Development of Tsunami Frequency-Fatality Numbers ( F-N ) Curve for Coastal Communities Subjected to Cascadia Subduction Earthquakes
Author:
Affiliation:
1. Dept. of Earth Sciences, Western Univ., London, ON, Canada.
2. Dept. of Earth and Environmental Sciences, Univ. of Waterloo, Waterloo, ON, Canada.
Publisher
American Society of Civil Engineers
Link
https://ascelibrary.org/doi/pdf/10.1061/9780784485163.070
Reference11 articles.
1. What Is Wrong with Criterion FN-Lines for Judging the Tolerability of Risk?
2. Stochastic source modelling and tsunami simulations of Cascadia subduction earthquakes for Canadian Pacific coast.;Goda K.;Coastal Eng. J,2022
3. Goda K. (2023). “Probabilistic multi-hazard shaking-tsunami risk assessment for the District of Tofino British Columbia Canada subjected to megathrust Cascadia subduction events.” Proc. 14th Intl. Conf. App. Stat. Prob. Civil Eng. (ICASP14) Dublin Ireland Paper 26.
4. Goldfinger C. et al. (2012). Turbidite Event History: Methods and Implications for Holocene Paleoseismicity of the Cascadia Subduction Zone. United States Geological Survey Professional Paper 1661–F. Available at: http://pubs.usgs.gov/pp/pp1661f/.
5. HSE (Health and Safety Executive). (1992). The Tolerability of Risks from Nuclear Power Stations. Her Majesty’s Stationery Office, London, United Kingdom.
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