sessione 2.3 - Ogs

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GNGTS 2009 SESSIONE <strong>2.3</strong> ries to be used as meaningful design input. The “spectral cloud” is defined as the ensemble of the spectral ordinates, computed at multiple reference periods, of a group of seismic records (Fig. 1). If, in addition to the complete knowledge of the characteristics of the distribution of the random variables, were the autocorrelation functions of the response spectra known, the response spectra could be seen as a set of signals of a stochastic process. The identification of earthquake inputs of given hazard is generally obtained through a two-step association. The first step encompasses the association between an exceedance probability, 500
GNGTS 2009 SESSIONE <strong>2.3</strong> Fig. 2 - Uniform hazard spectrum and uniform hazard spectral cloud, for the site of Bologna over an observation time of t = 50 years, for a rare seismic hazard level. 501
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GNGTS 2009 sessione 2.3 Rischio sis
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GNGTS 2009 SESSIONE 2.3 INDIVIDUATI
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GNGTS 2009 SESSIONE 2.3 Fig. 4 - Sc
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GNGTS 2009 SESSIONE 2.3 Fig. 4 - a)
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GNGTS 2009 SESSIONE 2.3 sismiche è
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GNGTS 2009 SESSIONE 2.3 Fig. 2 - (a
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GNGTS 2009 SESSIONE 2.3 RIVISITANDO
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sessione 2.3 - Ogs

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