The USGS 2023 Conterminous U.S. Time-Independent Earthquake Rupture Forecast

Author:

Field Edward H.1ORCID,Milner Kevin R.2ORCID,Hatem Alexandra E.1ORCID,Powers Peter M.1ORCID,Pollitz Fred F.3ORCID,Llenos Andrea L.1ORCID,Zeng Yuehua1ORCID,Johnson Kaj M.4ORCID,Shaw Bruce E.5ORCID,McPhillips Devin6ORCID,Thompson Jobe Jessica1ORCID,Shumway Allison M.1ORCID,Michael Andrew J.3ORCID,Shen Zheng-Kang7ORCID,Evans Eileen L.8ORCID,Hearn Elizabeth H.9ORCID,Mueller Charles S.1ORCID,Frankel Arthur D.10ORCID,Petersen Mark D.1ORCID,DuRoss Christopher1ORCID,Briggs Richard W.1ORCID,Page Morgan T.6ORCID,Rubinstein Justin L.3ORCID,Herrick Julie A.1ORCID

Affiliation:

1. 1U.S. Geological Survey, Denver Federal Center, Denver, Colorado, U.S.A.

2. 2University of Southern California, Southern California Earthquake Center, Los Angeles, California, U.S.A.

3. 3Earthquake Science Center, Moffett Field, California, U.S.A.

4. 4Department of Geological Sciences, Indiana University, Indiana, U.S.A.

5. 5Lamont–Doherty Earth Observatory, Columbia University, Palisades, New York, U.S.A.

6. 6U.S. Geological Survey, Pasadena, California, U.S.A.

7. 7Department of Earth, Planetary, and Space Sciences/UCLA, Los Angeles, California, U.S.A.

8. 8California State University, Northridge, Northridge, California, U.S.A.

9. 9Capstone Geophysics, Portola Valley, California, U.S.A.

10. 10U.S. Geological Survey, Seattle, Washington, U.S.A.

Abstract

ABSTRACT We present the 2023 U.S. Geological Survey time-independent earthquake rupture forecast for the conterminous United States, which gives authoritative estimates of the magnitude, location, and time-averaged frequency of potentially damaging earthquakes throughout the region. In addition to updating virtually all model components, a major focus has been to provide a better representation of epistemic uncertainties. For example, we have improved the representation of multifault ruptures, both in terms of allowing more and less fault connectivity than in the previous models, and in sweeping over a broader range of viable models. An unprecedented level of diagnostic information has been provided for assessing the model, and the development was overseen by a 19-member participatory review panel. Although we believe the new model embodies significant improvements and represents the best available science, we also discuss potential model limitations, including the applicability of logic tree branch weights with respect different types of hazard and risk metrics. Future improvements are also discussed, with deformation model enhancements being particularly worthy of pursuit, as well as better representation of sampling errors in the gridded seismicity components. We also plan to add time-dependent components, and assess implications with a wider range of hazard and risk metrics.

Publisher

Seismological Society of America (SSA)

Subject

Geochemistry and Petrology,Geophysics

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