Bulletin of the Seismological Society of America
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Bulletin of the Seismological Society of America; August 2004; v. 94; no. 4; p. 1369-1378; DOI: 10.1785/012003083
© 2004 Seismological Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (7)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Bragato, P. L.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Article

Regression Analysis with Truncated Samples and Its Application to Ground-Motion Attenuation Studies

Pier Luigi Bragato

Istituto Nazionale di Oceanografia e di Geofisica Sperimentale
Dipartimento Centro Ricerche Sismologiche
Via Treviso, 55
33100 Cussignacco (UD), Italy
pbragato{at}inogs.it

Manuscript received 30 April 2003.

The estimation of empirical attenuation laws with standard regression techniques commonly assumes the lognormal distribution of the response variable (e.g., peak ground acceleration [PGA]) for fixed values of the predictor variables (e.g., magnitude and distance from the source). Such an assumption may be invalidated by restrictions on the available sample induced by the acquisition system or imposed by the analyst, so that bias may be introduced in the estimation of regression parameters. In this article I analyze the distortion from lognormality due to station triggering. I propose a technique based on truncated regression analysis that does not require knowledge of which stations did not trigger. Furthermore, I introduce randomly truncated regression analysis to deal with thresholds that change randomly over time. This technique is adopted for stations that trigger based on the ratio between a short (STA) and long-term average (LTA) of the signal (STA/LTA ratio). I show the effectiveness of these techniques with applications to the estimation of PGA attenuation relations for both synthetic and real data sets. Real applications will refer to strong motion data from the European area and to weak motion data collected in the Friuli-Venezia Giulia and Veneto regions (northeast Italy).




This article has been cited by other articles:


Home page
Bulletin of the Seismological Society of AmericaHome page
P. J. Stafford
Conditional Prediction of Absolute Durations
Bulletin of the Seismological Society of America, June 1, 2008; 98(3): 1588 - 1594.
[Abstract] [Full Text] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
B. Pace, L. Peruzza, G. Lavecchia, and P. Boncio
Layered Seismogenic Source Model and Probabilistic Seismic-Hazard Analyses in Central Italy
Bulletin of the Seismological Society of America, February 1, 2006; 96(1): 107 - 132.
[Abstract] [Full Text] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
P. L. Bragato
Estimating an Upper Limit Probability Distribution for Peak Ground Acceleration Using the Randomly Clipped Normal Distribution
Bulletin of the Seismological Society of America, December 1, 2005; 95(6): 2058 - 2065.
[Abstract] [Full Text] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
P. L. Bragato and A. Tento
Local Magnitude in Northeastern Italy
Bulletin of the Seismological Society of America, April 1, 2005; 95(2): 579 - 591.
[Abstract] [Full Text] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
P. L. Bragato and D. Slejko
Empirical Ground-Motion Attenuation Relations for the Eastern Alps in the Magnitude Range 2.5-6.3
Bulletin of the Seismological Society of America, February 1, 2005; 95(1): 252 - 276.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2004 by the Seismological Society of America.