1990
DOI: 10.1016/0266-8920(90)90018-f
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Nonstationary Kanai-Tajimi models for El Centro 1940 and Mexico City 1985 earthquakes

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Cited by 101 publications
(37 citation statements)
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“…For the El-Centro 1940 earthquake ground motion, the value of the intensity parameter, S 0 suggested by Fan and Ahmadi [14] is equal to 1 cm 2 /s 3 . However, it will be interesting to study the variation of optimum m for dierent intensities of the earthquake ground motion (keeping the same frequency content of ground motion).…”
Section: Eects Of Intensity Of Excitation (S 0 )mentioning
confidence: 98%
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“…For the El-Centro 1940 earthquake ground motion, the value of the intensity parameter, S 0 suggested by Fan and Ahmadi [14] is equal to 1 cm 2 /s 3 . However, it will be interesting to study the variation of optimum m for dierent intensities of the earthquake ground motion (keeping the same frequency content of ground motion).…”
Section: Eects Of Intensity Of Excitation (S 0 )mentioning
confidence: 98%
“…To describe such ground motions, multi-variate random process model has been proposed. The generalised non-stationary Kanai± Tajimi model of El-Centro 1940 earthquake which was recently developed by Fan and Ahmadi [14] is considered for the present study. This model preserves the non-stationary evolution of amplitude and frequency content of the original records.…”
Section: Earthquake Ground Motionmentioning
confidence: 99%
See 1 more Smart Citation
“…To describe such ground motions, a multivariate random process model has been proposed. The generalized non-stationary Kanai-Tajimi model of the El-Centro 1940 earthquake, which was developed by Fan and Ahmadi [13], is considered for the present study. This model preserves the non-stationary evolution of amplitude and frequency content of the original record.…”
Section: Model Of Earthquake Excitationmentioning
confidence: 99%
“…Di erent ground motion generation models have di erent assumptions on stationarity or non-stationarity of the amplitude and frequency content. In this study Fan and Ahmadi [2] generalized nonstationary Kanai-Tajimi ÿlter is used, which provides a process nonstationary both in amplitude and frequency content. The interesting feature of this model is that the generated ground motions preserve the amplitude and frequency content evolution of the base ground motion.…”
Section: Introductionmentioning
confidence: 99%