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Are Regionally Calibrated Seismicity Models More Informative than Global Models? Insights from California, New Zealand, and Italy

Authors

Bayona,  José A.
External Organizations;

Savran,  William H.
External Organizations;

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Iturrieta,  Pablo Cristián
2.6 Seismic Hazard and Risk Dynamics, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Gerstenberger,  Matthew C.
External Organizations;

Graham,  Kenny M.
External Organizations;

Marzocchi,  Warner
External Organizations;

/persons/resource/ds

Schorlemmer,  Danijel
2.6 Seismic Hazard and Risk Dynamics, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Werner,  Maximilian J.
External Organizations;

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Fulltext (public)

5022638.pdf
(Publisher version), 9MB

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There is no public supplementary material available
Citation

Bayona, J. A., Savran, W. H., Iturrieta, P. C., Gerstenberger, M. C., Graham, K. M., Marzocchi, W., Schorlemmer, D., Werner, M. J. (2023): Are Regionally Calibrated Seismicity Models More Informative than Global Models? Insights from California, New Zealand, and Italy. - The Seismic Record, 3, 2, 86-95.
https://doi.org/10.1785/0320230006


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5022638
Abstract
Earthquake forecasting models express hypotheses about seismogenesis that underpin global and regional probabilistic seismic hazard assessments (PSHAs). An implicit assumption is that the comparatively higher spatiotemporal resolution datasets from which regional models are generated lead to more informative seismicity forecasts than global models, which are however calibrated on greater datasets of large earthquakes. Here, we prospectively assess the ability of the Global Earthquake Activity Rate (GEAR1) model and 19 time‐independent regional models to forecast M 4.95+ seismicity in California, New Zealand, and Italy from 2014 through 2021, using metrics developed by the Collaboratory for the Study of Earthquake Predictability (CSEP). Our results show that regional models that adaptively smooth small earthquake locations perform best in California and Italy during the evaluation period; however, GEAR1, based on global seismicity and geodesy datasets, performs surprisingly well across all testing regions, ranking first in New Zealand, second in California, and third in Italy. Furthermore, the performance of the models is highly sensitive to spatial smoothing, and the optimal smoothing likely depends on the regional tectonic setting. Acknowledging the limited prospective test data, these results provide preliminary support for using GEAR1 as a global reference M 4.95+ seismicity model that could inform eight‐year regional and global PSHAs.