Ground motion models derived using data from widespread stations and earthquakes induce significant aleatory variability when applied to predict ground motions for a single site. This issue can be even worse when the sites of interest show complex site response characteristics and do not have enough similar sites in the ground motion model development dataset. This work provides a machine-learning-based ground motion modeling framework for sites with numerous earthquake recordings. The Onahama Port Array, a liquefiable site in Japan that has recorded more than 1200 earthquakes in the last 25 years, was selected as a case study. The gradient boosting method was employed to predict response spectra with periods from 0.01 to 10 s for earthquakes with Japan Meteorological Agency (JMA) magnitude ranging from 2.4 to 9.0. Different predictor combinations were tested, and two gradient boosting models were recommended: the basic model that requires earthquake magnitude and epicentral distance as inputs, and the optimal model that requires three additional inputs, focal depth, azimuth, and rainfall. The basic and optimal gradient boosting models have the root mean square error of 0.004 and 0.001 g, average r(2) of 5-fold cross validation of 0.915 and 0.983, respectively. The results shed light on seismic hazard assessment for critical sites with long-term earthquake recordings.
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Anderson JG., 1999, SEISMOL RES LETT, V70, P19, DOI [DOI 10.1785/GSSRL.70.1.19, 10.1785/gssrl.70.1.19]
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US Geol Survey, Menlo Pk, CA 94025 USAUS Geol Survey, Menlo Pk, CA 94025 USA
Boore, David M.
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Stewart, Jonathan P.
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Univ Calif Los Angeles, Los Angeles, CA 90095 USAUS Geol Survey, Menlo Pk, CA 94025 USA
Stewart, Jonathan P.
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Seyhan, Emel
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Risk Management Solut, Newark, CA USA
Univ Calif Los Angeles, Civil & Environm Engn Dept, Los Angeles, CA 90024 USAUS Geol Survey, Menlo Pk, CA 94025 USA
Seyhan, Emel
;
Atkinson, Gail M.
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Univ Western Ontario, London, ON, CanadaUS Geol Survey, Menlo Pk, CA 94025 USA
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Sungkyunkwan Univ, Dept Stat, 25-2 Sungkyunkwan Ro, Seoul 03063, South KoreaSungkyunkwan Univ, Dept Stat, 25-2 Sungkyunkwan Ro, Seoul 03063, South Korea
Kim, Sunyul
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Hwang, Youngdeok
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CUNY, Baruch Coll, Paul H Chook Dept Informat Syst & Stat, 55 Lexington Ave, New York, NY 10010 USASungkyunkwan Univ, Dept Stat, 25-2 Sungkyunkwan Ro, Seoul 03063, South Korea
Hwang, Youngdeok
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Seo, Hwanwoo
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Ulsan Natl Inst Sci & Technol, Sch Urban & Environm Engn, 50 UNIST Gil, Ulsan 44919, South KoreaSungkyunkwan Univ, Dept Stat, 25-2 Sungkyunkwan Ro, Seoul 03063, South Korea
Seo, Hwanwoo
;
Kim, Byungmin
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Ulsan Natl Inst Sci & Technol, Sch Urban & Environm Engn, 50 UNIST Gil, Ulsan 44919, South KoreaSungkyunkwan Univ, Dept Stat, 25-2 Sungkyunkwan Ro, Seoul 03063, South Korea
机构:
US Geol Survey, Menlo Pk, CA 94025 USAUS Geol Survey, Menlo Pk, CA 94025 USA
Boore, David M.
;
Stewart, Jonathan P.
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h-index: 0
机构:
Univ Calif Los Angeles, Los Angeles, CA 90095 USAUS Geol Survey, Menlo Pk, CA 94025 USA
Stewart, Jonathan P.
;
Seyhan, Emel
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h-index: 0
机构:
Risk Management Solut, Newark, CA USA
Univ Calif Los Angeles, Civil & Environm Engn Dept, Los Angeles, CA 90024 USAUS Geol Survey, Menlo Pk, CA 94025 USA
Seyhan, Emel
;
Atkinson, Gail M.
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Univ Western Ontario, London, ON, CanadaUS Geol Survey, Menlo Pk, CA 94025 USA
机构:
Sungkyunkwan Univ, Dept Stat, 25-2 Sungkyunkwan Ro, Seoul 03063, South KoreaSungkyunkwan Univ, Dept Stat, 25-2 Sungkyunkwan Ro, Seoul 03063, South Korea
Kim, Sunyul
;
Hwang, Youngdeok
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CUNY, Baruch Coll, Paul H Chook Dept Informat Syst & Stat, 55 Lexington Ave, New York, NY 10010 USASungkyunkwan Univ, Dept Stat, 25-2 Sungkyunkwan Ro, Seoul 03063, South Korea
Hwang, Youngdeok
;
Seo, Hwanwoo
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h-index: 0
机构:
Ulsan Natl Inst Sci & Technol, Sch Urban & Environm Engn, 50 UNIST Gil, Ulsan 44919, South KoreaSungkyunkwan Univ, Dept Stat, 25-2 Sungkyunkwan Ro, Seoul 03063, South Korea
Seo, Hwanwoo
;
Kim, Byungmin
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h-index: 0
机构:
Ulsan Natl Inst Sci & Technol, Sch Urban & Environm Engn, 50 UNIST Gil, Ulsan 44919, South KoreaSungkyunkwan Univ, Dept Stat, 25-2 Sungkyunkwan Ro, Seoul 03063, South Korea