Complementing regional moment magnitudes to GCMT: a perspective from the rebuilt International Seismological Centre Bulletin
-
Published:2021-05-10
Issue:5
Volume:13
Page:1957-1985
-
ISSN:1866-3516
-
Container-title:Earth System Science Data
-
language:en
-
Short-container-title:Earth Syst. Sci. Data
Author:
Di Giacomo DomenicoORCID, Harris James, Storchak Dmitry A.ORCID
Abstract
Abstract. Seismologists and geoscientists often need earthquake catalogues for various types of research.
This input usually contains basic earthquake parameters such as location (longitude, latitude, depth, and origin time), as well as
magnitude information. For the latter, the moment magnitude Mw has become the most sought after magnitude scale in the
seismological community to characterize the size of an earthquake. In this contribution we provide an informative account of
the Mw content for the newly rebuilt Bulletin of the International Seismological Centre (ISC, http://www.isc.ac.uk, last access: May 2021),
which is regarded as the most comprehensive record of the Earth's seismicity.
From this data, we extracted a list of hypocentres with Mw from a multitude of agencies reporting data to the ISC.
We first summarize the main temporal and spatial features of the Mw provided by
global (i.e. providing results for moderate to great earthquakes worldwide)
and regional agencies (i.e. also providing results for small earthquakes in a specific area).
Following this, we discuss their comparisons, by considering not only Mw
but also the surface wave magnitude MS and short-period body wave magnitude mb.
By using the Global Centroid Moment Tensor solutions as an authoritative global agency, we identify regional agencies
that best complement it and show examples of frequency–magnitude distributions in different areas obtained both
from the Global Centroid Moment Tensor alone and complemented by Mw from regional agencies.
The work done by the regional agencies in terms of Mw is fundamental to improve our understanding of the seismicity of an area, and we call for
the implementation of procedures to compute Mw in a systematic way in areas currently not well covered in this respect, such as vast parts of
continental Asia and Africa. In addition, more studies are needed to clarify the causes of the apparent overestimation of global Mw estimations
compared to regional Mw. Such difference is also observed in the comparisons of Mw with MS and mb.
The results presented here are obtained from the dataset (Di Giacomo and Harris, 2020, https://doi.org/10.31905/J2W2M64S)
stored at the ISC Dataset Repository (http://www.isc.ac.uk/dataset_repository/, last access: May 2021).
Funder
National Science Foundation U.S. Geological Survey
Publisher
Copernicus GmbH
Subject
General Earth and Planetary Sciences
Reference76 articles.
1. Aki, K.: Generation and Propagation of G Waves from the Niigata Earthquake of
June 16, 1964. Part 2. Estimation of earthquake moment, released energy, and
stress-strain drop from the G wave spectrum, Bulletin of the Earthquake
Research Institute, University of Tokyo, 44, 73–88,
available at: http://hdl.handle.net/2261/12237 (last access: April 2021), 1966. a 2. Alver, F., Ömer Kılıçarslan, Kuterdem, K., Türkoğlu, M., and
Şentürk, M. D.: Seismic Monitoring at the Turkish National Seismic
Network (TNSN), Summ. Bull. Internatl. Seismol. Cent., 53, 41–58,
https://doi.org/10.31905/D9GRP8RD, 2019. a 3. Ammon, C. J., Herrmann, R. B., Langston, C. A., and Benz, H.: Faulting
Parameters of the January 16, 1994 Wyomissing Hills, Pennsylvania
Earthquakes, Seismol. Res. Lett., 69, 261–269,
https://doi.org/10.1785/gssrl.69.3.261, 1998. a 4. Amorese, D.: Applying a Change-Point Detection Method on Frequency-Magnitude
Distributions, B. Seismol. Soc. Am., 97,
1742–1749, https://doi.org/10.1785/0120060181, 2007. a, b 5. Andrews, D. J.: Objective Determination of Source Parameters and Similarity of
Earthquakes of Different Size, in: Earthquake Source Mechanics, edited by:
S. Das, J. B. and Scholz, C., American Geophysical Union, 259–267,
https://doi.org/10.1029/gm037p0259, 1986. a
Cited by
11 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
1. Enriching the GEOFON seismic catalog with automatic energy magnitude estimations;Earth System Science Data;2024-04-05 2. World Seismic Networks and Earthquake Catalogs;Russian Journal of Earth Sciences;2024-02-29 3. Thermal structure of the southern Caribbean and northwestern South America: implications for seismogenesis;Solid Earth;2024-02-15 4. Scale of local magnitudes ML for earthquakes in the Terek-Caspian trough;Russian Journal of Seismology;2023-06-26 5. Comments on “Unbiased Estimation of Moment Magnitude from Body- and Surface-Wave Magnitudes,” by R. Das, H. Wason, and M. Sharma and “Earthquake Magnitude Conversion Problem” by R. Das, H. Wason, G. Gonzalez, M. Sharma, D. Choudhury, C. Lindholm, N. Roy, and P. Salazar;Bulletin of the Seismological Society of America;2023-03-01
|
|