Articles | Volume 19, issue 12
https://doi.org/10.5194/nhess-19-2811-2019
© 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-19-2811-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
13 Dec 2019
Research article |
| 13 Dec 2019
| 13 Dec 2019
Infrasound and seismoacoustic signatures of the 28 September 2018 Sulawesi super-shear earthquake
BGR, B4.3 (Federal Institute for Geosciences and Natural Resources),
Hanover, Germany
Peter Gaebler
BGR, B4.3 (Federal Institute for Geosciences and Natural Resources),
Hanover, Germany
Lars Ceranna
BGR, B4.3 (Federal Institute for Geosciences and Natural Resources),
Hanover, Germany
Alexis Le Pichon
CEA, DAM, DIF, 91297 Arpajon, France
Julien Vergoz
CEA, DAM, DIF, 91297 Arpajon, France
Anna Perttu
EOS (Earth Observatory of Singapore), NTU (Nanyang Technological
University), Singapore
Dorianne Tailpied
EOS (Earth Observatory of Singapore), NTU (Nanyang Technological
University), Singapore
Benoit Taisne
EOS (Earth Observatory of Singapore), NTU (Nanyang Technological
University), Singapore
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Seismic and infrasound methods are techniques used to monitor natural events and explosions. At low frequencies, band signal can be dominated by microbaroms and microseisms. The noise observations in the Kazakh network are performed and compared with source and propagation modeling. The network is dense and well situated for studying very distant source regions of the ambient noise. The prospects are opening for the use of ocean noise in solid Earth and atmosphere tomography.
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Sedimentary beds can exhibit signs of local deformation in pyroclastic strata. Patterns are reviewed and trigger mechanisms interpreted.
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Morgan Vervoort, Katleen Wils, Kris Vanneste, Roberto Urrutia, Mario Pino, Catherine Kissel, Marc De Batist, and Maarten Van Daele
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Melody Philippon, Jean Roger, Jean-Frédéric Lebrun, Isabelle Thinon, Océane Foix, Stéphane Mazzotti, Marc-André Gutscher, Leny Montheil, and Jean-Jacques Cornée
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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
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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.
Danhua Xin, James Edward Daniell, Zhenguo Zhang, Friedemann Wenzel, Shaun Shuxun Wang, and Xiaofei Chen
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2024-138, https://doi.org/10.5194/nhess-2024-138, 2024
Revised manuscript accepted for NHESS
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A high-resolution fixed asset model can help improve the accuracy of earthquake loss assessment. We develop a grid-level fixed asset model for China from 1951 to 2020. We first compile the provincial-level fixed asset from yearbook-related statistics. Then, this dataset is disaggregated into 1 km*1 km grids by using multiple remote sensing data as the weight indicator. We find that fixed asset value increased rapidly after the 1980s and reached 589.31 trillion Chinese yuan in 2020.
Alaa Jbara and Michael Tsesarsky
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2024-150, https://doi.org/10.5194/nhess-2024-150, 2024
Revised manuscript under review for NHESS
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Fragile geological features are the only empirical data to validate seismic hazard analysis over prehistoric timescales. We present a fragility analysis of a 42 m high rock pillar. Based on LiDAR scanning and in-situ rock elastic modulus measurements, we developed an accurate finite element model. The model was validated by comparing computational modal analysis with in-situ measurements of natural vibrations. Dynamic fragility analysis was used to challenge regional seismic hazard estimates.
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.
Jia Cheng, Chong Xu, Xiwei Xu, Shimin Zhang, and Pengyu Zhu
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2024-96, https://doi.org/10.5194/nhess-2024-96, 2024
Revised manuscript accepted for NHESS
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The Northwestern Yunnan Region (NWYR), with a complex network of active faults, presents significant seismic hazards such as multi-segment ruptures and landslides. This article introduces a new seismic hazard model, which integrates fault slip parameters to assess the risks associated with multi-segment ruptures. The results reveal the intricate relationship between these ruptures and the regional small block rotation induced by regional low-crustal flow and gravitational collapse.
Quetzalcoatl Rodríguez-Pérez and F. Ramón Zúñiga
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2024-92, https://doi.org/10.5194/nhess-2024-92, 2024
Revised manuscript under review for NHESS
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Seismic intensity reflects earthquake damage, although this parameter is often subjective. On the other hand, peak acceleration values are a direct measure of earthquake effects. Seismic intensity was used to describe historical earthquakes, and its use is rare today. For this reason, it is important to have a relationship between these parameters of strong movements in order to predict the acceleration of historical earthquakes.
Bénédicte Donniol Jouve, Anne Socquet, Céline Beauval, Jesús Piña Valdès, and Laurentiu Danciu
EGUsphere, https://doi.org/10.5194/egusphere-2024-787, https://doi.org/10.5194/egusphere-2024-787, 2024
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This research investigates how geodetic monitoring enhances accuracy in seismic hazard assessment. By utilizing geodetic strain rate maps for Europe and the ESHM20 source model, we compare geodetic and seismic moment rates across the continent while addressing associated uncertainties. Our analysis reveals primary compatibility in high-activity zones. In well-constrained regions of lower activity, we also observed an overlap in the distribution of seismic and geodetic moments.
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.
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.
Oceane Foix, Stéphane Mazzotti, Hervé Jomard, Didier Bertil, and the Lesser Antilles Working Group
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2024-53, https://doi.org/10.5194/nhess-2024-53, 2024
Preprint under review for NHESS
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By analyzing historical and instrumental seismic data, fault knowledge and geodetic measurements, we provide a new understanding of seismic hazard in the Lesser Antilles via seismotectonic zoning. We propose new models that can have a significant impact on seismic hazard assessment, such as the inclusion of mantle wedge seismicity, volcanic seismicity and a complete revision of the subduction interface zoning.
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.
Olga-Joan Ktenidou, Antonia Papageorgiou, Erion-Vasilis Pikoulis, Spyros Liakopoulos, Fevronia Gkika, Ziya Cekinmez, Panagiotis Savvaidis, Kalliopi Fragouli, and Christos P. Evangelidis
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2023-233, https://doi.org/10.5194/nhess-2023-233, 2024
Revised manuscript accepted for NHESS
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Greek seismic data are valuable in European and even global databases, due to its high seismicity and numerous seismic stations. Seismic data coming from stations that lie on rock (i.e., not soil) sits are particularly valuable in seismology to define reference ground conditions and ground motions. However, little knowledge exists yet on how rock stations in Greece behave. This is the first time the network of the National Observatory is studied systematically to reveal reference stations.
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.
Marta Han, Leila Mizrahi, and Stefan Wiemer
EGUsphere, https://doi.org/10.5194/egusphere-2023-3153, https://doi.org/10.5194/egusphere-2023-3153, 2024
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Relying on recent accomplishments in collecting and harmonizing data by the 2020 European Seismic Hazard Model (ESHM20) and leveraging advancements in state-of-the-art earthquake forecasting methods, we develop a harmonized earthquake forecasting model for Europe. We propose several model variants and test them on training data for consistency and on a seven-year testing period against each other, as well as against both a time-independent benchmark and a global time-dependent benchmark.
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.
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.
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.
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.
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.
Cited articles
Ardhuin, F. and Herbers, T. H. C.: Noise generation in the solid Earth, oceans
and atmosphere, from nonlinear interacting surface gravity waves in finite
depth, J. Fluid Mech., 716, 316–348, https://doi.org/10.1017/jfm.2012.548, 2013.
Arrowsmith, S. J., Johnson, J. B., Drob, D. P., and Hedlin, M. A. H.: The
seismoacoustic wavefield: A new paradigm in studying geophysical phenomena,
Rev. Geophys., 48, RG4003, https://doi.org/10.1029/2010RG000335, 2010.
Assink, J. D., Averbuch, G., Smets, P. S. M., and Evers, L. G.: On the
infrasound detected from the 2013 and 2016 dprk's underground nuclear tests,
Geophys. Res. Lett., 43, 3526–3533, https://doi.org/10.1002/2016GL068497, 2016.
Bao, H., Ampuero, J.-P., Meng, L., Fielding, E. J., Liang, C., Milliner, C. W. D., Feng,
T., and Huang, H.: Early and persistent supershear rupture of the 2018
magnitude 7.5 Palu earthquake, Nat. Geosci., 12, 200–205, https://doi.org/10.1038/s41561-018-0297-z, 2019.
Bernard, P. and Baumont, D.: Shear Mach wave characterization for kinematic
fault rupture models with constant supershear rupture velocity, Geophys.
J. Int., 162, 431–447, https://doi.org/10.1111/j.1365-246X.2005.02611.x, 2005.
Bouchon, M. and Vallée, M.: Observation of Long Supershear Rupture
during the Magnitude 8.1 Kunlunshan Earthquake, Science, 301, 824–826, https://doi.org/10.1126/science.1086832, 2003.
Bouchon, M., Toksöz, N., Karabulut, H., Bouin, M.-P., Dietrich, M.,
Aktar, M., and Edie, M.: Seismic imaging of the 1999 Izmit (Turkey) Rupture
inferred from the near-fault recordings, Geophys. Res. Lett., 27, 3013–3016,
https://doi.org/10.1029/2000GL011761, 2000.
Bowman, D. C.: Yield and emplacement depth effects on acoustic signals from
buried explosions in hard rock, B. Seismol. Soc.
Am., 109, 944–958, https://doi.org/10.1785/0120180285, 2019.
Cansi, Y.: An automatic seismic event processing for detection and location:
the PMCC method, Geophys. Res. Lett., 22, 1021–1024, https://doi.org/10.1029/95GL00468,
1995.
Doan, M.-L. and Gary, G.: Rock pulverization at high strain rate near the
San Andreas fault, Nat. Geosci., 2, 709–712, https://doi.org/10.1038/NGEO640, 2009.
Donn, W. L. and Naini, B.: Sea wave origin of microbaroms and microseisms,
J. Geophys. Res., 78, 4482–4488, https://doi.org/10.1029/JC078i021p04482, 1973.
Drob, D. P., Picone, J. M., and Garcés, M. A.: Global morphology of
infrasound propagation, J. Geophys. Res., 108, 4680, https://doi.org/10.1029/2002JD003307, 2003.
Drob, D. P., Emmert, J. T., Crowley, G., Picone, J. M., Shepherd, G. G.,
Skinner, W., Hays, P., Niciejewski, R. J., Larsen, M., She, C. Y.,
Meriwether, J. W., Hernandez, G., Jarvis, M. J., Sipler, D. P., Tepley, C.
A., O'Brien, M. S., Bowman, J. R., Wu, Q., Murayama, Y., Kawamura, S., Reid,
I. M., and Vincent R. A.: An Empirical Model of the Earth's Horizontal Wind
Fields: HWM07, J. Geophys. Res., 113, A12304, https://doi.org/10.1029/2008JA013668, 2008.
Dunham, E. M. and Archuleta, R. J.: Evidence for a Supershear Transient
during the 2002 Denali Fault Earthquake, B. Seismol.
Soc. Am., 94, S256, https://doi.org/10.1785/0120040616, 2004.
ECMWF: European Centre for Medium-Range Weather Forecasts, Integrated Forecast System analysis data, available at: https://www.ecmwf.int (last access: 2 September 2019), 2018.
Gaebler, P., Ceranna, L., Nooshiri, N., Barth, A., Cesca, S., Frei, M., Grünberg, I., Hartmann, G., Koch, K., Pilger, C., Ross, J. O., and Dahm, T.: A multi-technology analysis of the 2017 North Korean nuclear test, Solid Earth, 10, 59–78, https://doi.org/10.5194/se-10-59-2019, 2019.
Garcés, M. A.: On Infrasound Standards, Part 1: Time, Frequency, and
Energy Scaling, InfraMatics, 2, 13–35, https://doi.org/10.4236/inframatics.2013.22002, 2013.
Gibbons, S. J., Asming, V., Eliasson, L., Fedorov, A., Fyen, J., Kero, J.,
Kozlovskaya, E., Kvaerna, T., Liszka, L., Näsholm, S. P., Raita, T.,
Roth, M., Tiira, T., and Vinogradov, Y.: The European Arctic: A Laboratory
for Seismoacoustic Studies, Seismol. Res. Lett., 86, 917–928, https://doi.org/10.1785/0220140230, 2015a.
Gibbons, S. J., Kværna, T., and Mykkeltveit, S.: Could the IMS
Infrasound Stations Support a Global Network of Small Aperture Seismic
Arrays?, Seismol. Res. Lett., 86, 1148–1159, https://doi.org/10.1785/0220150068, 2015b.
Green, D. N., Vergoz, J., Gibson, R., Le Pichon A., and Ceranna, L.:
Infrasound radiated by the Gerdec and Chelopechene explosions: propagation
along unexpected paths, Geophys. J. Int., 185, 890–910, https://doi.org/10.1111/j.1365-246X.2011.04975.x, 2011.
Hedlin, M. A. H., Walker, K. T., Drob, D. P., and de Groot-Hedlin, C. D.:
Infrasound: Connecting the Solid Earth, Oceans, and Atmosphere, Annu. Rev. Earth Pl. Sc., 40, 327–354, https://doi.org/10.1146/annurev-earth-042711-105508, 2012.
Heidarzadeh, M., Muhari, A., and Wijanarto, A. B.: Insights on the Source of
the 28 September 2018 Sulawesi Tsunami, Indonesia Based on Spectral Analyses
and Numerical Simulations, Pure Appl. Geophys., 176, 25–43, https://doi.org/10.1007/s00024-018-2065-9, 2019.
Hernandez, B., Le Pichon, A., Vergoz, J., Herry, P., Ceranna, L., Pilger,
C., Marchetti, E., Ripepe, M., and Bossu, R.: Estimating the Ground-Motion
Distribution of the 2016 Mw 6.2 Amatrice, Italy, Earthquake Using Remote
Infrasound Observations, Seismol. Res. Lett., 89, 2227–2236, https://doi.org/10.1785/0220180103, 2018.
Jamelot, A., Gailler, A., Heinrich, P., Vallage, A., and Champenois, J.:
Tsunami Simulations of the Sulawesi Mw 7.5 Event: Comparison of Seismic
Sources Issued from a Tsunami Warning Context Versus Post-Event Finite
Source, Pure Appl. Geophys., 176, 3351–3376, https://doi.org/10.1007/s00024-019-02274-5,
2019.
Katili, J. A.: Past and Present Geotectonic Position of Sulawesi, Indonesia,
Tectonophysics, 45, 289–322, https://doi.org/10.1016/0040-1951(78)90166-X, 1978.
Kulichkov, S. N., Chunchuzov, I. P., and Popov, O. I.: Simulating the
Influence of an Atmospheric Fine Inhomogeneous Structure on Long Range
Propagation of Pulsed Acoustic Signals, Izv. Atmos. Ocean.
Phys.+, 46, 60–68, https://doi.org/10.1134/S0001433810010093, 2010.
Landès, M., Le Pichon, A., Shapiro, N. M., Hillers, G., and Campillo, M.:
Explaining global patterns of microbarom observations with wave action
models, Geophys. J. Int., 199, 1328–1337, https://doi.org/10.1093/gji/ggu324,
2014.
Le Pichon, A., Guilbert, J., Vega, A., Garcés, M. A., and Brachet, N.:
Ground-coupled air waves and diffracted infrasound from the Arequipa
earthquake of June 23, 2001, Geophys. Res. Lett., 29, 1886–1889, https://doi.org/10.1029/2002GL015052, 2002.
Le Pichon, A., Guilbert, J., Vallée, M., Dessa, J. X., and Ulziibat, M.:
Infrasonic imaging of the Kunlun Mountains for the great 2001 China
earthquake, Geophys. Res. Lett., 30, 1814–1817, https://doi.org/10.1029/2003GL017581,
2003.
Le Pichon, A., Herry, P., Mialle, P., Vergoz, J., Brachet, N., Garces, M.
A., Drob, D., and Ceranna, L.: Infrasound associated with 2004–2005 large
Sumatra earthquakes and tsunami, Geophys. Res. Lett., 32, L19802, https://doi.org/10.1029/2005GL023893, 2005.
Le Pichon, A., Mialle, P., Guilbert, J., and Vergoz, J.: Multistation
infrasonic observations of the Chilean earthquake of 2005 June 13,
Geophys. J. Int., 167, 838–844, https://doi.org/10.1111/j.1365-246X.2006.03190.x, 2006.
Le Pichon, A., Blanc, E., and Hauchecorne, A. (Eds.): Infrasound Monitoring
for Atmospheric Studies, Springer, Heidelberg, Germany, ISBN 978-1-4020-9507-8, 2010.
Le Pichon, A., Ceranna, L., and Vergoz, J.: Incorporating numerical modeling
into estimates of the detection capability of the IMS infrasound network,
J. Geophys. Res., 117, D05121, https://doi.org/10.1029/2011JD016670, 2012.
Le Pichon, A., Blanc, E., and Hauchecorne, A. (Eds.): Infrasound for
Atmospheric Studies – Challenges in Middle Atmosphere Dynamics and Societal
Benefits, Springer, Heidelberg, Germany, ISBN 978-3-319-75138-2, 2019.
Marchetti, E., Lacanna, G., Le Pichon, A., Piccinini, D., and Ripepe, M.:
Evidence of large infrasonic radiation induced by earthquake interaction
with alluvial sediments, Seismol. Res. Lett., 87, 678–684, https://doi.org/10.1785/0220150223, 2016.
Matoza, R., Green, D. N., Le Pichon, A., Shearer, P. M., Fee, D., Mialle,
P., and Ceranna, L.: Automated detection and cataloging of global explosive
volcanism using the International Monitoring System infrasound network,
J. Geophys. Res.-Sol. Ea., 122, 2946–2971, https://doi.org/10.1002/2016JB013356,
2017.
Mutschlecner, J. P. and Whitaker, R. W.: Infrasound from earthquakes,
J. Geophys. Res., 110, D01108, https://doi.org/10.1029/2004JD005067, 2005.
Negraru, P. T., Golden, P., and Herrin, E. T.: Infrasound Propagation in the
“Zone of Silence”, Seismol. Res. Lett., 81, 614–624, https://doi.org/10.1785/gssrl.81.4.614, 2010.
Olson, J. V., Wilson, C. R., and Hansen, R. A.: Infrasound associated with the
2002 Denali fault earthquake, Alaska, Geophys. Res. Lett., 30, 2195–2198, https://doi.org/10.1029/2003GL018568, 2003.
Omira, R., Dogan, G. G., Hidayat, R., Husrin, S., Prasetya, G., Annunziato,
A., Proietti, C., Probst, P., Paparo, M. A., Wronna, M., Zaytsev, A.,
Pronin, P., Giniyatullin, A., Putra, P. S., Hartanto, D., Ginanjar, G.,
Kongko, W., Pelinovsky, E., and Yalciner, A. C.: The September 28th, 2018,
Tsunami In Palu-Sulawesi, Indonesia: A Post-Event Field Survey, Pure
Appl. Geophys., 176, 1379–1395, https://doi.org/10.1007/s00024-019-02145-z, 2019.
Pailoplee, S.: Probabilities of Earthquake Occurrences along the
Sumatra-Andaman Subduction Zone, Open Geosci., 9, 53–60, https://doi.org/10.1515/geo-2017-0004, 2017.
Picone, J. M., Hedin, A. E., Drob, D. P., and Aikin, A. C.: NRLMSISE-00
Empirical Model of the Atmosphere: Statistical Comparisons and Scientific
Issues, J. Geophys. Res., 107, 1468–1483, https://doi.org/10.1029/2002JA009430,
2002.
Pilger, C., Ceranna, L., Ross, J. O., Vergoz, J., Le Pichon, A., Brachet, N.,
Blanc, E., Kero, J., Liszka, L., Gibbons, S., Kvaerna, T., Näsholm,
S. P., Marchetti, E., Ripepe, M., Smets, P., Evers, L., Ghica, D., Ionescu,
C., Sindelarova, T., Ben Horin, Y., and Mialle, P.: The European Infrasound
Bulletin, Pure Appl. Geophys., 175, 3619–3638, https://doi.org/10.1007/s00024-018-1900-3,
2018.
Shani-Kadmiel, S., Assink, J. D., Smets, P. S. M., and Evers, L. G.:
Seismoacoustic coupled signals from earthquakes in Central Italy: epicentral
and secondary sources of infrasound, Geophys. Res. Lett., 45, 427–435, https://doi.org/10.1002/2017GL076125, 2017.
Socquet, A., Hollingsworth, J., Pathier, E., and Bouchon, M.: Evidence of
supershear during the 2018 magnitude 7.5 Palu earthquake from space geodesy,
Nat. Geosci., 12, 192–199, https://doi.org/10.1038/s41561-018-0296-0, 2019.
Sutherland, L. C. and Bass, H. E.: Atmospheric absorption in the atmosphere
up to 160 km, J. Acoust. Soc. Am., 115, 1012–1032, https://doi.org/10.1121/1.1631937, 2004.
Tailpied, D., Le Pichon, A., Marchetti, E., Assink, J., and Vergniolle, S.:
Assessing and optimizing the performance of infrasound networks infrasound
networks to monitor volcanic eruptions, Geophys. J. Int.,
208, 437–448, https://doi.org/10.1093/gji/ggw400, 2017.
USGS: U.S. Geological Survey, Sulawesi 2018 earthquake event page, available
at: https://earthquake.usgs.gov/earthquakes/eventpage/us1000h3p4/ (last
access: 2 September 2019), 2018.
Walker, K. T., Le Pichon, A., Kim, T. S., de Groot-Hedlin, C., Che, I.-Y.,
and Garcés, M.: An analysis of ground shaking and transmission loss from
infrasound generated by the 2011 Tohoku earthquake, J. Geophys.
Res., 118, 12831–12851, https://doi.org/10.1002/2013JD020187, 2013.
Wang, D. and Mori, J.: The 2010 Qinghai, China, Earthquake: A Moderate
Earthquake with Supershear Rupture, B. Seismol. Soc.
Am., 102, 301–308, https://doi.org/10.1785/0120110034, 2012.
Waxler, R., Assink, J., Hetzer, C., and Velea, D.: NCPAprop – A software
package for infrasound propagation modeling, J. Acoust.
Soc. Am., 141, 3627–3627, https://doi.org/10.1121/1.4987797, 2017.
Wilson, D. K.: The sound-speed gradient and refraction in the near-ground
atmosphere, J. Acoust. Soc. Am., 113, 750–757, https://doi.org/10.1121/1.1532028, 2003.
Young, J. M. and Greene, G. E.: Anomalous infrasound generated by the
Alaskan earthquake of 28 march 1964, J. Acoust. Soc. Am., 71, 334–339, https://doi.org/10.1121/1.387457, 1982.
Yue, H., Lay, T., Freymueller, J. T., Ding, K., Rivera, L., Ruppert, N. A.,
and Koper, K. D.: Supershear rupture of the 5 January 2013 Craig, Alaska (Mw 7.5) earthquake, J. Geophys. Res., 118, 5903–5919, https://doi.org/10.1002/2013JB010594,
2013.
Short summary
This paper provides infrasound data analysis, modeling, and interpretation of the source characteristics of the 28 September 2018 magnitude 7.5 Sulawesi earthquake. Epicentral ground movement by the earthquake rupture as well as the secondary shaking of nearby mountainous topography is responsible for the strong infrasound generated. Findings allow one to improve knowledge of infrasonic and seismoacoustic source processes and the monitoring capabilities of the infrasound arrays used.
This paper provides infrasound data analysis, modeling, and interpretation of the source...
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