Does the future of tsunami intensity scales lie in past events?
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  • 作者:A. Barberopoulou ; F. Scheele
  • 关键词:Tsunami ; Intensity scale ; Hazard map ; Historical tsunami
  • 刊名:Natural Hazards
  • 出版年:2016
  • 出版时间:January 2016
  • 年:2016
  • 卷:80
  • 期:1
  • 页码:401-424
  • 全文大小:2,383 KB
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  • 作者单位:A. Barberopoulou (1) (2)
    F. Scheele (3)

    1. Tectonophysics, GNS Science, 1 Fairway Dr., Lower Hutt, 5010, New Zealand
    2. National Observatory of Athens, Lofos Nymphon, Thiseio, P.O. Box 20048, 11810, Athens, Greece
    3. Department of Geological Sciences, University of Canterbury, PB 4800, Christchurch, 8140, New Zealand
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciences
    Hydrogeology
    Geophysics and Geodesy
    Geotechnical Engineering
    Civil Engineering
    Environmental Management
  • 出版者:Springer Netherlands
  • ISSN:1573-0840
文摘
Post-disaster assessments for historical tsunami events (>25 years old) are either scarce or contain limited information. In this study, we assess ways to examine tsunami impacts by utilizing data from old events, but more importantly we examine how to best utilize information contained in tsunami historical databases, in order to provide meaningful products that describe the impact of the event. As such, a tsunami intensity scale was applied to two historical events that were observed in New Zealand (one local and one distant), in order to utilize the largest possible number of observations in our dataset. This is especially important for places like New Zealand where the tsunami historical record is short, going back only to the nineteenth century, and where instrument recordings are only available for the most recent events. We found that despite a number of challenges in using intensities—uncertainties partly due to limitations of historical event data—these data with the help of GIS tools can be used to produce hazard maps and offer an alternative way to exploit tsunami historical records. Most importantly, the assignment of intensities at each point of observation allows for the utilization of many more observations than if one depends on physical information alone, such as water heights. We hope these results may be used toward developing a well-defined methodology for hazard assessments and refine our knowledge for past tsunami events for which the tsunami sources are largely unknown, but also when physical quantities describing the tsunami (e.g., water height, flood depth, and run-up) are scarce. Keywords Tsunami Intensity scale Hazard map Historical tsunami

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