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1 AIR Worldwide Co.
388 Market
Street, Suite 750
San Francisco, California
94111
pbazzurro@air-worldwide.com
(P.B.)
2 Civil and Environmental Engineering
Department
Stanford University
Stanford, California
94305
(C.A.C.)
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We thank Stewart and Goulet for taking an interest in our work and for bringing to our attention the article by Baturay and Stewart (2003), which should have been included in our reference list. Unlike the approach presented in our article, the article by Baturay and Stewart tackles the problem of quantifying the effects of local soil to the incipient seismic waves using an empirical rather than an analytical procedure.
We certainly agree with the conclusions reached by Stewart and Goulet stating
the applicability of both methodologies for seismic-hazard estimation of
critical facilities. Our approach, which is predominantly analytical,
undoubtedly benefits from a comparison with a procedure that is based on
observations. In Figure 1 of their discussion, Stewart and Goulet provide a
useful comparison of the record- to-record variability,
, of the elastic
spectral acceleration at the soil surface,
, for f
= 3.33 Hz, conditional on the level of peak ground acceleration
(PGA) at the bedrock that derives from the application of both
procedures to different National Earthquake Hazards Reduction Program
(NEHRP) soil categories and to soft-soil sites. We were pleased to
see that this comparison is very favorable and that the values from both
approaches appear to be statistically indistinguishable. This enhanced the
credibility of both procedures. Note, however, that the values of
in Figure 1
computed using the analytical method by Bazzurro and Cornell could potentially
be reduced. Of course, reducing the variability in the surface spectral
acceleration is
Related articles in Bulletin of the Seismological Society of America:
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