Articles | Volume 17, issue 5
https://doi.org/10.5194/essd-17-2087-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/essd-17-2087-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Data description paper
| 
19 May 2025
Data description paper |
| 19 May 2025
| 19 May 2025
Seismic survey in an urban area: the activities of the EMERSITO INGV emergency group in Ancona (Italy) following the 2022 Mw 5.5 Costa Marchigiana–Pesarese earthquake
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Roma1, Rome, Italy
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Roma1, Rome, Italy
Giuseppe Di Giulio
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Roma1, L'Aquila, Italy
Giovanna Cultrera
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Roma1, Rome, Italy
Francesca Pacor
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Milano, Milan, Italy
Sara Lovati
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Milano, Milan, Italy
Gaetano Riccio
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Irpinia, Grottaminarda, Italy
Maurizio Vassallo
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Roma1, L'Aquila, Italy
Giulio Brunelli
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Milano, Milan, Italy
Antonio Costanzo
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Osservatorio Nazionale Terremoti, Rende, Italy
Antonella Bobbio
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Osservatorio Vesuviano, Naples, Italy
Marta Pischiutta
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Roma2, Rome, Italy
Rodolfo Puglia
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Milano, Milan, Italy
Marco Massa
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Milano, Milan, Italy
Rocco Cogliano
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Irpinia, Grottaminarda, Italy
Salomon Hailemikael
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Roma1, Rome, Italy
Alessia Mercuri
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Roma1, Rome, Italy
Giuliano Milana
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Roma1, Rome, Italy
Luca Minarelli
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Roma1, L'Aquila, Italy
Alessandro Di Filippo
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Osservatorio Vesuviano, Naples, Italy
Lucia Nardone
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Osservatorio Vesuviano, Naples, Italy
Simone Marzorati
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Osservatorio Nazionale Terremoti, Ancona, Italy
Chiara Ladina
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Osservatorio Nazionale Terremoti, Ancona, Italy
Debora Pantaleo
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Osservatorio Nazionale Terremoti, Ancona, Italy
Carlo Calamita
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Osservatorio Nazionale Terremoti, Ancona, Italy
Maria Grazia Ciaccio
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Roma1, Rome, Italy
Antonio Fodarella
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Irpinia, Grottaminarda, Italy
Stefania Pucillo
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Irpinia, Grottaminarda, Italy
Giuliana Mele
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Roma1, Rome, Italy
Carla Bottari
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Osservatorio Etneo, Catania, Italy
Gaetano De Luca
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Osservatorio Nazionale Terremoti, L'Aquila, Italy
Luigi Falco
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Irpinia, Grottaminarda, Italy
Antonino Memmolo
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Irpinia, Grottaminarda, Italy
Giulia Sgattoni
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna, Bologna, Italy
Gabriele Tarabusi
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna, Bologna, Italy
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Paolo Boncio, Giuliano Milana, Fabrizio Cara, Giuseppe Di Giulio, Deborah Di Naccio, Daniela Famiani, Francesca Liberi, Fabrizio Galadini, Gianluigi Rosatelli, and Maurizio Vassallo
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2016-313, https://doi.org/10.5194/nhess-2016-313, 2016
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The paper discusses geological aspects, methodological procedures of seismic microzonation and the implications on seismic site response of an urbanized area in a geologic environment of deep continental basin (the Avezzano town in the Fucino continental basin of central Apennines, Italy). The paper is of potential interest for the geological community and also for non-geologist scientists/technicians/decision makers working in the field of earthquake hazard.
Andrea Pio Ferreri, Annalisa Romeo, Rossella Giannuzzi, Teresa Ninivaggi, Marilena Filippucci, Gianpaolo Cecere, Luigi Falco, Maddalena Michele, Giulio Selvaggi, and Andrea Tallarico
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2025-335, https://doi.org/10.5194/essd-2025-335, 2025
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The Gargano Promontory (Italy) has been monitored by the OTRIONS network since 2013 and has contributed to civil protection surveillance since 2019. A decade of records were reanalyzed with automatic methods, identifying over 6900 events, of which only 60% were earthquakes, confirming the need for manual review. The revised seismicity reveals that seismic sources are located deep in the lower crust in the centre Gargano and at intermediate crust along the Mattinata fault in the southern Gargano.
Marco Massa, Andrea Luca Rizzo, Davide Scafidi, Elisa Ferrari, Sara Lovati, Lucia Luzi, and MUDA working group
Earth Syst. Sci. Data, 16, 4843–4867, https://doi.org/10.5194/essd-16-4843-2024, https://doi.org/10.5194/essd-16-4843-2024, 2024
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MUDA (geophysical and geochemical MUltiparametric DAtabase) is a new infrastructure of the National Institute of Geophysics and Volcanology serving geophysical and geochemical multiparametric data. MUDA collects information from different sensors, such as seismometers, accelerometers, hydrogeochemical sensors, meteorological stations and sensors for the flux of carbon dioxide and radon gas, with the aim of making correlations between seismic phenomena and variations in environmental parameters.
Lauro Chiaraluce, Richard Bennett, David Mencin, Wade Johnson, Massimiliano Rinaldo Barchi, Marco Bohnhoff, Paola Baccheschi, Antonio Caracausi, Carlo Calamita, Adriano Cavaliere, Adriano Gualandi, Eugenio Mandler, Maria Teresa Mariucci, Leonardo Martelli, Simone Marzorati, Paola Montone, Debora Pantaleo, Stefano Pucci, Enrico Serpelloni, Mariano Supino, Salvatore Stramondo, Catherine Hanagan, Liz Van Boskirk, Mike Gottlieb, Glen Mattioli, Marco Urbani, Francesco Mirabella, Assel Akimbekova, Simona Pierdominici, Thomas Wiersberg, Chris Marone, Luca Palmieri, and Luca Schenato
Sci. Dril., 33, 173–190, https://doi.org/10.5194/sd-33-173-2024, https://doi.org/10.5194/sd-33-173-2024, 2024
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We built six observatory stations in central Italy to monitor a fault potentially capable of generating a strong earthquake. Each site has 80–160 m deep wells equipped with strainmeters and seismometers. At the surface, we placed GNSS antennas and seismic and meteorological sensors. All data, which are open access for the scientific community, will help us to better understand the complex physical and chemical processes that lead to the generation of the full range of slow and fast earthquakes.
Fabrizio Marra, Alberto Frepoli, Dario Gioia, Marcello Schiattarella, Andrea Tertulliani, Monica Bini, Gaetano De Luca, and Marco Luppichini
Nat. Hazards Earth Syst. Sci., 22, 2445–2457, https://doi.org/10.5194/nhess-22-2445-2022, https://doi.org/10.5194/nhess-22-2445-2022, 2022
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Through the analysis of the morphostructural setting in which the seismicity of Rome is framed, we explain why the city should not expect to suffer damage from a big earthquake.
Nicola Piana Agostinetti and Giulia Sgattoni
Solid Earth, 12, 2717–2733, https://doi.org/10.5194/se-12-2717-2021, https://doi.org/10.5194/se-12-2717-2021, 2021
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One of the present-day challenges for geoscientists is tackling the big data revolution. An ever-growing amount of data needs to be processed and data are subjectively handled before using them to make inferences on the Earth’s interior. But imposing subjective decisions on the data might have strong influences on the final outputs. Here we present a totally novel and automatic application for screening the data and for defining data volumes that are consistent with physical hypotheses.
Lucia Nardone, Roberta Esposito, Danilo Galluzzo, Simona Petrosino, Paola Cusano, Mario La Rocca, Mauro Antonio Di Vito, and Francesca Bianco
Adv. Geosci., 52, 75–85, https://doi.org/10.5194/adgeo-52-75-2020, https://doi.org/10.5194/adgeo-52-75-2020, 2020
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We studied the subsoil structure of the Campi Flegrei area using both spectral ratios and array techniques (f-k and MSPAC) applied to seismic noise recorded by three different array. By means of joint inversion of dispersion curve and spectral ratio we obtained a Vs model, that is in a good agreement with the stratigraphic information available in the area. In areas such as Campi Flegrei the definition of the velocity model is a crucial issue to characterize the physical parameters of the medium
Danilo Galluzzo, Lucia Nardone, Mario La Rocca, Antonietta M. Esposito, Roberto Manzo, and Rosa Di Maio
Adv. Geosci., 52, 67–74, https://doi.org/10.5194/adgeo-52-67-2020, https://doi.org/10.5194/adgeo-52-67-2020, 2020
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Spectral analysis has been applied to seismic events recorded at Vesuvius volcano to test a new tool for a fast event classification. We computed two spectral parameters, central frequency and shape factor from the spectral moments. The results show that volcano-tectonic earthquakes and low frequency events are distinguishable though the spectral moments. Since the computation of spectral parameters is easy and fast, it may become an effective tool for classification in observatory practice.
Stefano Gori, Emanuela Falcucci, Chiara Ladina, Simone Marzorati, and Fabrizio Galadini
Solid Earth, 8, 319–337, https://doi.org/10.5194/se-8-319-2017, https://doi.org/10.5194/se-8-319-2017, 2017
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We integrated geological and geophysical data to study the evolution of a large sector of the central Apennines, in Italy. The adopted approach permitted us to cast light on timing of faults activity over the past about 2 million years. The results we obtained has implication in terms of assessment of seismic sources of strong earthquakes. In particular, we defined which of the investigated faults are able to produce large-magnitude seismic events and which are no longer able.
Aladino Govoni, Luciana Bonatto, Marco Capello, Adriano Cavaliere, Claudio Chiarabba, Ezio D'Alema, Stefania Danesi, Sara Lovati, Lucia Margheriti, Marco Massa, Salvatore Mazza, Francesco Mazzarini, Stephen Monna, Milena Moretti, Anna Nardi, Davide Piccinini, Claudia Piromallo, Silvia Pondrelli, Simone Salimbeni, Enrico Serpelloni, Stefano Solarino, Massimiliano Vallocchia, Marco Santulin, and the AlpArray Working Group
Adv. Geosci., 43, 39–52, https://doi.org/10.5194/adgeo-43-39-2017, https://doi.org/10.5194/adgeo-43-39-2017, 2017
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We describe here the contribution of Istituto Nazionale di Geofisica e Vulcanolgia (INGV) to the AlpArray Seismic Network (AASN) in the framework of the AlpArray project (http://www.alparray.ethz.ch), a large European collaborative research initiative.
The aim of AlpArray is carrying out cutting edge research to advance our understanding of the deep structure, geodynamics, tectonics and seismic hazard of the greater Alpine area (Alps-Apennines-Carpathians-Dinarides orogenic system).
Paolo Boncio, Giuliano Milana, Fabrizio Cara, Giuseppe Di Giulio, Deborah Di Naccio, Daniela Famiani, Francesca Liberi, Fabrizio Galadini, Gianluigi Rosatelli, and Maurizio Vassallo
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2016-313, https://doi.org/10.5194/nhess-2016-313, 2016
Manuscript not accepted for further review
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The paper discusses geological aspects, methodological procedures of seismic microzonation and the implications on seismic site response of an urbanized area in a geologic environment of deep continental basin (the Avezzano town in the Fucino continental basin of central Apennines, Italy). The paper is of potential interest for the geological community and also for non-geologist scientists/technicians/decision makers working in the field of earthquake hazard.
F. Masci and G. De Luca
Nat. Hazards Earth Syst. Sci., 13, 1313–1319, https://doi.org/10.5194/nhess-13-1313-2013, https://doi.org/10.5194/nhess-13-1313-2013, 2013
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Regional-scale shear-wave velocity profiles for ground response analyses and uncertainty evaluations – the Piedmont region (northwest Italy) database
Satellite Altimetry-based Extension of global-scale in situ river discharge Measurements (SAEM)
Advancing geodynamic research in Antarctica: reprocessing GNSS data to infer consistent coordinate time series (GIANT-REGAIN)
Capacity Building Enables Unique Near-Fault Observations of the destructive 2025 Mw 7.7 Myanmar Earthquake
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Airborne gravimetry with quantum technology: observations from Iceland and Greenland
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CRA-LICOM: A global high-frequency atmospheric and oceanic temporal gravity field product (2002–2024)
Rescue, Integration, and Analytical Application of historical data from eight pioneering geomagnetic observatories in China
The 2024 Noto Peninsula earthquake building damage dataset: Multi-source visual assessment
GravIS: mass anomaly products from satellite gravimetry
cigFacies: a massive-scale benchmark dataset of seismic facies and its application
GCL-Mascon2024: a novel satellite gravimetry mascon solution using the short-arc approach
Synthetic ground motions in heterogeneous geologies from various sources: the HEMEWS-3D database
HUST-Grace2024: a new GRACE-only gravity field time series based on more than 20 years of satellite geodesy data and a hybrid processing chain
A new repository of electrical resistivity tomography and ground-penetrating radar data from summer 2022 near Ny-Ålesund, Svalbard
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AIUB-GRACE gravity field solutions for G3P: processing strategies and instrument parameterization
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Global Navigation Satellite System (GNSS) time series and velocities about a slowly convergent margin processed on high-performance computing (HPC) clusters: products and robustness evaluation
TRIMS LST: a daily 1 km all-weather land surface temperature dataset for China's landmass and surrounding areas (2000–2022)
Comprehensive data set of in situ hydraulic stimulation experiments for geothermal purposes at the Äspö Hard Rock Laboratory (Sweden)
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Global physics-based database of injection-induced seismicity
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The European Preinstrumental Earthquake Catalogue EPICA, the 1000–1899 catalogue for the European Seismic Hazard Model 2020
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Earth Syst. Sci. Data, 17, 2175–2191, https://doi.org/10.5194/essd-17-2175-2025, https://doi.org/10.5194/essd-17-2175-2025, 2025
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Estimates of earthquake ground motion rely on evaluating soil and rock profiles, with shear-wave velocity (Vs) as a key factor. Uncertainty in Vs impacts seismic hazard predictions. Stochastic procedures model this uncertainty but must be calibrated using detailed geological data and Vs databases. This paper provides a new Vs profile database for Piedmont (northwest Italy), integrating geological modelling and geophysical data and supporting similar studies in other regions.
Peyman Saemian, Omid Elmi, Molly Stroud, Ryan Riggs, Benjamin M. Kitambo, Fabrice Papa, George H. Allen, and Mohammad J. Tourian
Earth Syst. Sci. Data, 17, 2063–2085, https://doi.org/10.5194/essd-17-2063-2025, https://doi.org/10.5194/essd-17-2063-2025, 2025
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Our study addresses the need for better river discharge data, crucial for water management, by expanding global gauge networks with satellite data. We used satellite altimetry to estimate river discharge for over 8700 stations worldwide, filling gaps in existing records. Our data set, SAEM, supports a better understanding of water systems, helping to manage water resources more effectively, especially in regions with limited monitoring infrastructure.
Eric Buchta, Mirko Scheinert, Matt A. King, Terry Wilson, Achraf Koulali, Peter J. Clarke, Demián Gómez, Eric Kendrick, Christoph Knöfel, and Peter Busch
Earth Syst. Sci. Data, 17, 1761–1780, https://doi.org/10.5194/essd-17-1761-2025, https://doi.org/10.5194/essd-17-1761-2025, 2025
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Geodetic GPS measurements in Antarctica have been used to track bedrock displacement, which is vital for understanding geodynamic processes such as plate motion and glacial isostatic adjustment. However, the potential of GPS data has been limited by its partially fragmented availability and unreliable metadata. A new dataset, which spans the period from 1995 to 2021, offers consistently processed coordinate time series for 286 GPS sites and promises to enhance future geodynamic research.
Ssu-Ting Lai, Kyaw Moe Oo, Yin Myo Min Htwe, Tin Yi, Htay Htay Than, Oo Than, Zaw Min, Tun Minn Oo, Phyo Maung Maung, Dino Bindi, Fabrice Cotton, Peter L. Evans, Andres Heinloo, Laura Hillmann, Joachim Saul, Christoph Sens-Schoenfelder, Angelo Strollo, Frederik Tilmann, Graeme Weatherill, Ming-Hsuan Yen, Riccardo Zaccarelli, Thomas Zieke, and Claus Milkereit
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2025-216, https://doi.org/10.5194/essd-2025-216, 2025
Revised manuscript accepted for ESSD
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On March 28, 2025, Myanmar was struck by a destructive Mw 7.7 earthquake. We present detailed information on the data and metadata availability for station NPW, the only local strong-motion station located near the Sagaing Fault that recorded the mainshock without saturation. We also highlight the collaborative effort that made the installation of NPW possible. The high-quality recordings from NPW offer critical insights for seismic hazard assessment in the region.
Li Wei, Dongri Song, Peng Cui, Lijun Su, Gordon G. D. Zhou, Kaiheng Hu, Fangqiang Wei, Yong Hong, Guoqiang Ou, Jun Zhang, Zhicheng Kang, Xiaojun Guo, Wei Zhong, Xiaoyu Li, Yaonan Zhang, and Hui Tang
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2025-190, https://doi.org/10.5194/essd-2025-190, 2025
Revised manuscript accepted for ESSD
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This research presents a unique debris flow dataset over 64 years (1961–2024) at Jiangjia Ravine, Dongchuan, Yunnan, China. The dataset includes detailed measurements of debris-flow kinematic parameters (velocity, depth, discharge), physical-mechanical properties (particle size, yield stress, viscosity), seismic data, and hydrometeorological records (minute-by-minute rainfall, soil moisture, et al.). The dataset is publicly accessible via the National Cryosphere Desert Data Center (NCDC).
Tim Enzlberger Jensen, Bjørnar Dale, Andreas Stokholm, René Forsberg, Alexandre Bresson, Nassim Zahzam, Alexis Bonnin, and Yannick Bidel
Earth Syst. Sci. Data, 17, 1667–1684, https://doi.org/10.5194/essd-17-1667-2025, https://doi.org/10.5194/essd-17-1667-2025, 2025
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The availability of data from two airborne gravity campaigns using sensors based on both classical and quantum technology is presented. Data are made available by the European Space Agency as raw, intermediate, and final data products. Here “raw” refers to the sensor output, while “final” refers to the along-track gravity estimates. This makes the data relevant for users interested in applications ranging from data processing and quantum studies to geophysical studies using gravity observations.
Andrea Tertulliani, Andrea Antonucci, Filippo Bernardini, Viviana Castelli, Emanuela Ercolani, Laura Graziani, Alessandra Maramai, Martina Orlando, Antonio Rossi, and Tiziana Tuvè
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2025-10, https://doi.org/10.5194/essd-2025-10, 2025
Revised manuscript accepted for ESSD
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We present the results of a rapid and reliable study of 45 Italian earthquakes and characterized by datasets with potential inconsistencies or inhomogeneities. The used methodology obviates the need for exhaustive earthquake re-evaluation, and it is particularly effective for the updating of medium-low events, with a large number of low-intensity data. The result is a new dataset very useful to improve “seismic histories” and to contribute to enhance the seismic hazard of an area.
Fan Yang, Jiahui Bai, Hailong Liu, Weihang Zhang, Yi Wu, Shuhao Liu, Chunxiang Shi, Tao Zhang, Min Zhong, Zitong Zhu, Changqing Wang, Ehsan Forootan, Jiangfeng Yu, Zipeng Yu, and Yun Xiao
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2025-81, https://doi.org/10.5194/essd-2025-81, 2025
Revised manuscript accepted for ESSD
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We introduce China’s first de-aliasing computation platform, incorporating China’s Atmospheric Reanalysis and an in-house ocean circulation model. This platform produces CRA-LICOM, a high-frequency atmospheric and oceanic gravity de-aliasing product with a 6-hourly, 50 km resolution covering 2002–2024 globally. This product is reliable for de-aliasing, signal separation in satellite gravity missions, and climate change studies.
Suqin Zhang, Changhua Fu, Jianjun Wang, Chuanhua Chen, Guohao Zhu, Qian Zhao, Jun Chen, Shaopeng He, Bin Wang, Pengkun Guo, Na Deng, Jinghui Lu, and Hongchi Yu
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2025-6, https://doi.org/10.5194/essd-2025-6, 2025
Revised manuscript accepted for ESSD
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The objective of this study is to rescue and integrate historical data from eight pioneering geomagnetic observatories in China. Data quality is significantly improved through integration. The integrated dataset is now publicly available for easy access and use by the academic community and the public. These datasets are of great significance for optimizing historical geomagnetic field models, investigating changing magnetic fields, the main geomagnetic field.
Ruben Vescovo, Bruno Adriano, Sesa Wiguna, Chia Yee Ho, Jorge Morales, Xuanyan Dong, Shin Ishii, Kazuki Wako, Yudai Ezaki, Ayumu Mizutani, Erick Mas, Satoshi Tanaka, and Shunichi Koshimura
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2024-363, https://doi.org/10.5194/essd-2024-363, 2025
Revised manuscript accepted for ESSD
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We compiled an inventory of building condition (destroyed vs. survived) following the 2024 Noto Peninsula Earthquake for the entire affected area, totalling over 140,000 structures. We discuss how we fused freely available data of different types and from different sources to generate the final dataset. We show that our method produces highly accurate results relative to those obtained by on-site surveys. This data can be used to train AI to quickly detect damaged structures in future disasters.
Christoph Dahle, Eva Boergens, Ingo Sasgen, Thorben Döhne, Sven Reißland, Henryk Dobslaw, Volker Klemann, Michael Murböck, Rolf König, Robert Dill, Mike Sips, Ulrike Sylla, Andreas Groh, Martin Horwath, and Frank Flechtner
Earth Syst. Sci. Data, 17, 611–631, https://doi.org/10.5194/essd-17-611-2025, https://doi.org/10.5194/essd-17-611-2025, 2025
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GRACE and GRACE-FO are unique observing systems to quantify mass changes at the Earth’s surface from space. Time series of these mass changes are of high value for various applications, e.g., in hydrology, glaciology, and oceanography. GravIS (Gravity Information Service) provides easy access to user-friendly, regularly updated mass anomaly products. The portal visualizes and describes these data, aiming to highlight their significance for understanding changes in the climate system.
Hui Gao, Xinming Wu, Xiaoming Sun, Mingcai Hou, Hang Gao, Guangyu Wang, and Hanlin Sheng
Earth Syst. Sci. Data, 17, 595–609, https://doi.org/10.5194/essd-17-595-2025, https://doi.org/10.5194/essd-17-595-2025, 2025
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We propose three strategies for field seismic data curation, knowledge-guided synthesization, and generative adversarial network (GAN)-based generation to construct a massive-scale, feature-rich, and high-realism benchmark dataset of seismic facies and evaluate its effectiveness in training a deep-learning model for automatic seismic facies classification.
Zhengwen Yan, Jiangjun Ran, Pavel Ditmar, C. K. Shum, Roland Klees, Patrick Smith, and Xavier Fettweis
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2024-512, https://doi.org/10.5194/essd-2024-512, 2025
Revised manuscript accepted for ESSD
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The Gravity Recovery And Climate Experiment (GRACE) mission has greatly improved our understanding of changes in Earth's gravity field over time. A novel mass concentration (mascon) dataset, GCL-Mascon2024, was determined by leveraging the short-arc approach, advanced spatial constraints, frequency-dependent noise processing strategy, and parameterization integrating natural boundaries, which aims to enhance accuracy for monitoring mass transportation on Earth.
Fanny Lehmann, Filippo Gatti, Michaël Bertin, and Didier Clouteau
Earth Syst. Sci. Data, 16, 3949–3972, https://doi.org/10.5194/essd-16-3949-2024, https://doi.org/10.5194/essd-16-3949-2024, 2024
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Numerical simulations are a promising approach to characterizing the intensity of ground motion in the presence of geological uncertainties. However, the computational cost of 3D simulations can limit their usability. We present the first database of seismic-induced ground motion generated by an earthquake simulator for a collection of 30 000 heterogeneous geologies. The HEMEWS-3D dataset can be helpful for geophysicists, seismologists, and machine learning scientists, among others.
Hao Zhou, Lijun Zheng, Yaozong Li, Xiang Guo, Zebing Zhou, and Zhicai Luo
Earth Syst. Sci. Data, 16, 3261–3281, https://doi.org/10.5194/essd-16-3261-2024, https://doi.org/10.5194/essd-16-3261-2024, 2024
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The satellite gravimetry mission Gravity Recovery and Climate Experiment (GRACE) and its follower GRACE-FO play a vital role in monitoring mass transportation on Earth. Based on the latest observation data derived from GRACE and GRACE-FO and an updated data processing chain, a new monthly temporal gravity field series, HUST-Grace2024, was determined.
Francesca Pace, Andrea Vergnano, Alberto Godio, Gerardo Romano, Luigi Capozzoli, Ilaria Baneschi, Marco Doveri, and Alessandro Santilano
Earth Syst. Sci. Data, 16, 3171–3192, https://doi.org/10.5194/essd-16-3171-2024, https://doi.org/10.5194/essd-16-3171-2024, 2024
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We present the geophysical data set acquired close to Ny-Ålesund (Svalbard islands) for the characterization of glacial and hydrological processes and features. The data have been organized in a repository that includes both raw and processed (filtered) data and some representative results of 2D models of the subsurface. This data set can foster multidisciplinary scientific collaborations among many disciplines: hydrology, glaciology, climatology, geology, geomorphology, etc.
Dino Bindi, Riccardo Zaccarelli, Angelo Strollo, Domenico Di Giacomo, Andres Heinloo, Peter Evans, Fabrice Cotton, and Frederik Tilmann
Earth Syst. Sci. Data, 16, 1733–1745, https://doi.org/10.5194/essd-16-1733-2024, https://doi.org/10.5194/essd-16-1733-2024, 2024
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The size of an earthquake is often described by a single number called the magnitude. Among the possible magnitude scales, the seismic moment (Mw) and the radiated energy (Me) scales are based on physical parameters describing the rupture process. Since these two magnitude scales provide complementary information that can be used for seismic hazard assessment and for seismic risk mitigation, we complement the Mw catalog disseminated by the GEOFON Data Centre with Me values.
Neda Darbeheshti, Martin Lasser, Ulrich Meyer, Daniel Arnold, and Adrian Jäggi
Earth Syst. Sci. Data, 16, 1589–1599, https://doi.org/10.5194/essd-16-1589-2024, https://doi.org/10.5194/essd-16-1589-2024, 2024
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This paper discusses strategies to improve the GRACE gravity field monthly solutions computed at the Astronomical Institute of the University of Bern. We updated the input observations and background models, as well as improving processing strategies in terms of instrument data screening and instrument parameterization.
Athina Peidou, Donald F. Argus, Felix W. Landerer, David N. Wiese, and Matthias Ellmer
Earth Syst. Sci. Data, 16, 1317–1332, https://doi.org/10.5194/essd-16-1317-2024, https://doi.org/10.5194/essd-16-1317-2024, 2024
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This study recommends a framework for preparing and processing vertical land displacements derived from GPS positioning for future integration with Gravity Recovery and Climate Experiment (GRACE) and GRACE-Follow On (GRACE-FO) measurements. We derive GPS estimates that only reflect surface mass signals and evaluate them against GRACE (and GRACE-FO). We also quantify uncertainty of GPS vertical land displacement estimates using various uncertainty quantification methods.
Lavinia Tunini, Andrea Magrin, Giuliana Rossi, and David Zuliani
Earth Syst. Sci. Data, 16, 1083–1106, https://doi.org/10.5194/essd-16-1083-2024, https://doi.org/10.5194/essd-16-1083-2024, 2024
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This study presents 20-year time series of more than 350 GNSS stations located in NE Italy and surroundings, together with the outgoing velocities. An overview of the input data, station information, data processing and solution quality is provided. The documented dataset constitutes a crucial and complete source of information about the deformation of an active but slowly converging margin over the last 2 decades, also contributing to the regional seismic hazard assessment of NE Italy.
Wenbin Tang, Ji Zhou, Jin Ma, Ziwei Wang, Lirong Ding, Xiaodong Zhang, and Xu Zhang
Earth Syst. Sci. Data, 16, 387–419, https://doi.org/10.5194/essd-16-387-2024, https://doi.org/10.5194/essd-16-387-2024, 2024
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This paper reported a daily 1 km all-weather land surface temperature (LST) dataset for Chinese land mass and surrounding areas – TRIMS LST. The results of a comprehensive evaluation show that TRIMS LST has the following special features: the longest time coverage in its class, high image quality, and good accuracy. TRIMS LST has already been released to the scientific community, and a series of its applications have been reported by the literature.
Arno Zang, Peter Niemz, Sebastian von Specht, Günter Zimmermann, Claus Milkereit, Katrin Plenkers, and Gerd Klee
Earth Syst. Sci. Data, 16, 295–310, https://doi.org/10.5194/essd-16-295-2024, https://doi.org/10.5194/essd-16-295-2024, 2024
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We present experimental data collected in 2015 at Äspö Hard Rock Laboratory. We created six cracks in a rock mass by injecting water into a borehole. The cracks were monitored using special sensors to study how the water affected the rock. The goal of the experiment was to figure out how to create a system for generating heat from the rock that is better than what has been done before. The data collected from this experiment are important for future research into generating energy from rocks.
Quetzalcoatl Rodríguez-Pérez and F. Ramón Zúñiga
Earth Syst. Sci. Data, 15, 4781–4801, https://doi.org/10.5194/essd-15-4781-2023, https://doi.org/10.5194/essd-15-4781-2023, 2023
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We present a comprehensive catalog of focal mechanisms for earthquakes in Mexico and neighboring areas spanning February 1928 to July 2022. The catalog comprises a wide range of earthquake magnitudes and depths and includes data from diverse geological environments. We collected and revised focal mechanism data from various sources and methods. The catalog is a valuable resource for future studies on earthquake source mechanisms, tectonics, and seismic hazard in the region.
Iman R. Kivi, Auregan Boyet, Haiqing Wu, Linus Walter, Sara Hanson-Hedgecock, Francesco Parisio, and Victor Vilarrasa
Earth Syst. Sci. Data, 15, 3163–3182, https://doi.org/10.5194/essd-15-3163-2023, https://doi.org/10.5194/essd-15-3163-2023, 2023
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Induced seismicity has posed significant challenges to secure deployment of geo-energy projects. Through a review of published documents, we present a worldwide, multi-physical database of injection-induced seismicity. The database contains information about in situ rock, tectonic and geologic characteristics, operational parameters, and seismicity for various subsurface energy-related activities. The data allow for an improved understanding and management of injection-induced seismicity.
Claudia Finger, Marco P. Roth, Marco Dietl, Aileen Gotowik, Nina Engels, Rebecca M. Harrington, Brigitte Knapmeyer-Endrun, Klaus Reicherter, Thomas Oswald, Thomas Reinsch, and Erik H. Saenger
Earth Syst. Sci. Data, 15, 2655–2666, https://doi.org/10.5194/essd-15-2655-2023, https://doi.org/10.5194/essd-15-2655-2023, 2023
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Passive seismic analyses are a key technology for geothermal projects. The Lower Rhine Embayment, at the western border of North Rhine-Westphalia in Germany, is a geologically complex region with high potential for geothermal exploitation. Here, we report on a passive seismic dataset recorded with 48 seismic stations and a total extent of 20 km. We demonstrate that the network design allows for the application of state-of-the-art seismological methods.
Jia-Hao Li, Zhao-Liang Li, Xiangyang Liu, and Si-Bo Duan
Earth Syst. Sci. Data, 15, 2189–2212, https://doi.org/10.5194/essd-15-2189-2023, https://doi.org/10.5194/essd-15-2189-2023, 2023
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The Advanced Very High Resolution Radiometer (AVHRR) is the only sensor that has the advantages of frequent revisits (twice per day), relatively high spatial resolution (4 km at the nadir), global coverage, and easy access prior to 2000. This study developed a global historical twice-daily LST product for 1981–2021 based on AVHRR GAC data. The product is suitable for detecting and analyzing climate changes over the past 4 decades.
Konstantinos Michailos, György Hetényi, Matteo Scarponi, Josip Stipčević, Irene Bianchi, Luciana Bonatto, Wojciech Czuba, Massimo Di Bona, Aladino Govoni, Katrin Hannemann, Tomasz Janik, Dániel Kalmár, Rainer Kind, Frederik Link, Francesco Pio Lucente, Stephen Monna, Caterina Montuori, Stefan Mroczek, Anne Paul, Claudia Piromallo, Jaroslava Plomerová, Julia Rewers, Simone Salimbeni, Frederik Tilmann, Piotr Środa, Jérôme Vergne, and the AlpArray-PACASE Working Group
Earth Syst. Sci. Data, 15, 2117–2138, https://doi.org/10.5194/essd-15-2117-2023, https://doi.org/10.5194/essd-15-2117-2023, 2023
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We examine the spatial variability of the crustal thickness beneath the broader European Alpine region by using teleseismic earthquake information (receiver functions) on a large amount of seismic waveform data. We compile a new Moho depth map of the broader European Alps and make our results freely available. We anticipate that our results can potentially provide helpful hints for interdisciplinary imaging and numerical modeling studies.
Muhammad Rizwan Asif, Nikolaj Foged, Thue Bording, Jakob Juul Larsen, and Anders Vest Christiansen
Earth Syst. Sci. Data, 15, 1389–1401, https://doi.org/10.5194/essd-15-1389-2023, https://doi.org/10.5194/essd-15-1389-2023, 2023
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To apply a deep learning (DL) algorithm to electromagnetic (EM) methods, subsurface resistivity models and/or the corresponding EM responses are often required. To date, there are no standardized EM datasets, which hinders the progress and evolution of DL methods due to data inconsistency. Therefore, we present a large-scale physics-driven model database of geologically plausible and EM-resolvable subsurface models to incorporate consistency and reliability into DL applications for EM methods.
Médéric Gravelle, Guy Wöppelmann, Kevin Gobron, Zuheir Altamimi, Mikaël Guichard, Thomas Herring, and Paul Rebischung
Earth Syst. Sci. Data, 15, 497–509, https://doi.org/10.5194/essd-15-497-2023, https://doi.org/10.5194/essd-15-497-2023, 2023
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We produced a reanalysis of GNSS data near tide gauges worldwide within the International GNSS Service. It implements advances in data modelling and corrections, extending the record length by about 7 years. A 28 % reduction in station velocity uncertainties is achieved over the previous solution. These estimates of vertical land motion at the coast supplement data from satellite altimetry or tide gauges for an improved understanding of sea level changes and their impacts along coastal areas.
Michal Kruszewski, Gerd Klee, Thomas Niederhuber, and Oliver Heidbach
Earth Syst. Sci. Data, 14, 5367–5385, https://doi.org/10.5194/essd-14-5367-2022, https://doi.org/10.5194/essd-14-5367-2022, 2022
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The authors assemble an in situ stress magnitude and orientation database based on 429 hydrofracturing tests that were carried out in six coal mines and two coal bed methane boreholes between 1986 and 1995 within the greater Ruhr region (Germany). Our study summarises the results of the extensive in situ stress test campaign and assigns quality to each data record using the established quality ranking schemes of the World Stress Map project.
Andrea Rovida, Andrea Antonucci, and Mario Locati
Earth Syst. Sci. Data, 14, 5213–5231, https://doi.org/10.5194/essd-14-5213-2022, https://doi.org/10.5194/essd-14-5213-2022, 2022
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EPICA is the 1000–1899 catalogue compiled for the European Seismic Hazard Model 2020 and contains 5703 earthquakes with Mw ≥ 4.0. It relies on the data of the European Archive of Historical Earthquake Data (AHEAD), both macroseismic intensities from historical seismological studies and parameters from regional catalogues. For each earthquake, the most representative datasets were selected and processed in order to derive harmonised parameters, both from intensity data and parametric catalogues.
Suqin Zhang, Changhua Fu, Jianjun Wang, Guohao Zhu, Chuanhua Chen, Shaopeng He, Pengkun Guo, and Guoping Chang
Earth Syst. Sci. Data, 14, 5195–5212, https://doi.org/10.5194/essd-14-5195-2022, https://doi.org/10.5194/essd-14-5195-2022, 2022
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The Sheshan observatory has nearly 150 years of observation history, and its observation data have important scientific value. However, with time, these precious historical data face the risk of damage and loss. We have carried out a series of rescues on the historical data of the Sheshan observatory. New historical datasets were released, including the quality-controlled absolute hourly mean values of three components (D, H, and Z) from 1933 to 2019.
Guoyu Li, Wei Ma, Fei Wang, Huijun Jin, Alexander Fedorov, Dun Chen, Gang Wu, Yapeng Cao, Yu Zhou, Yanhu Mu, Yuncheng Mao, Jun Zhang, Kai Gao, Xiaoying Jin, Ruixia He, Xinyu Li, and Yan Li
Earth Syst. Sci. Data, 14, 5093–5110, https://doi.org/10.5194/essd-14-5093-2022, https://doi.org/10.5194/essd-14-5093-2022, 2022
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A permafrost monitoring network was established along the China–Russia crude oil pipeline (CRCOP) route at the eastern flank of the northern Da Xing'anling Mountains in Northeast China. The resulting datasets fill the gaps in the spatial coverage of mid-latitude mountain permafrost databases. Results show that permafrost warming has been extensively observed along the CRCOP route, and local disturbances triggered by the CRCOPs have resulted in significant permafrost thawing.
Alessandro Cicoira, Samuel Weber, Andreas Biri, Ben Buchli, Reynald Delaloye, Reto Da Forno, Isabelle Gärtner-Roer, Stephan Gruber, Tonio Gsell, Andreas Hasler, Roman Lim, Philippe Limpach, Raphael Mayoraz, Matthias Meyer, Jeannette Noetzli, Marcia Phillips, Eric Pointner, Hugo Raetzo, Cristian Scapozza, Tazio Strozzi, Lothar Thiele, Andreas Vieli, Daniel Vonder Mühll, Vanessa Wirz, and Jan Beutel
Earth Syst. Sci. Data, 14, 5061–5091, https://doi.org/10.5194/essd-14-5061-2022, https://doi.org/10.5194/essd-14-5061-2022, 2022
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This paper documents a monitoring network of 54 positions, located on different periglacial landforms in the Swiss Alps: rock glaciers, landslides, and steep rock walls. The data serve basic research but also decision-making and mitigation of natural hazards. It is the largest dataset of its kind, comprising over 209 000 daily positions and additional weather data.
Xiaoli Chang, Huijun Jin, Ruixia He, Yanlin Zhang, Xiaoying Li, Xiaoying Jin, and Guoyu Li
Earth Syst. Sci. Data, 14, 3947–3959, https://doi.org/10.5194/essd-14-3947-2022, https://doi.org/10.5194/essd-14-3947-2022, 2022
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Based on 10-year observations of ground temperatures in seven deep boreholes in Gen’he, Mangui, and Yituli’he, a wide range of mean annual ground temperatures at the depth of 20 m (−2.83 to −0.49 ℃) and that of annual maximum thawing depth (about 1.1 to 7.0 m) have been revealed. This study demonstrates that most trajectories of permafrost changes in Northeast China are ground warming and permafrost degradation, except that the shallow permafrost is cooling in Yituli’he.
Alice C. Frémand, Julien A. Bodart, Tom A. Jordan, Fausto Ferraccioli, Carl Robinson, Hugh F. J. Corr, Helen J. Peat, Robert G. Bingham, and David G. Vaughan
Earth Syst. Sci. Data, 14, 3379–3410, https://doi.org/10.5194/essd-14-3379-2022, https://doi.org/10.5194/essd-14-3379-2022, 2022
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This paper presents the release of large swaths of airborne geophysical data (including gravity, magnetics, and radar) acquired between 1994 and 2020 over Antarctica by the British Antarctic Survey. These include a total of 64 datasets from 24 different surveys, amounting to >30 % of coverage over the Antarctic Ice Sheet. This paper discusses how these data were acquired and processed and presents the methods used to standardize and publish the data in an interactive and reproducible manner.
Cited articles
Agostini, A., Tofani, V., Nolesini, T., Gigli, G., Tanteri, L., Rosi, A., Cardellini, S., and Casagli, N.: A new appraisal of the Ancona landslide based on geotechnical investigations and stability modelling, Q. J. Eng. Geol. Hydroge., 47, 29–43, https://doi.org/10.1144/qjegh2013-028, 2014.
Akazawa, T.: A technique for automatic detection of onset time of P-and S-phases in strong motion records, 13th World Conference on Earthquake Engineering, Vancouver, Canada, 1–6 August 2004, https://www.iitk.ac.in/nicee/wcee/article/13_786.pdf (last access: 1 May 2025), 2004.
Albarello, D., Pacitti, P., Schiaroli, A., Tiberi, P., Fantozzi, P. L., Pieruccini, P., and Madiai, C.: La microzonazione sismica delle Marche. 10 anni di attività, Regione Marche, ISBN 978-88-95554-40-2, https://hdl.handle.net/2158/1325073 (last access: 1 May 2025), 2022.
Amanti, M., Battaglini, L., Campo, V., Cipolloni, C., Congi, M. P., Conte, G., Delogu, D., Ventura, R., and Zonetti, C.: La carta litologica d'italia alla scala 1:100000, in: Atti della 11a Conferenza Nazionale ASITA, Turin, Italy, 6–9 November 2007, http://atti.asita.it/Asita2007/Pdf/119.pdf (last access: 1 May 2025), 2007.
Bally, A. W., Burbi, L., Cooper, C., and Ghelardoni, R.: Balanced sections and seismic reflection profiles across the central Apennines, Mem. Soc. Geol. It., 35, 257–310, 1986.
Beyreuther, M., Barsch, R., Krischer, L., Megies, T., Behr, Y., and Wassermann, J.: ObsPy: A Python Toolbox for Seismology, Seismol. Res. Lett., 81, 530–533, https://doi.org/10.1785/gssrl.81.3.530, 2010
Bonamassa, O. and Vidale, J. E.: Directional site resonances observed from aftershocks of the 18 October 1989 Loma Prieta earthquake sequence, B. Seismol. Soc. Am., 81, 1945–1958, https://www.researchgate.net/publication/241436761_Directional_site_resonances_observed_from_aftershocks_of_the_18_October_1989_Loma_Prieta_earthquake (last access: 1 May 2025), 1991.
Borcherdt, R. D.: Effects of local geology on ground motion near San Francisco Bay, B. Seismol. Soc. Am., 60, 29–61, https://www.researchgate.net/publication/277995526_Effects_of_local_geology_on_ground_motion_near_San_Francisco_Bay (last access: 1 May 2025), 1970.
Calza, W., Maistrello, M., Marcellini, A., Morganti, C., Rampoldi, R., Rossi, B., Stucchi M., and Zonno, G.: Elementi di microzonazione dell'area anconetana, Pubbl. Prog. Final. Geodin., 430, 68 pp., 1981.
Cancelli, A., Marabini, F., Pellegrini, M., and Tonnetti, G.: Incidenze delle frane sull'evoluzione della costa adriatica da Pesaro a Vasto, Memorie della Società Geologica Italiana, 27, 555–568, 1984.
Cara, F. and Famiani, D.: Horizontal to vertical spectral ratios (HVNSR) on ambient noise recordings of stations of the 6N network during the activities of the EMERSITO INGV emergency group in Ancona (Italy) following the 2022 MW 5.5 Costa Marchigiana-Pesarese earthquake, Zenodo [data set], https://doi.org/10.5281/zenodo.14704661, 2025a.
Cara, F. and Famiani, D.: Horizontal to vertical spectral ratios (HVSR) on earthquake recordings of stations of the 6N network during the activities of the EMERSITO INGV emergency group in Ancona (Italy) following the 2022 MW 5.5 Costa Marchigiana-Pesarese earthquake, Zenodo [data set], https://doi.org/10.5281/zenodo.14672464, 2025b.
Cara, F. and Famiani, D.: Standard spectral ratios (SSR) on earthquake recordings of stations of the 6N network during the activities of the EMERSITO INGV emergency group in Ancona (Italy) following the 2022 MW 5.5 Costa Marchigiana-Pesarese earthquake, Zenodo [data set], https://doi.org/10.5281/zenodo.14672943, 2025c.
Cara, F., Di Giulio, G., Cavinato, G. P., Famiani, D., and Milana, G.: Seismic characterization and monitoring of Fucino Basin (Central Italy), B. Earthq. Eng., 9, 1961–1985, https://doi.org/10.1007/s10518-011-9282-2, 2011.
Cara, F., Cultrera, G., Riccio, G., Amoroso, S., Bordoni, P., Bucci, A., D'Alema, E., D'Amico, M., Cantore, L., Carannante, S., Cogliano, R., Di Giulio, G., Di Naccio, D., Famiani, D., Felicetta, C., Fodarella, A., Franceschina, G., Lanzano, G., Lovati, S., Luzi, L., Mascandola, C., Massa, M., Mercuri, A., Milana, G., Pacor, F., Piccarreda, D., Pischiutta, M., Pucillo, S., Puglia, R., Vassallo, M., Boniolo, G., Caielli, G., Corsi, A., de Franco, R., Tento, A., Bongiovanni, G., Hailemikael, S., Martini, G., Paciello, A., Peloso, A., Poggi, F., Verrubbi, V., Gallipoli, M. R., Stabile T. A., and Mancini, M.: Temporary dense seismic network during the 2016 Central Italy seismic emergency for microzonation studies, Sci. Data, 6, 182, https://doi.org/10.1038/s41597-019-0188-1, 2019.
Cara, F., Di Giulio, G., Cultrera, G., Lovati, S., Pacor, F., Riccio, G., Vassallo, M., Bagh, S., Bobbio, A., Bottari, C., Brunelli, G., Ciaccio, M. G., Cogliano, R., Costanzo, A., D'Alessandro, A., D'Ambrosio, M., D'Amico, V., De Luca, G., Di Filippo, A., Falco, L., Falcone, S., Famiani, D., Felicetta, C., Fodarella, A., Grassa, F., Hailemikael, S., La Piana, C., Liguoro, F., Colasanti, M., Mascandola, C., Massa, M., Mele, G., Melillo, G., Memmolo, A., Mercuri, A., Milana, G., Minarelli, L., Morelli, R. S., Nardone, L., Pagliuca, N., Paratore, M., Pischiutta, M., Pucillo, S., Puglia, R., Pulvirenti, M. S., Scudero, S., Sgattoni, G., Somma, R., Tarabusi, G., Tusa, G., Vitale, G., Zarrilli, L., and Amoroso, S.: Gruppo Operativo EMERSITO-Evento sismico Costa Marchigiana 2022, Rapporto N. 1 del 09/11/2022, https://www.earth-prints.org/handle/2122/15783 (last access: 1 May 2025), 2022a (in Italian).
Cara, F., Di Giulio, G., Cultrera, G., Pacor, F., Lovati, S., Riccio, G., Vassallo, M., Bobbio, A., Bottari, C., Brunelli, G., Cogliano, R., De Luca, G., Di Filippo, A., Falco, L., Famiani, D., Felicetta, C., Fodarella, A., Hailemikael, S., Mascandola, C., Massa, M., Memmolo, A., Mercuri, A., Milana, G., Minarelli, L., Nardone, L., Pischiutta, M., Pucillo, S., Puglia, R., Sgattoni, G., and Tarabusi, G.: Gruppo Operativo EMERSITO-Evento sismico Costa Marchigiana 2022, Rapporto N. 2 del 13/11/2022, https://www.earth-prints.org/handle/2122/15785 (last accesS: 1 May 2025), 2022b (in Italian).
Cara, F., Di Giulio, G., Cultrera, G., Pacor, F., Lovati, S., Riccio, G., Vassallo, M., Bobbio, A., Bottari, C., Brunelli, G., Cogliano, R., De Luca, G., Di Filippo, A., Falco, L., Famiani, D., Felicetta, C., Fodarella, A., Hailemikael, S., Mascandola, C., Massa, M., Memmolo, A., Mercuri, A., Milana, G., Minarelli, L., Nardone, L., Pischiutta, M., Pucillo, S., Puglia, R., Sgattoni, G., and Tarabusi, G.: Rapporto n. 3 attività del gruppo operativo emersito a seguito dell'evento sismico Costa Marchigiana Pesarese Mw 5.5 del 9/11/2022, https://www.earth-prints.org/handle/2122/15795 (last access: 1 May 2025), 2022c (in Italian).
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Short summary
This paper describes data and preliminary analyses made by the Istituto Nazionale di Geofisica e Vulcanologia (INGV) emergency task force EMERSITO, devoted to site effects and seismic microzonation studies, following the 9 November 2022 strong earthquake localized in the Adriatic Sea (Italy). Considering the affected area, EMERSITO deployed, from November 2022 to February 2023, a temporary seismic network of 11 stations (net code 6N) which sampled different geological units in the urban area of Ancona.
This paper describes data and preliminary analyses made by the Istituto Nazionale di Geofisica e...
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