In physics, in the area of dynamical systems, the Olami–Feder–Christensen model is an earthquake model conjectured to be an example of self-organized criticality where local exchange dynamics are not conservative. Despite the original claims of the authors and subsequent claims of other authors such as Lise, whether or not the model is self organized critical remains an open question. The system behaviour reproduces some empirical laws that earthquakes follow (such as the Gutenberg–Richter law and Omori's Law)
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| - Μοντέλο Olami–Feder–Christensen (el)
- Olami–Feder–Christensen model (en)
- Modelo Olami-Feder-Christensen (pt)
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| - Το μοντέλο Olami-Feder-Christensen (μοντέλο OFC) προσομοιώνει την πηγή της σεισμικής δραστηριότητας των τεκτονικών σεισμών. Το μοντέλο αυτό παρουσίασαν οι Olami Z., Feder H.J.S., και Christensen K. το 1991. Παρακάτω παρουσιάζονται μερικές βασικές πληροφορίες για το φαινόμενο των τεκτονικών σεισμών και στη συνέχεια για το πώς το μοντέλο OFC μοντελοποιεί αυτό το φαινόμενο και πώς γίνεται η προσομοίωση αυτού του μοντέλου μαζί με αποτελέσματα της προσομοίωσης . (el)
- In physics, in the area of dynamical systems, the Olami–Feder–Christensen model is an earthquake model conjectured to be an example of self-organized criticality where local exchange dynamics are not conservative. Despite the original claims of the authors and subsequent claims of other authors such as Lise, whether or not the model is self organized critical remains an open question. The system behaviour reproduces some empirical laws that earthquakes follow (such as the Gutenberg–Richter law and Omori's Law) (en)
- Na área de sistemas dinâmicos, o modelo Olami-Feder-Christensen (também conhecido como modelo OFC) foi inicialmente proposto por Z. Olami, H. J. S. Feder e K. Christensen como um modelo simplificado para a propagação de terremotos e como um exemplo da criticalidade auto-organizada (SOC). (pt)
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| - Το μοντέλο Olami-Feder-Christensen (μοντέλο OFC) προσομοιώνει την πηγή της σεισμικής δραστηριότητας των τεκτονικών σεισμών. Το μοντέλο αυτό παρουσίασαν οι Olami Z., Feder H.J.S., και Christensen K. το 1991. Παρακάτω παρουσιάζονται μερικές βασικές πληροφορίες για το φαινόμενο των τεκτονικών σεισμών και στη συνέχεια για το πώς το μοντέλο OFC μοντελοποιεί αυτό το φαινόμενο και πώς γίνεται η προσομοίωση αυτού του μοντέλου μαζί με αποτελέσματα της προσομοίωσης . (el)
- In physics, in the area of dynamical systems, the Olami–Feder–Christensen model is an earthquake model conjectured to be an example of self-organized criticality where local exchange dynamics are not conservative. Despite the original claims of the authors and subsequent claims of other authors such as Lise, whether or not the model is self organized critical remains an open question. The system behaviour reproduces some empirical laws that earthquakes follow (such as the Gutenberg–Richter law and Omori's Law) (en)
- Na área de sistemas dinâmicos, o modelo Olami-Feder-Christensen (também conhecido como modelo OFC) foi inicialmente proposto por Z. Olami, H. J. S. Feder e K. Christensen como um modelo simplificado para a propagação de terremotos e como um exemplo da criticalidade auto-organizada (SOC). (pt)
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