期刊
EARTH SYSTEM SCIENCE DATA
卷 13, 期 5, 页码 1957-1985出版社
COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/essd-13-1957-2021
关键词
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资金
- National Science Foundation [1811737, 1417970, 0949072]
- USGS [G14AC00149, G15AC00202, G18AP00035, G19AS00033]
- Directorate For Geosciences
- Division Of Earth Sciences [1417970] Funding Source: National Science Foundation
- Directorate For Geosciences
- Division Of Earth Sciences [0949072, 1811737] Funding Source: National Science Foundation
Seismologists and geoscientists often rely on earthquake catalogues, with global centroid moment tensor solutions and regional agencies providing valuable moment magnitude (Mw) information to better understand seismic activity, its distribution, and interrelationships.
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).
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