located, usually in 15 minutes or less, <strong>and</strong> a warning based on seismological evidence is<br />
released to the population of the area. Since the warning is issued on the basis of seismic data<br />
alone, it is to be anticipated that warnings will occasionally be issued when tsunamis have not<br />
been generated. Since the warnings are issued only to a restricted area <strong>and</strong> confirmation of the<br />
existence or nonexistence of a tsunami is rapidly obtained, dislocations due to the higher level<br />
of protection are minimized.<br />
Thanks to this international warning system, civil defense organizations in most of the countries<br />
bordering the Pacific Ocean now receive warnings of tsunamis several hours before they reach<br />
the coasts of their respective countries. They are thus able to put into action previously<br />
prepared plans for the evacuation of people from the endangered coastal areas. 7<br />
However, despite the development of the ocean-wide warning system, which uses the most<br />
advanced techniques of detection, measurement <strong>and</strong> communication, in many countries there<br />
are still obstacles to the rapid diffusion of warnings in thinly-populated areas or in regions where<br />
modern communication networks do not yet exist. In such areas, it is essential that the local<br />
population be informed about tsunamis. The population must be educated to recognize the<br />
signs that portend an approaching tsunami <strong>and</strong> to take appropriate action on their own initiative.<br />
The following “Tsunami Safety Rules,” issued by the United States Department of Commerce,<br />
provide an example of information that is useful in such situations:<br />
• All earthquakes do not cause tsunamis, but many do. When you hear that an earthquake<br />
has occurred, st<strong>and</strong> by for a tsunami emergency.<br />
• An earthquake in your area is a natural tsunami warning. Do not stay in low-lying coastal<br />
areas after a local earthquake.<br />
• A tsunami is not a single wave but a series of waves. Stay out of danger areas until an “allclear”<br />
is issued by competent authority.<br />
• Approaching tsunamis are sometimes heralded by a noticeable rise or fall of coastal water.<br />
This is nature’s tsunami warning <strong>and</strong> should be heeded.<br />
• A small tsunami at one beach can be a giant a few kilometers away. Don’t let the modest<br />
size of one make you lose respect for all.<br />
The Tsunami Warning <strong>Center</strong> does not issue false alarms. When a warning is issued, a<br />
tsunami exists. The tsunami of May 1960 killed 61 in Hilo, Hawaii, who thought it was “just<br />
another false alarm.”<br />
• All tsunamis—like hurricanes—are potentially dangerous, even though they may not damage<br />
every coastline they strike.<br />
• Never go down to the beach to watch for a tsunami. When you can see the wave, you are<br />
too close to escape it.<br />
• Sooner or later, tsunamis visit every coastline in the Pacific. Warnings apply to you if you live<br />
in any Pacific coastal area.<br />
• During a tsunami emergency, your local civil defense, police <strong>and</strong> other emergency<br />
organizations will try to save your life. Give them your fullest cooperation.<br />
• Unless otherwise determined by competent scientists:<br />
– for tsunamis of distant origin, potential danger areas are those less than 15 meters (50<br />
feet) above sea level <strong>and</strong> within 1 1/2 kilometers (one mile) of the coast