Papadopoulos-Imamura tsunami intensity scale Open new window
The proposed tsunami intensity scale by Papadopoulos and Imamura (2001) incorporates twelve divisions and is consistent with the several twelve-grade seismic intensity scales established and extensively used in Europe and North America in about the last 100 years. The new scale is arranged according to the effects on humans; the effects on objects, including vessels of variable size, and on nature; and damage to buildings. Maramai et al. (2014) specifies that this intensity scale has been calibrated to modern coastal environments, therefore does not provide accurate information when evaluating historical events .
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Intensity | Effects on humans | Effects on objects, including vessels of variable size, and on nature | Damage to buildings |
I. Not felt |
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II. Scarcelyfelt |
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III. Weak |
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IV. Largelyobserved |
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| V. Strong |
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VI. Slightlydamaging |
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VII. Damaging |
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VIII. Heavilydamaging |
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IX. Destructive |
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X. Verydestructive |
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XI. Devastating |
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XII. Completelydevastating |
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Reference: Papadopoulos, G. A., & Imamura, F. (2001, August). A proposal for a new tsunami intensity scale. In ITS 2001 proceedings (Vol. 5, pp. 569-577).
Classification of damage to building
Although the classification of damage to buildings due to earthquakes is well defined (e.g. Coburn & Spence, 1992) such a classification is not still available for damage to buildings due to tsunamis. Therefore, only a gross classification is used in association to the tsunami intensity scale:
- Grade 1: Slight damage
- Grade 2: Moderate damage
- Grade 3: Heavy damage
- Grade 4: Destruction
- Grade 5: Total damage
Source: The New Tsunami Intensity Scale. NEAMTIC, IOC/UNESCO. (a new window will open)