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)