1984
DOI: 10.1016/0141-1187(84)90050-6
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Numerical simulation of a random sea: a common error and its effect upon wave group statistics

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Cited by 160 publications
(89 citation statements)
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“…Eq. (16) implies that the relationship between the inertia-induced component of the quasi-static response and nodal water particle accelerations is not linear. The reason for nonlinearity is that in calculating the nonlinear quasi-static response, the effect of load intermittency on members in the splash zone has also been included.…”
Section: Simulation Of Linear Quasi-static Re-sponsementioning
confidence: 99%
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“…Eq. (16) implies that the relationship between the inertia-induced component of the quasi-static response and nodal water particle accelerations is not linear. The reason for nonlinearity is that in calculating the nonlinear quasi-static response, the effect of load intermittency on members in the splash zone has also been included.…”
Section: Simulation Of Linear Quasi-static Re-sponsementioning
confidence: 99%
“…The theoretical probability distribution of the linear quasi-static response extreme values during period T (based on the assumption that the linear response is a Gaussian random process) is derived from the following relationship [16]. (21) where denotes the linear response extreme value, M = T/T z is the expected number of zero-upcrossings of the linear response during period T and is the standard deviation of linear response.…”
Section: Theoretical Backgroundmentioning
confidence: 99%
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“…Modal amplitudes are drawn from a Rayleigh distribution with variance derived from the observed (or theoretical) density spectrum, and random phases are added (see Tucker et al, 1984).…”
Section: Deterministic Models: Time-domain and Spectral-domainmentioning
confidence: 99%