Yuchen Wang , Cesar Jiménez , Nick Moreno , Peitao Wang
{"title":"Tsunami characteristics and source estimation of the 2024 Yauca (Peru) earthquake","authors":"Yuchen Wang , Cesar Jiménez , Nick Moreno , Peitao Wang","doi":"10.1016/j.oceaneng.2025.121325","DOIUrl":null,"url":null,"abstract":"<div><div>The 2024 Yauca earthquake occurred on June 28 as a result of the subduction of the Nazca Plate beneath the South American Plate along the Peru-Chile Trench. It generated a moderate tsunami, which was recorded by tide gauges and offshore buoys. We removed low-frequency components from the sea level elevation records and analyzed the characteristics of the tsunami waveforms. Additionally, wavelet analysis was performed to investigate the temporal variations in dominant periods. We conducted a joint inversion using tsunami data from San Juan de Marcona, Chala, and DART 32401, along with teleseismic data from 25 broadband stations. A finite-fault model of 80.0 km × 60.0 km was proposed, consisting of 8 × 6 subfaults. We changed the rupture velocity (<span><math><mrow><msub><mi>V</mi><mi>r</mi></msub></mrow></math></span>) from 1.8 to 4.2 km/s. The optimum <span><math><mrow><msub><mi>V</mi><mi>r</mi></msub></mrow></math></span> was 3.6 km/s. In this scenario, the maximum and average slip values were 0.65 and 0.27 m, respectively. The finite-fault model resulted in a seismic moment (<span><math><mrow><msub><mi>M</mi><mn>0</mn></msub></mrow></math></span>) of 4.738 × 10<sup>19</sup> Nm and a moment magnitude (<span><math><mrow><msub><mi>M</mi><mi>w</mi></msub></mrow></math></span>) of 7.05. Our proposed model can effectively reproduce the tsunami behavior along the southern coast of Peru. It helps to understand the tsunami and earthquake hazards in this region.</div></div>","PeriodicalId":19403,"journal":{"name":"Ocean Engineering","volume":"331 ","pages":"Article 121325"},"PeriodicalIF":4.6000,"publicationDate":"2025-04-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Ocean Engineering","FirstCategoryId":"5","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0029801825010388","RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ENGINEERING, CIVIL","Score":null,"Total":0}
引用次数: 0
Abstract
The 2024 Yauca earthquake occurred on June 28 as a result of the subduction of the Nazca Plate beneath the South American Plate along the Peru-Chile Trench. It generated a moderate tsunami, which was recorded by tide gauges and offshore buoys. We removed low-frequency components from the sea level elevation records and analyzed the characteristics of the tsunami waveforms. Additionally, wavelet analysis was performed to investigate the temporal variations in dominant periods. We conducted a joint inversion using tsunami data from San Juan de Marcona, Chala, and DART 32401, along with teleseismic data from 25 broadband stations. A finite-fault model of 80.0 km × 60.0 km was proposed, consisting of 8 × 6 subfaults. We changed the rupture velocity () from 1.8 to 4.2 km/s. The optimum was 3.6 km/s. In this scenario, the maximum and average slip values were 0.65 and 0.27 m, respectively. The finite-fault model resulted in a seismic moment () of 4.738 × 1019 Nm and a moment magnitude () of 7.05. Our proposed model can effectively reproduce the tsunami behavior along the southern coast of Peru. It helps to understand the tsunami and earthquake hazards in this region.
期刊介绍:
Ocean Engineering provides a medium for the publication of original research and development work in the field of ocean engineering. Ocean Engineering seeks papers in the following topics.