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dc.contributor.authorPaolo
dc.contributor.authorBoccotti
dc.contributor.authorFelice
dc.contributor.authorArena
dc.contributor.authorVincenzo
dc.contributor.authorFiamma
dc.date.accessioned2017-05-08T22:04:14Z
dc.date.available2017-05-08T22:04:14Z
dc.date.copyrightMay 2013
dc.date.issued2013
dc.identifier.other%28asce%29ww%2E1943-5460%2E0000210.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl/handle/yetl/70447
dc.description.abstractAbout 6,300,000 pressure head waves beneath the sea surface were recorded by an array of 26 transducers aligned orthogonally to the coastline of Reggio Calabria, Italy. The data set covered spectra from very narrow unimodal to very broad multimodal and waves from shallow to deep waters. Herein, the quasi-determinism (QD) theory is proven to be very effective in predicting the probability of large-wave heights as well as the period and particle acceleration of these waves both on deep and shallow waters. In addition, the Tayfun model for predicting the probability of large-wave heights is also proven to be highly effective.
dc.publisherAmerican Society of Civil Engineers
dc.titleDistributions of Wave Heights in Time Domain in Stationary Sea States
dc.typeJournal Paper
dc.journal.volume139
dc.journal.issue3
dc.journal.titleJournal of Waterway, Port, Coastal, and Ocean Engineering
dc.identifier.doi10.1061/(ASCE)WW.1943-5460.0000164
dc.treeJournal of Waterway, Port, Coastal, and Ocean Engineering:;2013:;Volume ( 139 ):;issue: 003
dc.contenttypeFulltext


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