2021
DOI: 10.1111/risa.13690
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A Bayesian Network Model for Seismic Risk Analysis

Abstract: Earthquakes are one of the most unpredictable natural disasters. A series of secondary and derived disaster events may occur afterwards and lead to even more consequences. In such situations, a seismic risk analysis that takes into account secondary and derived disaster events is vital in reducing the risks of such disasters. The absence of a holistic seismic risk analysis model—one that takes into account the derived disaster events—may mean that the serious consequences of the disaster chains set off by eart… Show more

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Cited by 11 publications
(5 citation statements)
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“…Due to its' remarkable results, BNs have been used to deal with the occurrence and development process of emergencies, model and analyze the whole occurrence and development of emergencies. Ma and Zhang respectively introduced a conceptual framework based on Bayesian networks to analyze and verify earthquake disasters and emergency management measures [14][15].…”
Section: Literature Surveymentioning
confidence: 99%
“…Due to its' remarkable results, BNs have been used to deal with the occurrence and development process of emergencies, model and analyze the whole occurrence and development of emergencies. Ma and Zhang respectively introduced a conceptual framework based on Bayesian networks to analyze and verify earthquake disasters and emergency management measures [14][15].…”
Section: Literature Surveymentioning
confidence: 99%
“…Many organizations and regional plans around the world have emphasized the importance of improving natural disaster risk prevention capabilities [3][4][5]. Earthquakes are one of the main causes of geological disasters, and they can cause huge losses to regional populations [6][7][8][9]. A variety of disaster risk prevention measures have been formulated and adopted to reduce future impacts of earthquakes [10].…”
Section: Introductionmentioning
confidence: 99%
“…Great earthquakes can not only cause a large number of landslides, but they can also aggravate the instability of slopes for a long time after the earthquake [7,11,12,21,22]. For example, there were about 5000 landslides in the Haiti earthquake on 12 January 2010 [21], and in the Maule earthquake there were 1226 landslides over an area of 120,500 km 2 and the rock mass was more fragmented [6]. The asymmetric distribution of inclined fault may lead to differences of damage between hanging wall and footwall [23].…”
Section: Introductionmentioning
confidence: 99%
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