Articles | Volume 19, issue 7
https://doi.org/10.5194/nhess-19-1565-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/nhess-19-1565-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Revised earthquake sources along Manila trench for tsunami hazard assessment in the South China Sea
Qiang Qiu
Asian School of the Environment, Nanyang Technological University, Singapore
Department of Earth Sciences, University of Southern California, Los Angeles, CA, USA
School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou, China
Department of Civil and Environmental Engineering, National University of Singapore, Singapore
Ya-Ju Hsu
Institute of Earth Sciences, Academia Sinica, Taipei, Taiwan
Yu Wang
Department of Geosciences, National Taiwan University, Taipei, Taiwan
Chung-Han Chan
Earth Observatory of Singapore, Nanyang Technological University, Singapore
Adam D. Switzer
Asian School of the Environment, Nanyang Technological University, Singapore
Earth Observatory of Singapore, Nanyang Technological University, Singapore
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Jun Yu Puah, Ivan D. Haigh, David Lallemant, Kyle Morgan, Dongju Peng, Masashi Watanabe, and Adam D. Switzer
Ocean Sci., 20, 1229–1246, https://doi.org/10.5194/os-20-1229-2024, https://doi.org/10.5194/os-20-1229-2024, 2024
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Coastal currents have wide implications for port activities, transport of sediments, and coral reef ecosystems; thus a deeper understanding of their characteristics is needed. We collected data on current velocities for a year using current meters at shallow waters in Singapore. The strength of the currents is primarily affected by tides and winds and generally increases during the monsoon seasons across various frequencies.
Andrea Verolino, Su Fen Wee, Susanna F. Jenkins, Fidel Costa, and Adam D. Switzer
Nat. Hazards Earth Syst. Sci., 24, 1203–1222, https://doi.org/10.5194/nhess-24-1203-2024, https://doi.org/10.5194/nhess-24-1203-2024, 2024
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Submarine volcanic eruptions represent the majority of eruptions taking place on Earth. Still, they are vastly understudied worldwide. Here we compile a new dataset and assess the morphology, depth, and height of submarine volcanoes in Southeast Asia and its surroundings to understand their hazard-exposure potential in the region. This study will serve as a stepping stone for future quantitative hazard assessments from submarine eruptions in Southeast Asia and neighbouring countries.
Zhi Yang Koh, Benjamin S. Grandey, Dhrubajyoti Samanta, Adam D. Switzer, Benjamin P. Horton, Justin Dauwels, and Lock Yue Chew
EGUsphere, https://doi.org/10.5194/egusphere-2024-294, https://doi.org/10.5194/egusphere-2024-294, 2024
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Identifying tide-surge interaction (TSI) can be a complex task. We enhance existing statistical methods with a more robust test that accounts for complex tides, and investigate the influence of tidal phase alteration on TSI using a semi-empirical model. We apply these techniques to tide-gauge records from the east coast of Singapore and Malaysia. We found TSI at all studied locations, and that tidal phase alteration can change the timing of large surges with minimal impact on their height.
Edlira Xhafaj, Chung-Han Chan, and Kuo-Fong Ma
Nat. Hazards Earth Syst. Sci., 24, 109–119, https://doi.org/10.5194/nhess-24-109-2024, https://doi.org/10.5194/nhess-24-109-2024, 2024
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Our study introduces new earthquake forecasting models for Albania, aiming to map out future seismic hazards. By analysing earthquakes from 1960 to 2006, we have developed models that predict where activity is most likely to occur, highlighting the western coast and southern regions as high-hazard zones. Our validation process confirms these models are effective tools for anticipating seismic events, offering valuable insights for earthquake preparedness and hazard assessment efforts.
Gui Hu, Linlin Li, Zhiyuan Ren, and Kan Zhang
Nat. Hazards Earth Syst. Sci., 23, 675–691, https://doi.org/10.5194/nhess-23-675-2023, https://doi.org/10.5194/nhess-23-675-2023, 2023
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We explore the tsunamigenic mechanisms and the hydrodynamic characteristics of the 2022 Hunga Tonga–Hunga Ha'apai volcanic tsunami event. Through extensive analysis of tsunami waveforms, we identify four distinct tsunami components from different physical mechanisms. The long-lasting oscillation of the tsunami event in the Pacific Ocean was mainly associated with the interplay of the ocean waves left by atmospheric waves with local bathymetry.
Liqing Jiao, Teng Wang, Guangcai Feng, Paul Tapponnier, Andrean V. H. Simanjuntak, and Chung-Han Chan
EGUsphere, https://doi.org/10.5194/egusphere-2022-563, https://doi.org/10.5194/egusphere-2022-563, 2022
Preprint archived
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It is always difficult to quantify seismic hazard for a region with a complex fault system. Thus, we proposed a physics-based model and confirm its credibility through fitting a case of an Indonesian earthquake. Our model could be further applied for evaluating potential seismic hazard in strong ground shaking and fault displacement.
Raquel P. Felix, Judith A. Hubbard, Kyle E. Bradley, Karen H. Lythgoe, Linlin Li, and Adam D. Switzer
Nat. Hazards Earth Syst. Sci., 22, 1665–1682, https://doi.org/10.5194/nhess-22-1665-2022, https://doi.org/10.5194/nhess-22-1665-2022, 2022
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The Flores Thrust lies along the north coasts of Bali and Lombok. We model how an earthquake on this fault could trigger a tsunami that would impact the regional capital cities of Mataram and Denpasar. We show that for 3–5 m of slip on the fault (a Mw 7.5–7.9+ earthquake), the cities would experience a wave ca. 1.6–2.7 and ca. 0.6–1.4 m high, arriving in < 9 and ca. 23–27 min, respectively. They would also experience subsidence of 20–40 cm, resulting in long-term exposure to coastal hazards.
Kai Wan Yuen, Adam D. Switzer, Paul P. S. Teng, and Janice Ser Huay Lee
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2022-4, https://doi.org/10.5194/nhess-2022-4, 2022
Manuscript not accepted for further review
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Few databases provide standardized reporting of disaster-related agricultural damage and loss. We compiled cyclone-induced rice damage data from 1970–2018 in four countries in Asia (Bangladesh, Myanmar, Philippines and Vietnam). Of the 1,046 cyclone events recorded, 13 % or 138 events were associated with rice damage. Philippines and Vietnam accounted for 128 of these events. While higher cyclone intensity tend to cause most damage, lower intensity events were more frequent.
Chieh-Chen Chang, Chih-Yu Chang, and Chung-Han Chan
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2022-46, https://doi.org/10.5194/nhess-2022-46, 2022
Revised manuscript not accepted
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A rupture taking place along several faults can cause a large earthquake and often leads to disaster. This study identifies structures that could rupture simultaneously based on a physics-based model and proposes a set of formulas to evaluate their recurrence intervals and uncertainties. Our approach’s procedure can be applied to reexamining the composite ruptures of the seismogenic structure system in Taiwan and other regions, beneficial to subsequent probabilistic seismic hazard assessment.
Dominik Jackisch, Bi Xuan Yeo, Adam D. Switzer, Shaoneng He, Danica Linda M. Cantarero, Fernando P. Siringan, and Nathalie F. Goodkin
Nat. Hazards Earth Syst. Sci., 22, 213–226, https://doi.org/10.5194/nhess-22-213-2022, https://doi.org/10.5194/nhess-22-213-2022, 2022
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The Philippines is a nation very vulnerable to devastating typhoons. We investigate if stable isotopes of precipitation can be used to detect typhoon activities in the Philippines based on daily isotope measurements from Metropolitan Manila. We find that strong typhoons such as Rammasun, which occurred in July 2014, leave detectable isotopic signals in precipitation. Besides other factors, the distance of the typhoon to the sampling site plays a key role in influencing the signal.
Constance Ting Chua, Adam D. Switzer, Anawat Suppasri, Linlin Li, Kwanchai Pakoksung, David Lallemant, Susanna F. Jenkins, Ingrid Charvet, Terence Chua, Amanda Cheong, and Nigel Winspear
Nat. Hazards Earth Syst. Sci., 21, 1887–1908, https://doi.org/10.5194/nhess-21-1887-2021, https://doi.org/10.5194/nhess-21-1887-2021, 2021
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Port industries are extremely vulnerable to coastal hazards such as tsunamis. Despite their pivotal role in local and global economies, there has been little attention paid to tsunami impacts on port industries. For the first time, tsunami damage data are being extensively collected for port structures and catalogued into a database. The study also provides fragility curves which describe the probability of damage exceedance for different port industries given different tsunami intensities.
Kai Wan Yuen, Tang Thi Hanh, Vu Duong Quynh, Adam D. Switzer, Paul Teng, and Janice Ser Huay Lee
Nat. Hazards Earth Syst. Sci., 21, 1473–1493, https://doi.org/10.5194/nhess-21-1473-2021, https://doi.org/10.5194/nhess-21-1473-2021, 2021
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We used flow diagrams to represent the ways in which anthropogenic land use and natural hazards have affected rice production in the two
mega-deltas of Vietnam. Anthropogenic developments meant to improve productivity may create negative feedbacks on rice production and quality. Natural hazards further amplify problems created by human activities. A systems-thinking approach can yield nuanced perspectives for tackling environmental challenges.
Liqing Jiao, Chung-Han Chan, Luc Scholtès, Aurélia Hubert-Ferrari, Frédéric-Victor Donzé, and Paul Tapponnier
Solid Earth Discuss., https://doi.org/10.5194/se-2020-41, https://doi.org/10.5194/se-2020-41, 2020
Revised manuscript not accepted
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Seafloor geometry plays an important role in earthquake behaviors in a tectonic subducting system. Here, we simulate a subducting slab with a seafloor irregularity to perform the resulting deformation pattern of the overriding plate and spatial and temporal patterns of the seismicity activity in the subducting system. Our model is overall comparable to paleoseismic records, matches seismicity patterns, and fulfils the domain definition of a subduction system.
Linlin Li, Jie Yang, Chuan-Yao Lin, Constance Ting Chua, Yu Wang, Kuifeng Zhao, Yun-Ta Wu, Philip Li-Fan Liu, Adam D. Switzer, Kai Meng Mok, Peitao Wang, and Dongju Peng
Nat. Hazards Earth Syst. Sci., 18, 3167–3178, https://doi.org/10.5194/nhess-18-3167-2018, https://doi.org/10.5194/nhess-18-3167-2018, 2018
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Typhoon Hato was one of the most damaging natural disaster events in the western Pacific region in 2017. It caused the the worst flooding in Macau since its instrumental records began in 1925. We present a high-resolution survey map recording inundation depths and distances at 278 sites in Macau. We provide a series of inundation maps under different tidal and sea levels. The maps that highlight adaptive strategies are essential in order to keep up with the pace of rising sea level.
Chung-Han Chan
Nat. Hazards Earth Syst. Sci., 16, 2177–2187, https://doi.org/10.5194/nhess-16-2177-2016, https://doi.org/10.5194/nhess-16-2177-2016, 2016
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This study provides some new insights into earthquake forecasting models that are applied to regions with subduction systems, including the depth component for forecasting grids and time-dependent factors. These insights into the applications of forecasting models could provide key information regarding seismic and tsunami hazard assessments.
Related subject area
Earthquake Hazards
Co- and postseismic subaquatic evidence for prehistoric fault activity near Coyhaique, Aysén Region, Chile
Forearc crustal faults as tsunami sources in the upper plate of the Lesser Antilles subduction zone: the case study of the Morne Piton fault system
The 2020 European Seismic Hazard Model: overview and results
Risk-informed representative earthquake scenarios for Valparaíso and Viña del Mar, Chile
Harmonizing seismicity information in Central Asian countries: earthquake catalogue and active faults
Comparing components for seismic risk modelling using data from the 2019 Le Teil (France) earthquake
2021 Alaska Earthquake: entropy approach to its precursors and aftershock regimes
Modelling seismic ground motion and its uncertainty in different tectonic contexts: challenges and application to the 2020 European Seismic Hazard Model (ESHM20)
Correlation between seismic activity and acoustic emission on the basis of in-situ monitoring
Scoring and ranking probabilistic seismic hazard models: an application based on macroseismic intensity data
A dense micro-electromechanical system (MEMS)-based seismic network in populated areas: rapid estimation of exposure maps in Trentino (NE Italy)
Exploring inferred geomorphological sediment thickness as a new site proxy to predict ground-shaking amplification at regional scale: application to Europe and eastern Türkiye
Surface rupture kinematics of the 2020 Mw 6.6 Masbate (Philippines) earthquake determined from optical and radar data
The influence of aftershocks on seismic hazard analysis: a case study from Xichang and the surrounding areas
Characteristics and mechanisms of near-surface negative atmospheric electric field anomalies preceding the 5 September 2022, Ms 6.8 Luding earthquake in China
Seismogenic depth and seismic coupling estimation in the transition zone between Alps, Dinarides and Pannonian Basin for the new Slovenian seismic hazard model
Towards a dynamic earthquake risk framework for Switzerland
Understanding flow characteristics from tsunami deposits at Odaka, Joban Coast, using a deep neural network (DNN) inverse model
Spring water anomalies before two consecutive earthquakes (Mw 7.7 and Mw 7.6) in Kahramanmaraş (Türkiye) on 6 February 2023
Update on the seismogenic potential of the Upper Rhine Graben southern region
Earthquake forecasting model for Albania: the area source model and the smoothing model
Estimating Ground Motion Intensities Using Simulation-Based Estimates of Local Crustal Seismic Response
Testing the 2020 European Seismic Hazard Model (ESHM20) against observations from Romania
Probabilistic Seismic Hazard Assessment of Sweden
The footprint of a historical paleoearthquake: the sixth-century-CE event in the European western Southern Alps
Strategies for Comparison of Modern Probabilistic Seismic Hazard Models and Insights from the Germany and France Border Region
Seismic background noise levels in the Italian strong-motion network
Testing machine learning models for heuristic building damage assessment applied to the Italian Database of Observed Damage (DaDO)
The seismic hazard from the Lembang Fault, Indonesia, derived from InSAR and GNSS data
Development of a regional probabilistic seismic hazard model for Central Asia
The European Fault-Source Model 2020 (EFSM20): geologic input data for the European Seismic Hazard Model 2020
Rapid estimation of seismic intensities by analyzing early aftershock sequences using the robust locally weighted regression program (LOWESS)
Sedimentary record of historic seismicity in a small, southern Oregon lake
A 2700-yr record of Cascadia megathrust and crustal/slab earthquakes from Upper and Lower Squaw Lakes, Oregon
Towards improving the spatial testability of aftershock forecast models
The Earthquake Risk Model of Switzerland ERM-CH23
Accounting for path and site effects in spatial ground-motion correlation models using Bayesian inference
Seismogenic potential and tsunami threat of the strike-slip Carboneras fault in the western Mediterranean from physics-based earthquake simulations
Earthquake hazard characterization by using entropy: application to northern Chilean earthquakes
Seismic risk scenarios for the residential buildings in the Sabana Centro province in Colombia
Looking for undocumented earthquake effects: a probabilistic analysis of Italian macroseismic data
Spatiotemporal seismicity pattern of the Taiwan orogen
A web-based GIS (web-GIS) database of the scientific articles on earthquake-triggered landslides
Evaluation of liquefaction triggering potential in Italy: a seismic-hazard-based approach
Earthquake vulnerability assessment of the built environment in the city of Srinagar, Kashmir Himalaya, using a geographic information system
Earthquake-induced landslides in Norway
PERL: a dataset of geotechnical, geophysical, and hydrogeological parameters for earthquake-induced hazards assessment in Terre del Reno (Emilia-Romagna, Italy)
Development of a seismic loss prediction model for residential buildings using machine learning – Ōtautahi / Christchurch, New Zealand
A non-extensive approach to probabilistic seismic hazard analysis
Inferring the depth and magnitude of pre-instrumental earthquakes from intensity attenuation curves
Morgan Vervoort, Katleen Wils, Kris Vanneste, Roberto Urrutia, Mario Pino, Catherine Kissel, Marc De Batist, and Maarten Van Daele
Nat. Hazards Earth Syst. Sci., 24, 3401–3421, https://doi.org/10.5194/nhess-24-3401-2024, https://doi.org/10.5194/nhess-24-3401-2024, 2024
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This study identifies a prehistoric earthquake around 4400 years ago near the city of Coyhaique (Aysén Region, Chilean Patagonia) and illustrates the potential seismic hazard in the region. We found deposits in lakes and a fjord that can be related to subaquatic and onshore landslides, all with a similar age, indicating that they were most likely caused by an earthquake. Through modeling we found that this was an earthquake of magnitude 6.3 to 7.0 on a fault near the city of Coyhaique.
Melody Philippon, Jean Roger, Jean-Frédéric Lebrun, Isabelle Thinon, Océane Foix, Stéphane Mazzotti, Marc-André Gutscher, Leny Montheil, and Jean-Jacques Cornée
Nat. Hazards Earth Syst. Sci., 24, 3129–3154, https://doi.org/10.5194/nhess-24-3129-2024, https://doi.org/10.5194/nhess-24-3129-2024, 2024
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Using novel geophysical datasets, we reassess the slip rate of the Morne Piton fault (Lesser Antilles) at 0.2 mm yr−1 by dividing by four previous estimations and thus increasing the earthquake time recurrence and lowering the associated hazard. We evaluate a plausible magnitude for a potential seismic event of Mw 6.5 ± 0.5. Our multi-segment tsunami model representative of the worst-case scenario gives an overview of tsunami generation if all the fault segments ruptured together.
Laurentiu Danciu, Domenico Giardini, Graeme Weatherill, Roberto Basili, Shyam Nandan, Andrea Rovida, Céline Beauval, Pierre-Yves Bard, Marco Pagani, Celso G. Reyes, Karin Sesetyan, Susana Vilanova, Fabrice Cotton, and Stefan Wiemer
Nat. Hazards Earth Syst. Sci., 24, 3049–3073, https://doi.org/10.5194/nhess-24-3049-2024, https://doi.org/10.5194/nhess-24-3049-2024, 2024
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The 2020 European Seismic Hazard Model (ESHM20) is the latest seismic hazard assessment update for the Euro-Mediterranean region. This state-of-the-art model delivers a broad range of hazard results, including hazard curves, maps, and uniform hazard spectra. ESHM20 provides two hazard maps as informative references in the next update of the European Seismic Design Code (CEN EC8), and it also provides a key input to the first earthquake risk model for Europe.
Hugo Rosero-Velásquez, Mauricio Monsalve, Juan Camilo Gómez Zapata, Elisa Ferrario, Alan Poulos, Juan Carlos de la Llera, and Daniel Straub
Nat. Hazards Earth Syst. Sci., 24, 2667–2687, https://doi.org/10.5194/nhess-24-2667-2024, https://doi.org/10.5194/nhess-24-2667-2024, 2024
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Seismic risk management uses reference earthquake scenarios, but the criteria for selecting them do not always consider consequences for exposed assets. Hence, we adopt a definition of representative scenarios associated with a return period and loss level to select such scenarios among a large set of possible earthquakes. We identify the scenarios for the residential-building stock and power supply in Valparaíso and Viña del Mar, Chile. The selected scenarios depend on the exposed assets.
Valerio Poggi, Stefano Parolai, Natalya Silacheva, Anatoly Ischuk, Kanatbek Abdrakhmatov, Zainalobudin Kobuliev, Vakhitkhan Ismailov, Roman Ibragimov, Japar Karaev, Paola Ceresa, and Paolo Bazzurro
Nat. Hazards Earth Syst. Sci., 24, 2597–2613, https://doi.org/10.5194/nhess-24-2597-2024, https://doi.org/10.5194/nhess-24-2597-2024, 2024
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As part of the Strengthening Financial Resilience and Accelerating Risk Reduction in Central Asia (SFRARR) programme, funded by the European Union in collaboration with the World Bank and GFDRR, a regionally consistent probabilistic multi-hazard and multi-asset risk assessment has been developed. This paper describes the preparation of the input datasets (earthquake catalogue and active-fault database) required for the implementation of the probabilistic seismic hazard model.
Konstantinos Trevlopoulos, Pierre Gehl, Caterina Negulescu, Helen Crowley, and Laurentiu Danciu
Nat. Hazards Earth Syst. Sci., 24, 2383–2401, https://doi.org/10.5194/nhess-24-2383-2024, https://doi.org/10.5194/nhess-24-2383-2024, 2024
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The models used to estimate the probability of exceeding a level of earthquake damage are essential to the reduction of disasters. These models consist of components that may be tested individually; however testing these types of models as a whole is challenging. Here, we use observations of damage caused by the 2019 Le Teil earthquake and estimations from other models to test components of seismic risk models.
Eugenio E. Vogel, Denisse Pastén, Gonzalo Saravia, Michel Aguilera, and Antonio Posadas
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2024-106, https://doi.org/10.5194/nhess-2024-106, 2024
Revised manuscript accepted for NHESS
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For the first time, an entropy analysis has been performed in Alaska, a seismic-rich region located in a subduction zone that shows non-trivial behavior: the subduction arc changes seismic activity from the eastern zone to the western zone, showing a decrease in this activity along subduction. This study shows how an entropy approach can help understand seismicity in subduction zones.
Graeme Weatherill, Sreeram Reddy Kotha, Laurentiu Danciu, Susana Vilanova, and Fabrice Cotton
Nat. Hazards Earth Syst. Sci., 24, 1795–1834, https://doi.org/10.5194/nhess-24-1795-2024, https://doi.org/10.5194/nhess-24-1795-2024, 2024
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The ground motion models (GMMs) selected for the 2020 European Seismic Hazard Model (ESHM20) and their uncertainties require adaptation to different tectonic environments. Using insights from new data, local experts and developments in the scientific literature, we further calibrate the ESHM20 GMM logic tree to capture previously unmodelled regional variation. We also propose a new scaled-backbone logic tree for application to Europe's subduction zones and the Vrancea deep seismic source.
Zhiwen Zhu, Zihan Jiang, Federico Accornero, and Alberto Carpinteri
EGUsphere, https://doi.org/10.5194/egusphere-2024-688, https://doi.org/10.5194/egusphere-2024-688, 2024
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1. The dense clusters of AE appear to anticipate the major seismic events. 2. AE has a strong correlation to seismic swarms occurring in surrounding areas. AE tends to regularly anticipates by approximately 17 hours both the considered seismic events. 3. The trends of b-value and natural-time variance can be used as seismic precursors.
Vera D'Amico, Francesco Visini, Andrea Rovida, Warner Marzocchi, and Carlo Meletti
Nat. Hazards Earth Syst. Sci., 24, 1401–1413, https://doi.org/10.5194/nhess-24-1401-2024, https://doi.org/10.5194/nhess-24-1401-2024, 2024
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We propose a scoring strategy to rank multiple models/branches of a probabilistic seismic hazard analysis (PSHA) model that could be useful to consider specific requests from stakeholders responsible for seismic risk reduction actions. In fact, applications of PSHA often require sampling a few hazard curves from the model. The procedure is introduced through an application aimed to score and rank the branches of a recent Italian PSHA model according to their fit with macroseismic intensity data.
Davide Scafidi, Alfio Viganò, Jacopo Boaga, Valeria Cascone, Simone Barani, Daniele Spallarossa, Gabriele Ferretti, Mauro Carli, and Giancarlo De Marchi
Nat. Hazards Earth Syst. Sci., 24, 1249–1260, https://doi.org/10.5194/nhess-24-1249-2024, https://doi.org/10.5194/nhess-24-1249-2024, 2024
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Our paper concerns the use of a dense network of low-cost seismic accelerometers in populated areas to achieve rapid and reliable estimation of exposure maps in Trentino (northeast Italy). These additional data, in conjunction with the automatic monitoring procedure, allow us to obtain dense measurements which only rely on actual recorded data, avoiding the use of ground motion prediction equations. This leads to a more reliable picture of the actual ground shaking.
Karina Loviknes, Fabrice Cotton, and Graeme Weatherill
Nat. Hazards Earth Syst. Sci., 24, 1223–1247, https://doi.org/10.5194/nhess-24-1223-2024, https://doi.org/10.5194/nhess-24-1223-2024, 2024
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Earthquake ground shaking can be strongly affected by local geology and is often amplified by soft sediments. In this study, we introduce a global geomorphological model for sediment thickness as a protentional parameter for predicting this site amplification. The results show that including geology and geomorphology in site-amplification predictions adds important value and that global or regional models for sediment thickness from fields beyond engineering seismology are worth considering.
Khelly Shan Sta. Rita, Sotiris Valkaniotis, and Alfredo Mahar Francisco Lagmay
Nat. Hazards Earth Syst. Sci., 24, 1135–1161, https://doi.org/10.5194/nhess-24-1135-2024, https://doi.org/10.5194/nhess-24-1135-2024, 2024
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The ground movement and rupture produced by the 2020 Masbate earthquake in the Philippines were studied using satellite data. We highlight the importance of the complementary use of optical and radar datasets. The slip measurements and field observations helped improve our understanding of the seismotectonics of the region, which is critical for seismic hazard studies.
Qing Wu, Guijuan Lai, Jian Wu, and Jinmeng Bi
Nat. Hazards Earth Syst. Sci., 24, 1017–1033, https://doi.org/10.5194/nhess-24-1017-2024, https://doi.org/10.5194/nhess-24-1017-2024, 2024
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Aftershocks are typically ignored for traditional probabilistic seismic hazard analyses, which underestimate the seismic hazard to some extent and may cause potential risks. A probabilistic seismic hazard analysis based on the Monte Carlo method was combined with the Omi–Reasenberg–Jones model to systematically study how aftershocks impact seismic hazard analyses. The influence of aftershocks on probabilistic seismic hazard analysis can exceed 50 %.
Lixin Wu, Xiao Wang, Yuan Qi, Jingchen Lu, and Wenfei Mao
Nat. Hazards Earth Syst. Sci., 24, 773–789, https://doi.org/10.5194/nhess-24-773-2024, https://doi.org/10.5194/nhess-24-773-2024, 2024
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The atmospheric electric field (AEF) is the bridge connecting the surface charges and atmospheric particle changes before an earthquake, which is essential for the study of the coupling process between the coversphere and atmosphere caused by earthquakes. This study discovers AEF anomalies before the Luding earthquake in 2022 and clarifies the relationship between the surface changes and atmosphere changes possibly caused by the earthquake.
Polona Zupančič, Barbara Šket Motnikar, Michele M. C. Carafa, Petra Jamšek Rupnik, Mladen Živčić, Vanja Kastelic, Gregor Rajh, Martina Čarman, Jure Atanackov, and Andrej Gosar
Nat. Hazards Earth Syst. Sci., 24, 651–672, https://doi.org/10.5194/nhess-24-651-2024, https://doi.org/10.5194/nhess-24-651-2024, 2024
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We considered two parameters that affect seismic hazard assessment in Slovenia. The first parameter we determined is the thickness of the lithosphere's section where earthquakes are generated. The second parameter is the activity of each fault, which is expressed by its average displacement per year (slip rate). Since the slip rate can be either seismic or aseismic, we estimated both components. This analysis was based on geological and seismological data and was validated through comparisons.
Maren Böse, Laurentiu Danciu, Athanasios Papadopoulos, John Clinton, Carlo Cauzzi, Irina Dallo, Leila Mizrahi, Tobias Diehl, Paolo Bergamo, Yves Reuland, Andreas Fichtner, Philippe Roth, Florian Haslinger, Frédérick Massin, Nadja Valenzuela, Nikola Blagojević, Lukas Bodenmann, Eleni Chatzi, Donat Fäh, Franziska Glueer, Marta Han, Lukas Heiniger, Paulina Janusz, Dario Jozinović, Philipp Kästli, Federica Lanza, Timothy Lee, Panagiotis Martakis, Michèle Marti, Men-Andrin Meier, Banu Mena Cabrera, Maria Mesimeri, Anne Obermann, Pilar Sanchez-Pastor, Luca Scarabello, Nicolas Schmid, Anastasiia Shynkarenko, Bozidar Stojadinović, Domenico Giardini, and Stefan Wiemer
Nat. Hazards Earth Syst. Sci., 24, 583–607, https://doi.org/10.5194/nhess-24-583-2024, https://doi.org/10.5194/nhess-24-583-2024, 2024
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Seismic hazard and risk are time dependent as seismicity is clustered and exposure can change rapidly. We are developing an interdisciplinary dynamic earthquake risk framework for advancing earthquake risk mitigation in Switzerland. This includes various earthquake risk products and services, such as operational earthquake forecasting and early warning. Standardisation and harmonisation into seamless solutions that access the same databases, workflows, and software are a crucial component.
Rimali Mitra, Hajime Naruse, and Tomoya Abe
Nat. Hazards Earth Syst. Sci., 24, 429–444, https://doi.org/10.5194/nhess-24-429-2024, https://doi.org/10.5194/nhess-24-429-2024, 2024
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This study estimates the behavior of the 2011 Tohoku-oki tsunami from its deposit distributed in the Joban coastal area. In this study, the flow characteristics of the tsunami were reconstructed using the DNN (deep neural network) inverse model, suggesting that the tsunami inundation occurred in the very high-velocity condition.
Sedat İnan, Hasan Çetin, and Nurettin Yakupoğlu
Nat. Hazards Earth Syst. Sci., 24, 397–409, https://doi.org/10.5194/nhess-24-397-2024, https://doi.org/10.5194/nhess-24-397-2024, 2024
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Two devastating earthquakes, Mw 7.7 and Mw 7.6, occurred in Türkiye on 6 February 2023. We obtained commercially bottled waters from two springs, 100 km from the epicenter of Mw 7.7. Samples of the first spring emanating from fault zone in hard rocks showed positive anomalies in major ions lasting for 6 months before the earthquake. Samples from the second spring accumulated in an alluvium deposit showed no anomalies. We show that pre-earthquake anomalies are geologically site-dependent.
Sylvain Michel, Clara Duverger, Laurent Bollinger, Jorge Jara, and Romain Jolivet
Nat. Hazards Earth Syst. Sci., 24, 163–177, https://doi.org/10.5194/nhess-24-163-2024, https://doi.org/10.5194/nhess-24-163-2024, 2024
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The Upper Rhine Graben, located in France and Germany, is bordered by north–south-trending faults, posing a potential threat to dense population and infrastructures on the Alsace plain. We build upon previous seismic hazard studies of the graben by exploring uncertainties in greater detail, revisiting a number of assumptions. There is a 99 % probability that a maximum-magnitude earthquake would be below 7.3 if assuming a purely dip-slip mechanism or below 7.6 if assuming a strike-slip one.
Edlira Xhafaj, Chung-Han Chan, and Kuo-Fong Ma
Nat. Hazards Earth Syst. Sci., 24, 109–119, https://doi.org/10.5194/nhess-24-109-2024, https://doi.org/10.5194/nhess-24-109-2024, 2024
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Our study introduces new earthquake forecasting models for Albania, aiming to map out future seismic hazards. By analysing earthquakes from 1960 to 2006, we have developed models that predict where activity is most likely to occur, highlighting the western coast and southern regions as high-hazard zones. Our validation process confirms these models are effective tools for anticipating seismic events, offering valuable insights for earthquake preparedness and hazard assessment efforts.
Himanshu Agrawal and John McCloskey
EGUsphere, https://doi.org/10.22541/essoar.169504548.82107207/v1, https://doi.org/10.22541/essoar.169504548.82107207/v1, 2024
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Rapidly growing cities in earthquake-prone Global South regions lack seismic event records, hindering accurate ground motion predictions for hazard assessment. Our study shows that even with these limitations, it is possible to generate reasonable predictions of the spatial variability in expected ground motions using high-resolution local geological information and simulation-based methods. We emphasize that substantial investments in the measurement of subsurface properties can prove valuable.
Elena F. Manea, Laurentiu Danciu, Carmen O. Cioflan, Dragos Toma-Danila, and Matt Gerstenberger
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2023-232, https://doi.org/10.5194/nhess-2023-232, 2024
Revised manuscript under review for NHESS
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We test and evaluate the results of the 2020 European Seismic Hazard Model (ESHM20; Danciu et al., 2021) against observations spamming over a few centuries at twelve cities in Romania. The full distribution of the hazard curves at the given location was considered, and the testing was done for two relevant peak ground acceleration (PGA) values. Our analysis suggests that the observed exceedance rates for the selected PGA levels are consistent with ESHM20 estimates.
Niranjan Joshi, Björn Lund, and Roland Roberts
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2023-213, https://doi.org/10.5194/nhess-2023-213, 2023
Revised manuscript accepted for NHESS
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Few large earthquakes and low occurrence rates makes seismic hazard assessment of Sweden a challenging task. Since 2000, expansion of the seismic network has improved the quality and quantity of the data recorded. We use this new data to estimate the Swedish seismic hazard using probabilistic methods. We find that hazard was previously underestimated in the north, which we find to have the highest hazard in Sweden with mean peak ground acceleration of up to 0.05 g for a 475 year return period.
Franz Livio, Maria Francesca Ferrario, Elisa Martinelli, Sahra Talamo, Silvia Cercatillo, and Alessandro Maria Michetti
Nat. Hazards Earth Syst. Sci., 23, 3407–3424, https://doi.org/10.5194/nhess-23-3407-2023, https://doi.org/10.5194/nhess-23-3407-2023, 2023
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Here we document the occurrence of an historical earthquake that occurred in the European western Southern Alps in the sixth century CE. Analysis of the effects due to earthquake shaking in the city of Como (N Italy) and a comparison with dated offshore landslides in the Alpine lakes allowed us to make an inference about the possible magnitude and the location of the seismic source for this event.
Graeme Weatherill, Fabrice Cotton, Guillaume Daniel, Irmela Zentner, Pablo Iturrieta, and Christian Bosse
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2023-98, https://doi.org/10.5194/nhess-2023-98, 2023
Revised manuscript accepted for NHESS
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New generations of seismic hazard models are developed with sophisticated approaches to quantify uncertainties in our knowledge of earthquake process. To understand why and how recent state-of-the-art seismic hazard models for France, Germany and Europe differ despite similar underlying assumptions, we present a systematic approach to investigate model-to-model differences and to quantify and visualise them while accounting for their respective uncertainties.
Simone Francesco Fornasari, Deniz Ertuncay, and Giovanni Costa
Nat. Hazards Earth Syst. Sci., 23, 3219–3234, https://doi.org/10.5194/nhess-23-3219-2023, https://doi.org/10.5194/nhess-23-3219-2023, 2023
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We analysed the background seismic noise for the Italian strong motion network by developing the Italian accelerometric low- and high-noise models. Spatial and temporal variations of the noise levels have been analysed. Several stations located near urban areas are affected by human activities, with high noise levels in the low periods. Our results provide an overview of the background noise of the strong motion network and can be used as a station selection criterion for future research.
Subash Ghimire, Philippe Guéguen, Adrien Pothon, and Danijel Schorlemmer
Nat. Hazards Earth Syst. Sci., 23, 3199–3218, https://doi.org/10.5194/nhess-23-3199-2023, https://doi.org/10.5194/nhess-23-3199-2023, 2023
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This study explores the efficacy of several machine learning models for damage characterization, trained and tested on the Database of Observed Damage (DaDO) for Italian earthquakes. Reasonable damage prediction effectiveness (68 % accuracy) is observed, particularly when considering basic structural features and grouping the damage according to the traffic-light-based system used during the post-disaster period (green, yellow, and red), showing higher relevancy for rapid damage prediction.
Ekbal Hussain, Endra Gunawan, Nuraini Rahma Hanifa, and Qori'atu Zahro
Nat. Hazards Earth Syst. Sci., 23, 3185–3197, https://doi.org/10.5194/nhess-23-3185-2023, https://doi.org/10.5194/nhess-23-3185-2023, 2023
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The earthquake potential of the Lembang Fault, located near the city of Bandung in West Java, Indonesia, is poorly understood. Bandung has a population of over 8 million people. We used satellite data to estimate the energy storage on the fault and calculate the likely size of potential future earthquakes. We use simulations to show that 1.9–2.7 million people would be exposed to high levels of ground shaking in the event of a major earthquake on the fault.
Valerio Poggi, Stefano Parolai, Natalya Silacheva, Anatoly Ischuk, Kanatbek Abdrakhmatov, Zainalobudin Kobuliev, Vakhitkhan Ismailov, Roman Ibragimov, Japar Karayev, Paola Ceresa, Marco Santulin, and Paolo Bazzurro
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2023-132, https://doi.org/10.5194/nhess-2023-132, 2023
Revised manuscript accepted for NHESS
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A regionally consistent probabilistic risk assessment for multiple hazards and assets was recently developed as part of the "Strengthening Financial Resilience and Accelerating Risk Reduction in Central Asia" (SFRARR) program, promoted by the European Union in collaboration with the World Bank and GFDRR. This paper describes the preparation of the source model and presents the main results of the probabilistic earthquake model for the Central Asian countries.
Roberto Basili, Laurentiu Danciu, Céline Beauval, Karin Sesetyan, Susana Pires Vilanova, Shota Adamia, Pierre Arroucau, Jure Atanackov, Stephane Baize, Carolina Canora, Riccardo Caputo, Michele Matteo Cosimo Carafa, Edward Marc Cushing, Susana Custódio, Mine Betul Demircioglu Tumsa, João C. Duarte, Athanassios Ganas, Julián García-Mayordomo, Laura Gómez de la Peña, Eulàlia Gràcia, Petra Jamšek Rupnik, Hervé Jomard, Vanja Kastelic, Francesco Emanuele Maesano, Raquel Martín-Banda, Sara Martínez-Loriente, Marta Neres, Hector Perea, Barbara Šket Motnikar, Mara Monica Tiberti, Nino Tsereteli, Varvara Tsironi, Roberto Vallone, Kris Vanneste, Polona Zupančič, and Domenico Giardini
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2023-118, https://doi.org/10.5194/nhess-2023-118, 2023
Revised manuscript accepted for NHESS
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This study presents the European Fault-Source Model 2020 (EFSM20), a dataset of 1,248 geologic crustal faults and four subduction systems, each having the necessary parameters to forecast long-term earthquake occurrences in the European continent. This dataset constituted one of the main inputs for the recently released European Seismic Hazard Model 2020, a key instrument to mitigate seismic risk in Europe. EFSM20 adopts recognized open-standard formats, and it is openly accessible and reusable.
Huaiqun Zhao, Wenkai Chen, Can Zhang, and Dengjie Kang
Nat. Hazards Earth Syst. Sci., 23, 3031–3050, https://doi.org/10.5194/nhess-23-3031-2023, https://doi.org/10.5194/nhess-23-3031-2023, 2023
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Early emergency response requires improving the utilization value of the data available in the early post-earthquake period. We proposed a method for assessing seismic intensities by analyzing early aftershock sequences using the robust locally weighted regression program. The seismic intensity map evaluated by the method can reflect the range of the hardest-hit areas and the spatial distribution of the possible property damage and casualties caused by the earthquake.
Ann Elizabeth Morey, Mark D. Shapley, Daniel G. Gavin, Alan R. Nelson, and Chris Goldfinger
EGUsphere, https://doi.org/10.21203/rs.3.rs-1631354/v2, https://doi.org/10.21203/rs.3.rs-1631354/v2, 2023
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Disturbance events from historic sediments from a small lake in Oregon were compared to known events to determine if Cascadia earthquakes are uniquely identifiable. Sedimentological methods and geochemical provenance data identify a deposit likely from the most recent Cascadia earthquake (which occurred in 1700), another type of earthquake deposit, and flood deposits, suggesting that small lakes are good recorders of megathrust earthquakes. New methods developed hold promise for other lakes.
Ann Elizabeth Morey and Chris Goldfinger
EGUsphere, https://doi.org/10.21203/rs.3.rs-2277419/v2, https://doi.org/10.21203/rs.3.rs-2277419/v2, 2023
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This study uses the characteristics from a deposit attributed to the 1700 CE Cascadia earthquake to identify other subduction earthquake deposits in sediments from two lakes located near the California/Oregon border. Seven deposits were identified in these records and an age-depth model suggests that these correlate in time to the largest Cascadia earthquakes preserved in the offshore record suggesting that inland lakes can be good recorders of Cascadia earthquakes.
Asim M. Khawaja, Behnam Maleki Asayesh, Sebastian Hainzl, and Danijel Schorlemmer
Nat. Hazards Earth Syst. Sci., 23, 2683–2696, https://doi.org/10.5194/nhess-23-2683-2023, https://doi.org/10.5194/nhess-23-2683-2023, 2023
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Testing of earthquake forecasts is important for model verification. Forecasts are usually spatially discretized with many equal-sized grid cells, but often few earthquakes are available for evaluation, leading to meaningless tests. Here, we propose solutions to improve the testability of earthquake forecasts and give a minimum ratio between the number of earthquakes and spatial cells for significant tests. We show applications of the proposed technique for synthetic and real case studies.
Athanasios N. Papadopoulos, Philippe Roth, Laurentiu Danciu, Paolo Bergamo, Francesco Panzera, Donat Fäh, Carlo Cauzzi, Blaise Duvernay, Alireza Khodaverdian, Pierino Lestuzzi, Ömer Odabaşi, Ettore Fagà, Paolo Bazzurro, Michèle Marti, Nadja Valenzuela, Irina Dallo, Nicolas Schmid, Philip Kästli, Florian Haslinger, and Stefan Wiemer
EGUsphere, https://doi.org/10.5194/egusphere-2023-1504, https://doi.org/10.5194/egusphere-2023-1504, 2023
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The Earthquake Risk Model of Switzerland (ERM-CH23), released in early 2023, is the culmination of a multidisciplinary effort aiming to achieve, for the first time, a comprehensive assessment of the potential consequences of earthquakes on the Swiss building stock and population. ERM-CH23 provides risk estimates for various impact metrics, ranging from economic loss as a result of damage to buildings and their contents, to human losses, such as deaths, injuries and displaced population.
Lukas Bodenmann, Jack W. Baker, and Božidar Stojadinović
Nat. Hazards Earth Syst. Sci., 23, 2387–2402, https://doi.org/10.5194/nhess-23-2387-2023, https://doi.org/10.5194/nhess-23-2387-2023, 2023
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Understanding spatial patterns in earthquake-induced ground motions is key for assessing the seismic risk of distributed infrastructure systems. To study such patterns, we propose a novel model that accounts for spatial proximity, as well as site and path effects, and estimate its parameters from past earthquake data by explicitly quantifying the inherent uncertainties.
José A. Álvarez-Gómez, Paula Herrero-Barbero, and José J. Martínez-Díaz
Nat. Hazards Earth Syst. Sci., 23, 2031–2052, https://doi.org/10.5194/nhess-23-2031-2023, https://doi.org/10.5194/nhess-23-2031-2023, 2023
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The strike-slip Carboneras fault is one of the largest sources in the Alboran Sea, with it being one of the faster faults in the eastern Betics. The dimensions and location of the Carboneras fault imply a high seismic and tsunami threat. In this work, we present tsunami simulations from sources generated with physics-based earthquake simulators. We show that the Carboneras fault has the capacity to generate locally damaging tsunamis with inter-event times between 2000 and 6000 years.
Antonio Posadas, Denisse Pasten, Eugenio E. Vogel, and Gonzalo Saravia
Nat. Hazards Earth Syst. Sci., 23, 1911–1920, https://doi.org/10.5194/nhess-23-1911-2023, https://doi.org/10.5194/nhess-23-1911-2023, 2023
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In this paper we understand an earthquake from a thermodynamics point of view as an irreversible transition; then it must suppose an increase in entropy. We use > 100 000 earthquakes in northern Chile to test the theory that Shannon entropy, H, is an indicator of the equilibrium state. Using variation in H, we were able to detect major earthquakes and their foreshocks and aftershocks, including the 2007 Mw 7.8 Tocopilla earthquake and 2014 Mw 8.1 Iquique earthquake.
Dirsa Feliciano, Orlando Arroyo, Tamara Cabrera, Diana Contreras, Jairo Andrés Valcárcel Torres, and Juan Camilo Gómez Zapata
Nat. Hazards Earth Syst. Sci., 23, 1863–1890, https://doi.org/10.5194/nhess-23-1863-2023, https://doi.org/10.5194/nhess-23-1863-2023, 2023
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This article presents the number of damaged buildings and estimates the economic losses from a set of earthquakes in Sabana Centro, a region of 11 towns in Colombia.
Andrea Antonucci, Andrea Rovida, Vera D'Amico, and Dario Albarello
Nat. Hazards Earth Syst. Sci., 23, 1805–1816, https://doi.org/10.5194/nhess-23-1805-2023, https://doi.org/10.5194/nhess-23-1805-2023, 2023
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The earthquake effects undocumented at 228 Italian localities were calculated through a probabilistic approach starting from the values obtained through the use of an intensity prediction equation, taking into account the intensity data documented at close localities for a given earthquake. The results showed some geographical dependencies and correlations with the intensity levels investigated.
Yi-Ying Wen, Chien-Chih Chen, Strong Wen, and Wei-Tsen Lu
Nat. Hazards Earth Syst. Sci., 23, 1835–1846, https://doi.org/10.5194/nhess-23-1835-2023, https://doi.org/10.5194/nhess-23-1835-2023, 2023
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Knowing the spatiotemporal seismicity patterns prior to impending large earthquakes might help earthquake hazard assessment. Several recent moderate earthquakes occurred in the various regions of Taiwan, which help to further investigate the spatiotemporal seismic pattern related to the regional tectonic stress. We should pay attention when a seismicity decrease of 2.5 < M < 4.5 events around the southern Central Range or an accelerating seismicity of 3 < M < 5 events appears in central Taiwan.
Luca Schilirò, Mauro Rossi, Federica Polpetta, Federica Fiorucci, Carolina Fortunato, and Paola Reichenbach
Nat. Hazards Earth Syst. Sci., 23, 1789–1804, https://doi.org/10.5194/nhess-23-1789-2023, https://doi.org/10.5194/nhess-23-1789-2023, 2023
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We present a database of the main scientific articles published on earthquake-triggered landslides in the last 4 decades. To enhance data viewing, the articles were catalogued into a web-based GIS, which was specifically designed to show different types of information, such as bibliometric information, the relevant topic and sub-topic category (or categories), and earthquake(s) addressed. Such information can be useful to obtain a general overview of the topic, especially for a broad readership.
Simone Barani, Gabriele Ferretti, and Davide Scafidi
Nat. Hazards Earth Syst. Sci., 23, 1685–1698, https://doi.org/10.5194/nhess-23-1685-2023, https://doi.org/10.5194/nhess-23-1685-2023, 2023
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In the present study, we analyze ground-motion hazard maps and hazard disaggregation in order to define areas in Italy where liquefaction triggering due to seismic activity can not be excluded. The final result is a screening map for all of Italy that classifies sites in terms of liquefaction triggering potential according to their seismic hazard level. The map and the associated data are freely accessible at the following web address: www.distav.unige.it/rsni/milq.php.
Midhat Fayaz, Shakil A. Romshoo, Irfan Rashid, and Rakesh Chandra
Nat. Hazards Earth Syst. Sci., 23, 1593–1611, https://doi.org/10.5194/nhess-23-1593-2023, https://doi.org/10.5194/nhess-23-1593-2023, 2023
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Earthquakes cause immense loss of lives and damage to properties, particularly in major urban centres. The city of Srinagar, which houses around 1.5 million people, is susceptible to high seismic hazards due to its peculiar geological setting, urban setting, demographic profile, and tectonic setting. Keeping in view all of these factors, the present study investigates the earthquake vulnerability of buildings in Srinagar, an urban city in the northwestern Himalayas, India.
Mathilde B. Sørensen, Torbjørn Haga, and Atle Nesje
Nat. Hazards Earth Syst. Sci., 23, 1577–1592, https://doi.org/10.5194/nhess-23-1577-2023, https://doi.org/10.5194/nhess-23-1577-2023, 2023
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Most Norwegian landslides are triggered by rain or snowmelt, and earthquakes have not been considered a relevant trigger mechanism even though some cases have been reported. Here we systematically search historical documents and databases and find 22 landslides induced by eight large Norwegian earthquakes. The Norwegian earthquakes induce landslides at distances and over areas that are much larger than those found for global datasets.
Chiara Varone, Gianluca Carbone, Anna Baris, Maria Chiara Caciolli, Stefania Fabozzi, Carolina Fortunato, Iolanda Gaudiosi, Silvia Giallini, Marco Mancini, Luca Paolella, Maurizio Simionato, Pietro Sirianni, Rose Line Spacagna, Francesco Stigliano, Daniel Tentori, Luca Martelli, Giuseppe Modoni, and Massimiliano Moscatelli
Nat. Hazards Earth Syst. Sci., 23, 1371–1382, https://doi.org/10.5194/nhess-23-1371-2023, https://doi.org/10.5194/nhess-23-1371-2023, 2023
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In 2012, Italy was struck by a seismic crisis characterized by two main shocks and relevant liquefaction events. Terre del Reno is one of the municipalities that experienced the most extensive liquefaction effects; thus it was chosen as case study for a project devoted to defining a new methodology to assess the liquefaction susceptibility. In this framework, about 1800 geotechnical, geophysical, and hydrogeological investigations were collected and stored in the publicly available PERL dataset.
Samuel Roeslin, Quincy Ma, Pavan Chigullapally, Joerg Wicker, and Liam Wotherspoon
Nat. Hazards Earth Syst. Sci., 23, 1207–1226, https://doi.org/10.5194/nhess-23-1207-2023, https://doi.org/10.5194/nhess-23-1207-2023, 2023
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This paper presents a new framework for the rapid seismic loss prediction for residential buildings in Christchurch, New Zealand. The initial model was trained on insurance claims from the Canterbury earthquake sequence. Data science techniques, geospatial tools, and machine learning were used to develop the prediction model, which also delivered useful insights. The model can rapidly be updated with data from new earthquakes. It can then be applied to predict building loss in Christchurch.
Sasan Motaghed, Mozhgan Khazaee, Nasrollah Eftekhari, and Mohammad Mohammadi
Nat. Hazards Earth Syst. Sci., 23, 1117–1124, https://doi.org/10.5194/nhess-23-1117-2023, https://doi.org/10.5194/nhess-23-1117-2023, 2023
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We modify the probabilistic seismic hazard analysis (PSHA) formulation by replacing the Gutenberg–Richter power law with the SCP (Sotolongo-Costa and Posadas) non-extensive model for earthquake size distribution and call it NEPSHA. The proposed method (NEPSHA) is implemented in the Tehran region, and the results are compared with the classic PSHA method. The hazard curves show that NEPSHA gives a higher hazard, especially in the range of practical return periods.
Paola Sbarra, Pierfrancesco Burrato, Valerio De Rubeis, Patrizia Tosi, Gianluca Valensise, Roberto Vallone, and Paola Vannoli
Nat. Hazards Earth Syst. Sci., 23, 1007–1028, https://doi.org/10.5194/nhess-23-1007-2023, https://doi.org/10.5194/nhess-23-1007-2023, 2023
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Earthquakes are fundamental for understanding how the earth works and for assessing seismic risk. We can easily measure the magnitude and depth of today's earthquakes, but can we also do it for pre-instrumental ones? We did it by analyzing the decay of earthquake effects (on buildings, people, and objects) with epicentral distance. Our results may help derive data that would be impossible to obtain otherwise, for any country where the earthquake history extends for centuries, such as Italy.
Cited articles
Avouac, J.-P., Meng, L., Wei, S., Wang, T., and Ampuero, J.-P.: Lower edge of
locked Main Himalayan Thrust unzipped by the 2015 Gorkha earthquake, Nat.
Geosci., 8, 708–711, https://doi.org/10.1038/ngeo2518, 2015.
Banerjee, P., Pollitz, F., Nagarajan, B., and Bürgmann, R.: Coseismic
Slip Distributions of the 26 December 2004 Sumatra-Andaman and 28 March 2005
Nias Earthquakes from gps Static Offsets, B. Seismol. Soc. Am., 97, S86–S102, https://doi.org/10.1785/0120050609, 2007.
Bautista, B. C., Bautista, M. L. P., Oike, K., Wu, F. T., and Punongbayan, R.
S.: A new insight on the geometry of subducting slabs in Northern Luzon,
Philippines, Tectonophysics, 339, 279–310, https://doi.org/10.1016/S0040-1951(01)00120-2, 2001.
Bautista, M. L. P. of Volcanology, P. I. and Seismology: Philippine Tsunamis and Seiches, 1589 to 2012, Department of Science and Technology, Philippine Institute of Volcanology and Seismology, available at:
https://books.google.com.sg/books?id=OHibnQAACAAJ (last access: 9 April 2019), 2012.
Bell, R., Holden, C., Power, W., Wang, X., and Downes, G.: Hikurangi margin
tsunami earthquake generated by slow seismic rupture over a subducted seamount, Earth Planet. Sc. Lett., 397, 1–9, https://doi.org/10.1016/j.epsl.2014.04.005, 2014.
Bilek, S. L. and Lay, T.: Subduction zone megathrust earthquakes, Geosphere,
14, 1468–1500, https://doi.org/10.1130/GES01608.1, 2018.
Bletery, Q., Thomas, A. M., Rempel, A. W., Karlstrom, L., Sladen, A., and
De Barros, L.: Mega-earthquakes rupture flat megathrusts, Science, 354, 1027–1031, https://doi.org/10.1126/science.aag0482, 2016.
Chlieh, M., Avouac, J. P., Hjorleifsdottir, V., Song, T. R. A., Ji, C., Sieh, K., Sladen, A., Hebert, H., Prawirodirdjo, L., Bock, Y., and Galetzka, J.: Coseismic slip and afterslip of the great Mw 9.15 Sumatra-Andaman earthquake of 2004, B. Seismol. Soc. Am., 97, S152–S173, https://doi.org/10.1785/0120050631, 2007.
Chlieh, M., Avouac, J. P., Sieh, K., Natawidjaja, D. H., and Galetzka, J.:
Heterogeneous coupling of the Sumatran megathrust constrained by geodetic and paleogeodetic measurements, J. Geophys. Res., 113, 1–31, https://doi.org/10.1029/2007JB004981, 2008.
Cifuentes, I. L.: The 1960 Chilean earthquakes, J. Geophys. Res.-Solid, 94, 665–680, https://doi.org/10.1029/JB094iB01p00665, 1989.
Duan, B.: Dynamic rupture of the 2011 Mw 9.0 Tohoku-Oki earthquake: Roles of
a possible subducting seamount, J. Geophys. Res.-Solid, 117, B05311, https://doi.org/10.1029/2011JB009124, 2012.
Fan, J., Zhao, D., and Dong, D.: Subduction of a buoyant plateau at the
Manila Trench: Tomographic evidence and geodynamic implications, Geochem. Geophy. Geosy., 17, 571–586, https://doi.org/10.1002/2015GC006201, 2016.
Furlong, K. P., Lay, T., and Ammon, C. J.: A Great Earthquake Rupture Across
a Rapidly Evolving Three-Plate Boundary, Science, 324, 226–229, https://doi.org/10.1126/science.1167476, 2009.
Gao, J., Wu, S., yao, Y., Chen, C., Song, T., Wang, J., Sun, J., Zhang, H., Ma, B., and Yangbing, X.: Tectonic deformation and fine structure of the
frontal accretionary wedge,northern Manila subduction zone, Chinese J.
Geophys. Chinese Ed., 61, 2845–2858, https://doi.org/10.6038/cjg2018L0461, 2018.
Grezio, A., Babeyko, A., Baptista, M. A., Behrens, J., Costa, A., Davies, G., Geist, E. L., Glimsdal, S., González, F. I., Griffin, J., Harbitz, C. B., LeVeque, R. J., Lorito, S., Løvholt, F., Omira, R., Mueller, C., Paris, R., Parsons, T., Polet, J., Power, W., Selva, J., Sørensen, M. B., and Thio, H. K.: Probabilistic Tsunami Hazard Analysis: Multiple Sources and
Global Applications, Rev. Geophys., 55, 1158–1198, https://doi.org/10.1002/2017RG000579, 2017.
Hayes, G. P., Wald, D. J., and Johnson, R. L.: Slab1.0: A three-dimensional
model of global subduction zone geometries, J. Geophys. Res.-Solid, 117, B01302, https://doi.org/10.1029/2011JB008524, 2012.
Heuret, A., Conrad, C. P., Funiciello, F., Lallemand, S., and Sandri, L.:
Relation between subduction megathrust earthquakes, trench sediment thickness and upper plate strain, Geophys. Res. Lett., 39, L05304, https://doi.org/10.1029/2011GL050712, 2012.
Hippchen, S. and Hyndman, R. D.: Thermal and structural models of the Sumatra subduction zone: Implications for the megathrust seismogenic zone, J. Geophys. Res.-Solid, 113, B12103, https://doi.org/10.1029/2008JB005698, 2008.
Hong Nguyen, P., Cong Bui, Q., Ha Vu, P., and The Pham, T.: Scenario-based
tsunami hazard assessment for the coast of Vietnam from the Manila Trench
source, Phys. Earth Planet. Inter., 236, 95–108, https://doi.org/10.1016/j.pepi.2014.07.003, 2014.
Hsu, Y.-J., Yu, S.-B., Simons, M., Kuo, L.-C., and Chen, H.-Y.: Interseismic
crustal deformation in the Taiwan plate boundary zone revealed by GPS
observations, seismicity, and earthquake focal mechanisms, Tectonophysics,
479, 4–18, https://doi.org/10.1016/j.tecto.2008.11.016, 2009.
Hsu, Y.-J., Yu, S.-B., Song, T.-R. A., and Bacolcol, T.: Plate coupling along
the Manila subduction zone between Taiwan and northern Luzon, J. Asian Earth
Sci., 51, 98–108, https://doi.org/10.1016/j.jseaes.2012.01.005, 2012.
Hsu, Y.-J., Yu, S.-B., Loveless, J. P., Bacolcol, T., Solidum, R., Luis Jr.,
A., Pelicano, A., and Woessner, J.: Interseismic deformation and moment deficit along the Manila subduction zone and the Philippine Fault system, J.
Geophys. Res.-Solid, 121, 7639–7665, https://doi.org/10.1002/2016JB013082, 2016.
Hyndman, R. D. and Wang, K.: Thermal constraints on the zone of major thrust
earthquake failure: the Cascadia Subduction Zone, J. Geophys. Res., 98, 2039–2060, https://doi.org/10.1029/92JB02279, 1993.
Johnson, J. M. and Satake, K.: Asperity Distribution of the 1952 Great Kamchatka Earthquake and its Relation to Future Earthquake Potential in
Kamchatka, in: Seismogenic and Tsunamigenic Processes in Shallow Subduction
Zones, edited by: Sauber, J. and Dmowska, R., Birkhäuser, Basel, 541–553, 1999.
Kagan, Y. Y. and Jackson, D. D.: Tohoku Earthquake: A Surprise? Tohoku
Earthquake: A Surprise?, B. Seismol. Soc. Am., 103, 1181–1194, https://doi.org/10.1785/0120120110, 2013.
Kanamori, H.: Re-examination of the earth's free oxcillations excited by the
Kamchatka earthquake of November 4, 1952, Phys. Earth Planet. Inter., 11,
216–226, 1976.
Kanamori, H.: Lessons from the 2004 Sumatra-Andaman earthquake, Philos. T. Roy. Soc. A, 364, 1927–1945, https://doi.org/10.1098/rsta.2006.1806, 2006.
Koketsu, K., Yokota, Y., Nishimura, N., Yagi, Y., Miyazaki, S., Satake, K.,
Fujii, Y., Miyake, H., Sakai, S., Yamanaka, Y., and Okada, T.: A unified
source model for the 2011 Tohoku earthquake, Earth Planet. Sc. Lett., 310, 480–487, https://doi.org/10.1016/j.epsl.2011.09.009, 2011.
Konca, A. O., Avouac, J.-P., Sladen, A., Meltzner, A. J., Sieh, K., Fang, P., Li, Z., Galetzka, J., Genrich, J., Chlieh, M., Natawidjaja, D. H., Bock, Y., Fielding, E. J., Ji, C., and Helmberger, D. V: Partial rupture of a locked patch of the Sumatra megathrust during the 2007 earthquake sequence, Nature, 456, 631–635, https://doi.org/10.1038/nature07572, 2008.
Koyama, J., Yoshizawa, K., Yomogida, K., and Tsuzuki, M.: Variability of
megathrust earthquakes in the world revealed by the 2011 Tohoku-oki
Earthquake, Earth Planets Space, 64, 129–146, https://doi.org/10.5047/eps.2012.04.011, 2013.
Kumagai, H., Pulido, N., Fukuyama, E., and Aoi, S.: Strong localized asperity
of the 2011 Tohoku-Oki earthquake, Japan, Earth Planets Space, 64, 649–654, https://doi.org/10.5047/eps.2012.01.004, 2012.
Lau, A. Y. A., Switzer, A. D., DomineyHowes, D., Aitchison, J. C., and Zong,
Y.: Written records of historical tsunamis in the northeastern South China
Sea-challenges associated with developing a new integrated database, Nat.
Hazards Earth Syst. Sci., 10, 1793–1806, https://doi.org/10.5194/nhess-10-1793-2010,
2010.
Lay, T.: A review of the rupture characteristics of the 2011 Tohoku-oki Mw 9.1 earthquake, Tectonophysics, 733, 4–36, https://doi.org/10.1016/j.tecto.2017.09.022, 2018.
Li, L., Switzer, A. D., Chan, C. H., Wang, Y., Weiss, R., and Qiu, Q.: How
heterogeneous coseismic slip affects regional probabilistic tsunami hazard
assessment: A case study in the South China Sea, J. Geophys. Res.-Solid, 121, 6250–6272, https://doi.org/10.1002/2016JB013111, 2016.
Li, L., Switzer, A. D., Wang, Y., Chan, C.-H., Qiu, Q., and Weiss, R.: A
modest 0.5-m rise in sea level will double the tsunami hazard in Macau, Sci.
Adv., 4, eaat1180, https://doi.org/10.1126/sciadv.aat1180, 2018.
Lin, A. T., Yao, B., Hsu, S.-K., Liu, C.-S., and Huang, C.-Y.: Tectonic
features of the incipient arc-continent collision zone of Taiwan:
Implications for seismicity, Tectonophysics, 479, 28–42,
https://doi.org/10.1016/j.tecto.2008.11.004, 2009.
Liu, P. L. F., Wang, X., and Salisbury, A. J.: Tsunami hazard and early
warning system in South China Sea, J. Asian Earth Sci., 36, 2–12, https://doi.org/10.1016/j.jseaes.2008.12.010, 2009.
Loveless, J. P. and Meade, B. J.: Geodetic imaging of plate motions, slip
rates, and partitioning of deformation in Japan, J. Geophys. Res., 115, B02410, https://doi.org/10.1029/2008JB006248, 2010.
Loveless, J. P. and Meade, B. J.: Spatial correlation of interseismic coupling and coseismic rupture extent of the 2011 MW = 9.0 Tohoku-oki
earthquake, Geophys. Res. Lett., 38, L17306, https://doi.org/10.1029/2011GL048561, 2011.
Ludwig, W. J.: The Manila Trench and West Luzon Trough – III. Seismic-refraction measurements, Deep-Sea Res. Oceanogr. Abstr., 17,
553–571, https://doi.org/10.1016/0011-7471(70)90067-7, 1970.
McCaffrey, R.: Dependence of earthquake size distributions on convergence rates at subduction zones, Geophys. Res. Lett., 21, 2327–2330, https://doi.org/10.1029/94GL02153, 1994.
McCaffrey, R.: Global frequency of magnitude 9 earthquakes, Geology, 36,
2630–266, https://doi.org/10.1130/g24402a.1, 2008.
Megawati, K., Shaw, F., Sieh, K., Huang, Z., Wu, T. R., Lin, Y., Tan, S. K.,
and Pan, T. C.: Tsunami hazard from the subduction megathrust of the South China Sea: Part I. Source characterization and the resulting tsunami, J.
Asian Earth Sci., 36, 13–20, https://doi.org/10.1016/j.jseaes.2008.11.012, 2009.
Meltzner, A. J., Sieh, K., Chiang, H.-W., Shen, C.-C., Suwargadi, B. W.,
Natawidjaja, D. H., Philibosian, B., and Briggs, R. W.: Persistent termini of
2004- and 2005-like ruptures of the Sunda megathrust, J. Geophys. Res., 117, B04405, https://doi.org/10.1029/2011JB008888, 2012.
Moore, G. F., Bangs, N. L., Taira, A., Kuramoto, S., Pangborn, E. and Tobin,
H. J.: Three-Dimensional Splay Fault Geometry and Implications for Tsunami
Generation, Science, 80, 1128–1131, https://doi.org/10.1126/science.1147195, 2007.
Moreno, M. S., Bolte, J., Klotz, J., and Melnick, D.: Impact of megathrust
geometry on inversion of coseismic slip from geodetic data: Application to
the 1960 Chile earthquake, Geophys. Res. Lett., 36, L16310, https://doi.org/10.1029/2009GL039276, 2009.
Morgan, P. M., Feng, L., Meltzner, A. J., Lindsey, E. O., Tsang, L. L. H., and Hill, E. M.: Sibling earthquakes generated within a persistent rupture
barrier on the Sunda megathrust under Simeulue Island, Geophys. Res. Lett.,
44, 2159–2166, https://doi.org/10.1002/2016GL071901, 2017.
Nishikawa, T. and Ide, S.: Earthquake size distribution in subduction zones
linked to slab buoyancy, Nat. Geosci., 7, 904–908, https://doi.org/10.1038/ngeo2279, 2014.
Okal, E. A., Synolakis, C. E., and Kalligeris, N.: Tsunami simulations for
regional sources in the South China and adjoining seas, Pure Appl. Geophys.,
168, 1153–1173, 2011.
Paris, R., Switzer, A. D., Belousova, M., Belousov, A., Ontowirjo, B., Whelley, P. L., and Ulvrova, M.: Volcanic tsunami: a review of source mechanisms, past events and hazards in Southeast Asia (Indonesia, Philippines, Papua New Guinea), Nat. Hazards, 70, 447–470,
https://doi.org/10.1007/s11069-013-0822-8, 2014.
Park, J.-O., Tsuru, T., Kodaira, S., Cummins, P. R., and Kaneda, Y.: Splay
Fault Branching Along the Nankai Subduction Zone, Science, 297, 1157–1160, https://doi.org/10.1126/science.1074111, 2002.
Pautot, G. and Rangin, C.: Subduction of the South China Sea axial ridge
below Luzon (Philippines), Earth Planet. Sc. Lett., 92, 57–69,
https://doi.org/10.1016/0012-821X(89)90020-4, 1989.
Peng, D., Hill, E. M., Li, L., Switzer, A. D., and Larson, K. M.: Application
of GNSS interferometric reflectometry for detecting storm surges, GPS Solut., 23, 47, https://doi.org/10.1007/s10291-019-0838-y, 2019.
Philip, L.-F.: Numerical solutions of three-dimensional run-up on a circular
island, Int. Symp. waves-physical Numer. Model. Univ. Br. Columbia,
Vancouver Canada, 1994, available at: https://ci.nii.ac.jp/naid/10016695852/en/ (last access: 9 April 2019), 1994.
Plafker, G.: Tectonic Deformation Associated with the 1964 Alaska Earthquake, Science 80, 1675–1687, https://doi.org/10.1126/science.148.3678.1675, 1965.
Pollitz, F. F., Brooks, B., Tong, X., Bevis, M. G., Foster, J. H., Bürgmann, R., Smalley Jr., R., Vigny, C., Socquet, A., Ruegg, J.-C.,
Campos, J., Barrientos, S., Parra, H., Soto, J. C. B., Cimbaro, S., and Blanco, M.: Coseismic slip distribution of the February 27, 2010 Mw 8.8 Maule, Chile earthquake, Geophys. Res. Lett., 38, L09309, https://doi.org/10.1029/2011GL047065, 2011.
Power, W., Wallace, L., Wang, X., and Reyners, M.: Tsunami Hazard Posed to New Zealand by the Kermadec and Southern New Hebrides Subduction Margins: An
Assessment Based on Plate Boundary Kinematics, Interseismic Coupling, and
Historical Seismicity, Pure Appl. Geophys., 169, 1–36, https://doi.org/10.1007/s00024-011-0299-x, 2012.
Qiu, Q., Hill, E. M., Barbot, S., Hubbard, J., Feng, W., Lindsey, E. O., Feng, L., Dai, K., Samsonov, S. V., and Tapponnier, P.: The mechanism of partial rupture of a locked megathrust: The role of fault morphology, Geology, 44, 875–878, https://doi.org/10.1130/G38178.1, 2016.
Ramos, N. T., Maxwell, K. V., Tsutsumi, H., Chou, Y. C., Duan, F., Shen, C. C., and Satake, K.: Occurrence of 1 ka-old corals on an uplifted reef terrace
in west Luzon, Philippines: Implications for a prehistoric extreme wave event in the South China Sea region, Geosci. Lett., 4, 12, https://doi.org/10.1186/s40562-017-0078-3, 2017.
Rong, Y., Jackson, D. D., Magistrale, H., and Goldfinger, C.: Magnitude Limits of Subduction Zone EarthquakesMagnitude Limits of Subduction Zone
Earthquakes, B. Seismol. Soc. America, 104, 2359–2377, https://doi.org/10.1785/0120130287, 2014.
Ruff, L. and Kanamori, H.: Seismicity and the subduction process, Phys. Earth Planet. Inter., 23, 240–252, https://doi.org/10.1016/0031-9201(80)90117-X, 1980.
Ruff, L. and Kanamori, H.: Seismic coupling and uncoupling at subduction zones, Tectonophysics, 99, 99–117, https://doi.org/10.1016/0040-1951(83)90097-5, 1983.
Ruiz, S., Metois, M., Fuenzalida, A., Ruiz, J., Leyton, F., Grandin, R., Vigny, C., Madariaga, R., and Campos, J.: Intense foreshocks and a slow slip
event preceded the 2014 Iquique Mw 8.1 earthquake, Science, 345, 1165–1169, https://doi.org/10.1126/science.1256074, 2014.
Salman, R., Hill, E. M., Feng, L., Lindsey, E. O., Mele veedu, D., Barbot, S., Banerjee, P., Hermawan, I., and Natawidjaja, D. H.: Piecemeal Rupture of
the Mentawai Patch, Sumatra: The 2008 Mw7.2 North Pagai Earthquake Sequence,
J. Geophys. Res.-Solid, 122, 9404–9419, https://doi.org/10.1002/2017JB014341, 2017.
Satake, K. and Atwater, B. F.: Long-Term Perspectives on Giant Earthquakes and Tsunamis at Subduction Zones, Annu. Rev. Earth Planet. Sci., 35, 349–374, https://doi.org/10.1146/annurev.earth.35.031306.140302, 2007.
Schellart, W. P. and Rawlinson, N.: Global correlations between maximum
magnitudes of subduction zone interface thrust earthquakes and physical
parameters of subduction zones, Phys. Earth Planet. Inter., 512, 299–302, https://doi.org/10.1016/j.pepi.2013.10.001, 2013.
Schurr, B., Asch, G., Hainzl, S., Bedford, J., Hoechner, A., Palo, M., Wang, R., Moreno, M., Bartsch, M., Zhang, Y., Oncken, O., Tilmann, F., Dahm, T.,
Victor, P., Barrientos, S., and Vilotte, J.-P.: Gradual unlocking of plate
boundary controlled initiation of the 2014 Iquique earthquake, Nature, 512, 299–302, https://doi.org/10.1038/nature13681, 2014.
Sella, G. F., Dixon, T. H., and Mao, A.: REVEL: A model for Recent plate
velocities from space geodesy, J. Geophys. Res.-Solid, 107, ETG 11-1–ETG 11-30, https://doi.org/10.1029/2000JB000033, 2002.
Singh, S. C., Hananto, N., Mukti, M., Robinson, D. P., Das, S., Chauhan, A.,
Carton, H., Gratacos, B., Midnet, S., Djajadihardja, Y., and Harjono, H.:
Aseismic zone and earthquake segmentation associated with a deep subducted
seamount in Sumatra, Nat. Geosci., 4, 308–311, 2011.
Song, T. R. A. and Simons, M.: Large trench-parallel gravity variations predict seismogenic behavior in subduction zones, Science, 301, 630–633, https://doi.org/10.1126/science.1085557, 2003.
Stein, S., and Okal, E. A.: Ultralong Period Seismic Study of the December 2004 Indian Ocean Earthquake and Implications for Regional Tectonics and the Subduction Process, B. Seismol. Soc. Am., 97, S279–S295, https://doi.org/10.1785/0120050617, 2007.
Stevens, V. L. and Avouac, J.: Interseismic Coupling on the Main Himalayan
Thrust, Geophys. Res. Lett., 42, 5828–5837, https://doi.org/10.1002/2015GL064845, 2015.
Sun, L., Zhou, X., Huang, W., Liu, X., Yan, H., Xie, Z., Wu, Z., Zhao, S., Shao, D., and Yang, W.: Preliminary evidence for a 1000-year-old tsunami in the South China Sea, Sci. Rep., 3, 1655, https://doi.org/10.1038/srep01655, 2013.
Suppe, J.: Tectonics of arc-continent collision on both sides of the South
China Sea: Taiwan and Mindoro, Acta Geol. Taiwanica, 26, 1–18, 1988.
Taylor, F. W., Briggs, R. W., Frohlich, C., Brown, A., Hornbach, M., Papabatu, A. K., Meltzner, A. J., and Billy, D.: Rupture across arc segment
and plate boundaries in the 1 April 2007 Solomons earthquake, Nat. Geosci., 1, 253, https://doi.org/10.1038/ngeo159, 2008.
Taylor, B. and Hayes, D. E.: The Tectonic Evolution of the South China Basin, in The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands, American Geophysical Union (AGU), 89–104, 2013.
Terry, J. P., Winspear, N., Goff, J., and Tan, P. H. H.: Past and potential
tsunami sources in the South China Sea: A brief synthesis, Earth-Sci. Rev., 167, 47–61, https://doi.org/10.1016/j.earscirev.2017.02.007, 2017.
Vigny, C., Simons, W. J. F., Abu, S., Bamphenyu, R., Satirapod, C., Choosakul, N., Subarya, C., Socquet, a, Omar, K., Abidin, H. Z., and
Ambrosius, B. A. C.: Insight into the 2004 Sumatra-Andaman earthquake from
GPS measurements in southeast Asia, Nature, 436, 201–206, https://doi.org/10.1038/nature03937, 2005.
Vigny, C., Socquet, A., Peyrat, S., Ruegg, J.-C., Métois, M., Madariaga,
R., Morvan, S., Lancieri, M., Lacassin, R., Campos, J., Carrizo, D.,
Bejar-Pizarro, M., Barrientos, S., Armijo, R., Aranda, C., Valderas-Bermejo,
M.-C., Ortega, I., Bondoux, F., Baize, S., Lyon-Caen, H., Pavez, A., Vilotte, J. P., Bevis, M., Brooks, B., Smalley, R., Parra, H., Baez, J.-C., Blanco, M., Cimbaro, S., and Kendrick, E.: The 2010 Mw 8.8 Maule Megathrust Earthquake of Central Chile, Monitored by GPS, Science, 332, 1417–1421, https://doi.org/10.1126/science.1204132, 2011.
Wang, K.: Elastic and viscoelastic models of crustal deformation in subduction earthquake cycles, in: Seism. Zo. subduction thrust faults, Columbia Univ. Press, New York, 540–575, 2007.
Wang, K. and Bilek, S. L.: Do subducting seamounts generate or stop large
earthquakes?, Geology, 39, 819–822, https://doi.org/10.1130/G31856.1, 2011.
Wang, X., Liu, P. L.-F., and Orfila, A.: Numerical simulations of tsunami runup onto a three-dimensional beach with shallow water equations, in: Advanced Numerical Models for Simulating Tsunami Waves and Runup, World Scientific, 2008, 249–253, 2008.
Wei, S., Graves, R., Helmberger, D., Avouac, J.-P., and Jiang, J.: Sources of
shaking and flooding during the Tohoku-Oki earthquake: A mixture of rupture
styles, Earth Planet. Sc. Lett., 333–334, 91–100, https://doi.org/10.1016/j.epsl.2012.04.006, 2012.
Wells, R. E., Blakely, R. J., Sugiyama, Y., Scholl, D. W., and Dinterman, P.
A.: Basin-centered asperities in great subduction zone earthquakes: A link
between slip, subsidence, and subduction erosion?, J. Geophys. Res.-Solid, 108, B102507, https://doi.org/10.1029/2002JB002072, 2003.
Wesnousky, S. G.: Seismological and structural evolution of strike-slip faults, Nature, 335, 340–343, https://doi.org/10.1038/335340a0, 1988.
Wesnousky, S. G.: Predicting the endpoints of earthquake ruptures, Nature,
444, 358–360, https://doi.org/10.1038/nature05275, 2006.
Witter, R. C., Carver, G. A., Briggs, R. W., Gelfenbaum, G., Koehler, R. D.,
La Selle, S., Bender, A. M., Engelhart, S. E., Hemphill-Haley, E., and Hill,
T. D.: Unusually large tsunamis frequent a currently creeping part of the
Aleutian megathrust, Geophys. Res. Lett., 43, 76–84, https://doi.org/10.1002/2015GL066083, 2016.
Wu, J., Suppe, J., Lu, R., and Kanda, R.: Philippine Sea and East Asian plate
tectonics since 52 Ma constrained by new subducted slab reconstruction
methods, J. Geophys. Res.-Solid, 121, 4670–4741, https://doi.org/10.1002/2016JB012923, 2016.
Wu, T.-R. and Huang, H.-C.: Modeling tsunami hazards from Manila trench to
Taiwan, J. Asian Earth Sci., 36, 21–28, https://doi.org/10.1016/j.jseaes.2008.12.006, 2009.
Xie, X., Chen, C., Li, L., Wu, S., Yuen, D. A., and Wang, D.: Tsunami hazard
assessment for atoll islands inside the South China Sea: A case study of the
Xisha Archipelago, Phys. Earth Planet. Inter., 290, 20–35, https://doi.org/10.1016/j.pepi.2019.03.003, 2019.
Yang, W., Sun, L., Yang, Z., Gao, S., Gao, Y., Shao, D., Mei, Y., Zang, J.,
Wang, Y., and Xie, Z.: Nan'ao, an archaeological site of Song dynasty destroyed by tsunami, Chinese Sci. Bull., 64, 107–120, 2018.
Yokota, Y., Ishikawa, T., Watanabe, S., Tashiro, T., and Asada, A.: Seafloor
geodetic constraints on interplate coupling of the Nankai Trough megathrust
zone, Nature, 534, 374–377, https://doi.org/10.1038/nature17632, 2016.
Yu, H., Liu, Y., Yang, H., and Ning, J.: Modeling earthquake sequences along
the Manila subduction zone: Effects of three-dimensional fault geometry,
Tectonophysics, 733, 73–84, https://doi.org/10.1016/j.tecto.2018.01.025, 2018.
Yu, K.-F., Zhao, J.-X., Shi, Q., and Meng, Q.-S.: Reconstruction of storm/tsunami records over the last 4000 years using transported coral blocks and lagoon sediments in the southern South China Sea, Quatern. Int., 195, 128–137, https://doi.org/10.1016/j.quaint.2008.05.004, 2009.
Zhu, J., Sun, Z., Kopp, H., Qiu, X., Xu, H., Li, S., and Zhan, W.: Segmentation of the Manila subduction system from migrated multichannel
seismics and wedge taper analysis, Mar. Geophys. Res., 34, 379–391, https://doi.org/10.1007/s11001-013-9175-7, 2013.
Short summary
The accuracy of tsunami hazard assessments is highly dependent on the reliability of earthquake source models. In this study, we combine the most updated geological and geophysical data of the Manila subduction zone to propose a series of possible rupture scenarios. These rupture models facilitate an improved understanding of the potential tsunami hazard in the South China Sea. The results highlight the grave consequences faced by the SCS, one of the world's most densely populated coastlines.
The accuracy of tsunami hazard assessments is highly dependent on the reliability of earthquake...
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