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Bulletin of the Seismological Society of America; December 1987; v. 77; no. 6; p. 2115-2124
© 1987 Seismological Society of America
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On least-squares estimation of b values

PETER GUTTORP

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.




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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.





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