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dc.contributor.authorJ. P.
dc.contributor.authorWang
dc.contributor.authorDuruo
dc.contributor.authorHuang
dc.contributor.authorSu-Chin
dc.contributor.authorChang
dc.contributor.authorYih-Min
dc.contributor.authorWu
dc.date.accessioned2017-05-08T21:57:44Z
dc.date.available2017-05-08T21:57:44Z
dc.date.copyrightFebruary 2014
dc.date.issued2014
dc.identifier.other%28asce%29nm%2E2153-5477%2E0000047.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl/handle/yetl/67510
dc.description.abstractEarthquake prediction is by all means controversial and challenging, given the fact that some recent catastrophic earthquakes went unpredicted. Not surprisingly, statistical approaches have been utilized to model earthquake randomness in time or space. One of the suggestions is that the earthquake’s temporal probability distribution should follow the Poisson model, which is suitable for rare events by definition. As a result, the customarily used hypothesis should be largely associated with the prior judgment that earthquakes are rare, but not as a result of abundant quantitative evidence or theoretical derivation. Therefore, this study aims to offer new empirical evidence to the hypothesis based on 110-year-long earthquake data around Taiwan. From the series of statistical tests, the first statistical inference is indeed in line with the model’s proposition: the level of fitting between observation and theory is better for earthquakes with a lower mean rate. To be more specific, it shows that the Poissonian hypothesis applied to local magnitude
dc.publisherAmerican Society of Civil Engineers
dc.titleNew Evidence and Perspective to the Poisson Process and Earthquake Temporal Distribution from 55,000 Events around Taiwan since 1900
dc.typeJournal Paper
dc.journal.volume15
dc.journal.issue1
dc.journal.titleNatural Hazards Review
dc.identifier.doi10.1061/(ASCE)NH.1527-6996.0000110
dc.treeNatural Hazards Review:;2014:;Volume ( 015 ):;issue: 001
dc.contenttypeFulltext


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