|
|
||||||||
DEPARTMENT OF STATISTICS GN-22 UNIVERSITY OF WASHINGTON, SEATTLE, WASHINGTON 98195
Abstract
Although the maximum-likelihood estimator of b values is optimal from a certain statistical point of view, given the Gutenberg-Richter frequency-magnitude relation, many researchers have been using least-squares fitting of a straight line to the frequency-magnitude plot. However, ordinary least squares is an inefficient method. A generalized least-squares approach is statistically more satisfactory. The details of this method are given and applied to data from California. The improvement in efficiency is substantial. In addition, the generalized least-squares approach works well also for data from a different frequency-magnitude relation, proposed by Lomnitz-Adler and Lomnitz. The maximum-likelihood estimator (from the Gutenberg-Richter model) has too large a variability in this situation.
This article has been cited by other articles:
![]() |
Duration Magnitude Uncertainty due to Seismic Noise: Inferences on the Temporal Pattern of G-R b-value at Mt. Vesuvius, Italy Bulletin of the Seismological Society of America, August 1, 2003; 93(4): 1847 - 1853. |
||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |