Abstract
The paper looks first into the history of the derivation of the currently common formulas for calculating seismic moment magnitude M w and energy magnitude M e into the type of data and relationships available in these years and the parameter assumptions made. The general relationship between M w and M e is analysed and formulated in physical terms. The original M w- and M e-defining relationships are then confronted with equivalent relationships derived on the basis of rich modern magnitude data measured according to recently accepted International Association of Seismology and Physics of the Earth’s Interior (IASPEI) standards for (a) 20-s surface-wave data and (b) broadband body P wave data as well as M 0 and E S data based on digital broadband waveform inversion or integration. The agreement between old and new data and derived relationships is of different quality. The Richter logE S-M S relationship, which has been instrumental for deriving the current standard M w formula, could be very well reproduced with orthogonally regressed M S(20) and logE S data, provided that the latter were not corrected for source mechanism-dependent radiation. In contrast, the relationships between old and modern m B-logE S as well as m B-M S(20) data pairs deviate significantly from the respective Gutenberg and Richter relationships. Also the average E S/M 0 ratio assumed by Kanamori when deriving his M w formula differs from those of respective recent data sets. But the various differences between old and new data and data relationships compensate each other partially when deriving related M w and M e formulas. Therefore, they do not justify the modification of the existing scaling formulas, also for very pragmatic reasons. On the other hand, most striking is the so far not yet considered and by far best correlation that exists between the IASPEI body-wave magnitude standard m B(BB) and seismic energy E S, both estimated via P wave broadband records. The scatter of the logE S-m B(BB) data pair plots is only half of that of logE S-M S(20). This questions the appropriateness of the current exclusive scaling of teleseismic M e to the practically monochromatic long-period 20-s surface-wave magnitude M S. The potential advantage of a complementary M e formula, which scales the currently common teleseismic broadband P wave E S data to P wave broadband m B(BB), as well as the benefit of fast joint determination and interpretation of M w and M e in general, is discussed.
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Acknowledgments
The author is grateful to Domenico Di Giacomo for the dataset preparation and the results shown in Figs. 3, 4 and 5 and to Joachim Saul for providing the GFZ m B(BB) values. Comments of D. Di Giacomo on a first draft version also helped to improve the manuscript. Careful reviews and constructive comments by Emile A. Okal and Paolo Gasperini helped to improve the manuscript.
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Prof. Peter Bormann passed away on 11 February 2015 when this manuscript had been reviewed with recommendation of minor revisions. The requested revisions were kindly made by Dr. Domenico Di Giacomo, who volunteered for preparing the final version of the paper. The Editor would like to express his sincere thanks to Dr. Domenico Di Giacomo. This is a small tribute to Prof. Bormann’s memory.
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Bormann, P. Are new data suggesting a revision of the current M w and M e scaling formulas?. J Seismol 19, 989–1002 (2015). https://doi.org/10.1007/s10950-015-9507-y
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DOI: https://doi.org/10.1007/s10950-015-9507-y