SEARCHING: IASPEI
S01 Observational Seismology - Open Session
Convener(s): Torsten Dahm (Germany)Co-Convener(s): Domenico Di Giacomo (UK) Johannes Schweitzer (Norway)
Description
The Commission on Seismological Observation and Interpretation (CoSOI) covers a broad spectrum of observational and theoretical seismology, and organises and coordinates several topic-oriented symposia to focus discussions and presentations. The open session in CoSOI provides space for any topics not already covered in the focused symposia. We invite presentations from all areas of CoSOI, including new developments for integrating non-seismological data into seismic observations. This year, it is also a forum for the presentation and discussion of methods for standardisation and automation of (near real-time) seismic data processing and interpretation including all CTBT related topics.
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S02 International, National, Regional and Local Networks and Earthquake Data Centers: Highlights and Challenges
Convener(s): Dmitry Storchak (UK)Co-Convener(s): Kristin Pankow (USA)
Description
National and regional seismic operation centers play an important role in monitoring for natural earthquakes, volcanic eruptions, and other phenomena, such as induced seismicity. The products generated by these centers, from raw waveforms to earthquake catalogs are used by a wide variety of stakeholders, including researchers, emergency management agencies, policy makers, educators, regulators, and the general public. This session focuses on the important role that earthquake centers play in advancing scientific study, especially as it relates to local and regional hazard; integrating new technological advances in data acquisition and processing; and communicating earthquake hazard and risk. We welcome contributions describing new and evolving networks, data policies and data sharing, new processing algorithms, hazard assessments, and novel education and outreach initiatives. Other topics that highlight current advances and challenges for earthquake operation centers are also of interest. Potential outcomes of the session may include summary publications, organized advocacy, and frameworks for closer collaboration.
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S03 Seismic Scattering and Absorption, Ambient Noise, and Monitoring Earth's Structure
Convener(s): Hisashi Nakahara (Japan)Co-Convener(s): Ulrich Wegler (Germany) Ludovic Margerin (France)
Description
Seismic scattered waves or coda waves carry rich information on heterogeneities within the Earth. Amplitude information from coda waves has been used to estimate the spatial distribution and the frequency dependence of the strength of scattering attenuation and intrinsic absorption in the Earth. Recently, ambient noise cross-correlation has also been used to study seismic structure in the Earth thanks to the development of seismic interferometry. Time-lapse imaging or monitoring of the Earth has been conducted using tiny changes in phase information of cross-correlation functions of ambient noise and coda waves. Increasing the spatial and temporal resolutions of the imaging will help to understand the Earth's heterogeneities and dynamics. In this session, we would like to widely invite presentations related to theoretical and observational studies of attenuation, coda waves, ambient noise, and their applications to the imaging and monitoring Earth’s heterogeneous structure.
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S04 Advancements in Acquisition, Processing and Interpretation of Seismological Data
Convener(s): Francesco Grigoli (Italy)Co-Convener(s): Mostafa Mousavi (USA) Aitaro Kato (Japan)
Description
Observational seismology is currently undergoing a revolution both concerning new types of instruments and processing paradigms. Distributed Acoustic Sensing (DAS) and Large-N nodal arrays, in combination with classical seismological instruments, led to a dramatic increase in the volume of available seismic data. On one hand, this data explosion gives us the possibility to further advance our understanding of tectonic and earthquake processes but, on the other hand, it highlights the limits of the current standard routine seismic analysis, often performed manually by seismologists. The combination of big datasets, new monitoring instrumentations, and novel processing methods, including improvements in rapid communication of scientific results, are leading to breakthroughs in many fields of seismology. For instance, machine-learning-based methods for seismic data analysis are now able to detect at least 10x the number of earthquakes as current operational best practice and reduce the magnitude of completeness by a full magnitude unit, revealing hidden patterns associated with the earthquake generation processes. Waveform-based methods have also grown in popularity and their extensive application is dramatically improving our capability to characterize seismicity in near real-time. Such techniques are particularly useful when working with data sets characterized by large numbers of weak events, with low signal-to-noise ratios, such as those collected in induced seismicity, seismic swarms, and volcanic monitoring operations. However, the results of these automatized processing approaches may have errors when their uncertainties are not carefully evaluated, suggesting future research focus directions. This session aims to bring to light new methods that can be applied to large data sets, either retroactively or in (near) real-time, to characterize seismicity (i.e., perform detection, location, magnitude, and source mechanisms estimation) at different scales and in different environments. We thus encourage contributions that demonstrate how the proposed methods help improve our understanding of the earthquake processes or seismic monitoring operations.
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S05 Advances in Earthquake and Explosion Monitoring Using Distributed Acoustic Sensing
Convener(s): Ben Dando (Norway)Co-Convener(s): Verónica Rodríguez Tribaldos (Germany) Meghan Miller (Australia) Herb Wang (USA)
Description
Distributed acoustic sensing has grown into an exciting topic within observational seismology over the last decade. The flexibility of how and where a fibre optic cable can be deployed provides significant opportunities for both novel network designs and a large range of monitoring and sensing applications. Despite this growth in interest, we are still, as a community, trying to understand both what the current limitations are and how far we can push these limits. Fundamental differences exist between DAS measurements and traditional seismometers. DAS measures strain or strain rate whereas seismometers measure particle velocity. Furthermore, DAS measures deformation at metre-scale and only in the direction of the cable whereas seismometers provide single-point measurements but in three orthogonal directions. While the differences in physical measurements require adaptation to extract meaningful signal characteristics, the continuous spatial measurements provide new opportunities for novel signal processing techniques that can take advantage of the vast quantities of data that are recorded. Existing DAS networks include fibre-optic cable buried in shallow trenches or vertical boreholes, cable deployed to emulate traditional seismic arrays, and the repurposing of telecommunication fibre and underwater cables for seismological applications. These networks have been used to demonstrate the potential for earthquake early warning, studies of Earth structure, seismic source analysis, global earthquake monitoring and explosion monitoring. Differences in cable construction and cable deployment can produce differences in the recorded signal. In this symposium we wish to encourage contributions that showcase how DAS can be best used and developed for enhancing seismological analyses relevant to earthquake and explosion monitoring. We are interested in novel methods, applications, networks, and case studies that can enrich our understanding of the topic.
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S06 Pre-Instrumental Earthquake Data
Convener(s): Paola Albini (Italy)Co-Convener(s): Kenji Satake (Japan)
Description
Evidence of global seismic activity from instrumental records covers about one century, too short a period to catch the recurrence interval of large earthquakes. Historical seismological studies and macroseismic intensity data have significantly expanded backwards in time our knowledge of the seismic behaviour of many areas in the world. Paleoseismological studies of inland active faults, as well as coastal geological studies on tsunami deposits or marine terraces, and marine geological studies on deep-ocean turbidites, have provided important information for the past occurrence of pre-instrumental earthquakes, too. The combination of data deriving from these three domains would result in a better vision of the long-term seismicity, which may be utilized for long-term forecast. However, challenges are still posed to researchers on how to best derive earthquake parameters from originally non-seismological observations of earthquake effects, as it is the case of both macroseismic and geological data. This session welcomes contributions suggesting new prospects related to these topics, such as case studies of historical and paleoseismological records, their unfiltered association to specific events as well as their usual parameterization in seismological terms, or their combination with modern instrumental data, or any further issue on long-term seismicity analysis and forecast of moderate and especially of large earthquakes.
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S07 Scientific Drilling and Downhole Monitoring – A Key to Understand Geohazards
Convener(s): Harold Tobin (USA)Co-Convener(s): Sukanta Roy (India) Kuo-Fong Ma (Taiwan) Patricia Martínez-Garzón (Germany) Thomas Wiersberg (Germany)
Description
Solid-earth geohazards such as earthquakes, volcanoes, and mass movements pose an ever-increasing threat to humankind. They occur on very different time and space scales, strongly depend on local geological conditions, and often involve only little signals, making each one of them challenging to assess, study, and forecast. It is of utmost relevance to decipher their underlying causes and the physical processes that drive them, to understand the full chain from hazard to risk. Shallow and deep scientific drilling is the ultimate method to gain in-situ data and retrieve uncompromised samples from the underground to calibrate models derived from surface studies or modeling. Boreholes provide unique access into the near-field source regions of geohazards and provide conditions for sampling and observing the system, which are not attainable at the Earth’s surface. Downhole monitoring is less influenced by environmental fluctuations close to the surface and near-surface geological structures. In last decades downhole monitoring techniques steadily improved and new sensor systems and approaches were developed. This session aims to provide an overview about state-of-the-art developments in the field of scientific drilling, sampling and monitoring in oceans and on continents to better understand and ultimately mitigate Geohazard associated risk. A focus will be on downhole monitoring and sampling, but we also welcome contributions on site surveys, drilling and logging techniques, coring, borehole testing and experiments, and modelling.
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S08 Anthropogenic Seismicity
Convener(s): Stanislaw Lasocki (Poland)Co-Convener(s): Thomas H. Goebel (USA) Haijiang Zhang (China) Beata Orlecka-Sikora (Poland) Harsh Gupta (India)
Description
Technological activities such as the creation of artificial water reservoirs, underground and open-pit mining, extraction of hydrocarbons, geothermal energy production, etc., are known to have triggered/induced earthquakes under favorable geological conditions. The socio-economic impact of seismicity induced/triggered by geo-resource exploitation is immense. Stronger anthropogenic earthquakes can cause damage, injuries, and even fatalities. Such earthquakes exceeding magnitude 5 occurred in connection with underground mining in South Africa and India, conventional and unconventional hydrocarbon exploitation in the USA, Russia, China, and elsewhere, and geothermal energy production in South Korea. There were even anthropogenic earthquakes of magnitude 6+, including the M6.3 reservoir-triggered earthquake at Koyna, India, in 1967 and the M7.5 one triggered by conventional hydrocarbon exploitation in Neftogorsk, Russia, in 1995. A proper understanding of the factors and situations conducive to such earthquakes is crucial. We invite to this session the contributions that present case histories, elucidate the genesis of such events, and provide methodologies to mitigate and manage the anthropogenic seismic hazard.
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S09 Earthquake Ground Motion and Seismic Hazard
Convener(s): Fabrice Cotton (Germany)Co-Convener(s): Trevor Allen (Australia) Dino Bindi (Germany) Carlo Cauzzi (Switzerland) Kuo-Fong Ma (Taiwan) Hiroe Miyake (Japan) Eric Thompson (USA)
Description
The aim of this session is to provide a comprehensive overview of state-of-the-art as well as innovative ideas and methods using the latest generation of open ground-motion datasets, data-mining analysis, HPC to evaluate strong ground motion and assess seismic hazard. We invite contributions related to:
(1) The estimation of earthquake ground motions and associated uncertainties (aleatoric and epistemic)
(2) Analysis of regional dependencies of source, path and site properties and their impact on ground motions and seismic hazard
(3) Assessment of ‘complex’ site effects (e.g. 2D/3D effects, non-linear effects, time dependencies), near-surface interactions, soil-structure interactions, ‘secondary’ hazards (e.g., earthquake induced mass movements, liquefaction, etc.)
(4) Characterization of near-source ground motion and assessment of source effects (e.g. pulses, directivity, fling step, etc.)
(5) New candidate parameters to characterize and model the shaking intensity
(6) Site-specific and ultra-high-density earthquake ground-motion modelling (e.g. non-ergodic ground-motion models, use of machine learning in engineering seismology)
(7) Improvement of current empirical ground-motion models by integrating physics-based models and waveforms
(8) Rapid characterization of event properties and rapid (urgent computing mode) ground shaking maps after a significant event employing instrumental and community-based intensity measures
(9) Transparent and innovative methods of testing and visualizing ground-motion and hazard models
(10) New instrumental ground-motion and macroseismic intensity datasets to complement and expand existing datasets.
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S10 Multi-Hazard Risk Assessment
Convener(s): Katsuichiro Goda (Canada)Co-Convener(s): Chen Huang (Norway)
Description
Natural hazards are a significant threat to the lives and livelihoods worldwide and result in catastrophic destruction and damage, which call for enhanced capacities in risk and resilience management and governance. The multi-hazard risk assessments provide a comprehensive analysis of the impact of multiple hazards for emergency responders, planning authorities, as well as scientific and industrial communities. Moreover, the communication of multi-hazard risks to citizens will enhance their understanding and thus raise the resilience of society. This session aims to share scientific advances in quantifying the multi-hazard risks, including: multi-hazard modelling considering the hazard interactions in space and time; multi-vulnerability assessment considering the interconnection and dynamics of physical exposure and social characteristics; multi-hazard exposure characterization considering the spatial and temporal evolution; multi-hazard and multi-risk decision support systems; and other theoretical, methodological and practical developments regarding the multi-hazard risk assessment. Furthermore, contributions related to the communication, cooperation, coordination and collaboration in multi-hazard disaster management, multi-risk reduction strategies, and emergency response management, are also welcomed.
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S11 Site Response in Urban Areas
Convener(s): Stefano Parolai (Italy)Co-Convener(s): Roberto Paolucci (Italy) Philippe Gueguen (France)
Description
The assessment of site effects is necessary for improved and reliable on-site seismic hazard and risk assessment. During the last decades, methods and tools have been developed to estimate both directly, using earthquake recordings, and indirectly , through active and passive investigation the site response. Large efforts have been dedicated in particular to the development of ad-hoc methods in urban areas, where the logistic of the experiments, and the anthropogenic disturbance might limit the capabilities of investigation. Recently, newly developed passive investigations, better exploiting the potential of seismic noise signals, the improved capabilities of numerical simulations, and the availability of new technologies of monitoring systems are allowing to amazingly improve the spatial resolution of the site response and to consider also the interaction of the building (city) structures with the soil. This symposium aims at providing an overview on the state of the art on site response analysis in urban areas with particular focus on innovative methodologies and tools. Studies including the usage of leading edge technogical equipment and the integration of multidisciplinary data are particularly welcome.
Solicited speaker: Alan Yong (US Geological Survey, USA)
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S12 Recent Devastating Earthquakes Including the Feb. 6, 2023 Turkey Sequence
Convener(s): Kenji Satake (Japan)Co-Convener(s): Thorne Lay (USA) Dmitry Storchak (UK) Li Li (China)
Description
Since the last IUGG General Assembly in July 2019, large, damaging earthquakes continue to strike globally, producing loss of life and destruction in many regions around the world. About 34 earthquakes with Mw ≥ 7 (NEIC/GCMT) have occurred globally as of August 30, 2022. Three great Mw~8+ earthquakes (GCMT) occurred in 2021: Kermadec Islands (March 4, Mw 8.1), Alaska (July 29, Mw 8.2), and South Sandwich Islands (August 12, Mw 8.3), with 16 more earthquakes in the world of Mw ≥ 7 that year. In terms of earthquake damage, the Haiti earthquake on August 14, 2021 (Mw 7.2) caused more than 2,000 casualties and the Afghanistan earthquake on June 22, 2022 (Mw 6.0) caused more than 1,000 casualties. Earthquake science is essential for revealing the nature of earthquake generation and for extracting lessons from these events to help society reduce the impacts of future events. Seismologists, Geodesists, Geologists and Tsunami experts have been cooperating to characterize the full earthquake cycle and to image the rupture process of earthquakes with steadily improving resolution. This session welcomes reports on all studies of recent large and/or devastating earthquakes with geodetic/seismological/tsunami techniques, including investigations of source process, slip distribution, damage, pre/co/post-seismic deformation, geological/geophysical structure around the source faults, tectonic implications, and other associated phenomena.
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S13 Development, Testing and Application of Earthquake Forecasting Models
Convener(s): Annemarie Christophersen (New Zealand)Co-Convener(s): Eleftheria Papadimitriou (Greece) Sebastian Hainzl (Germany) Jiangang Zhuang (Japan) Andrea Llenos (USA) Rodolfo Console (Italy)
Description
Contributions are invited on all aspects of developing, testing, and applying models that are designed to forecast earthquake occurrence in time and/or space. The development of earthquake forecasting models is being facilitated by the improvement of data, modeling inputs and new methods. Modeling efforts are welcome that focus on the short–term clustering of earthquakes, the time-varying probability of rupture of major fault sources, and the space-time-magnitude variation of the rate of earthquake occurrence in extended regions. Models can be statistical, physics-based, or machine learned. Data inputs include the past earthquake catalog, known or inferred dates of previous fault ruptures, modeled physical variables such as stress-accumulation and strain rates, and proposed precursory phenomena. Testability is an important issue. Thus, studies concerning formal performance testing of competing models and improved testing methods are also invited, as well as reports on the application of forecasts to inform the public or in support of planning earthquake countermeasures.
Solicited speakers: Maximilian Werner (University of Bristol, UK), Andrea Llenos (United State Geological Survey, Geologic Hazards Science Center, USA)
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S14 New Advances in Understanding the Earth's Crust Dynamics in the Light of Solving the Problem of Earthquake Forecasting
Convener(s): Sergey Pulinets (Russia)Co-Convener(s): Vladimir Kossobokov (Russia)
Description
Recent theoretical advances demonstrate that the activity of the faults on a global scale is more interconnected than previously considered. Calculation of the fault’s interactions based on the past earthquake catalogs within the Cosserat continuum theory demonstrates a presence of slow tectonic waves acting as triggers of earthquakes in the unstable zones encountered on their way. Simultaneously the calculated global shear traction distribution reflects the position of unstable seismically active tectonic zones. The unstable zones can also be detected by an increased degassing of the Earth’s crust. The radon proxy in the form of the atmospheric chemical potential demonstrates a high correlation with the shear traction changes, confirming the validity of the model based on the Cosserat continuum. The Symposium will collect the papers demonstrating the recent results on the global seismic activity distribution, technologies directed to the unstable zones detection including the b-value dynamics, geochemical measurements, and atmospheric effects at the final stage of the earthquake preparation cycle.
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S15 Boundary Layers in Earth’s Mantle: Origin, Structure, and Influence on Convection
Convener(s): Morvarid Saki (Germany)Co-Convener(s): Lauren Waszek (Australia) Rashni Anandawansha (USA)
Description
Earth’s mantle comprises numerous seismic discontinuities at multiple depths from the upper mantle down to the core-mantle boundary, arising as a consequence of mineral physics phase transitions or thermochemical variations. Some of these boundary layers act to impede or promote convection at global or regional scales. Thus, mapping the detailed properties of their structures offers key insight into heat and material flux throughout the whole mantle, with implications for global geodynamical processes and geochemical reservoirs. Over the last few decades, seismological studies have resulted in significantly improvements in direct observations of boundary layers in the mantle across both global and regional scales. However, the origins (thermal, chemical) of some of these features are still debated. Combining seismic observations with further constraints from mineral physics, geochemistry, and geodynamics provides important clues on composition, temperature, and dynamic processes associated with these discontinuities. This session aims to bring together scientists from different Seismological disciplines to better understanding the structure, composition, and influence of boundary layers in the Earth’s mantle, from the mantle transition zone down to the core mantle boundary. We particularly welcome multidisciplinary submissions, with an overarching goal to image the chemical evolution of Earth's interior, as well as the mechanisms affecting global circulation.
Solicited speakers: Laura Cobden (University of Utrecht, Netherlands), Stuart Russell (University of Cambridge, UK)
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S16 Earthquake Source Mechanics
Convener(s): Satoshi Ide (Japan)Co-Convener(s): Simone Cesca (Germany) Keisuke Ariyoshi (Japan) Daniela Kühn (Norway) Germán Prieto (Colombia) Seok Song (South Korea)
Description
Recent high-quality seismic and geodetic observations provide large data volumes, which enable accurate determination of earthquake source parameters (locations, magnitudes, durations, moment tensors, etc.) and detailed imaging of spatio-temporal deformation processes. Further, techniques for extracting information using inverse problems and machine/deep learning techniques have improved substantially. Abundant information from these analyses is the basis for studying a variety of earthquakes to seek the governing laws and conditions for their initiation, growth, and arrest. In addition to traditional earthquakes including foreshocks, aftershocks, swarms, repeaters, volcanic and induced events, we now observe various slow earthquakes such as tectonic tremors, low-frequency earthquakes, and slow slip events. The stress state, fault geometry, and fluid movement around seismogenic regions are also important issues. The latest high-performance computing can numerically simulate the entire earthquake process from long-term tectonic loading and slow nucleation to rapid rupture propagation with strong motion radiation. The validity of assumptions in these simulations is tested by data analysis, data assimilation, laboratory experiments, and field observations including several drilling projects. In this symposium, we invite contributions on data analysis and interpretation of earthquake source mechanics, on improvement and validation of analysis techniques, on theoretical and numerical modeling of dynamic ruptures and earthquake sequences, and observational and experimental studies on the physics of earthquakes.
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S17 Structure and evolution of the lithosphere in the circum-Mediterranean
Convener(s): Thomas Meier (Germany)Co-Convener(s): Claudio Faccenna (Italy) Claudia Piromallo (Italy) Enrico Serpelloni (Italy) Josip Stipčević (Croatia)
Description
The tectonic evolution in the circum-Mediterranean has been shaped by a fascinating complexity of oceanic subduction, continental collision, and backarc-spreading. Resulting mountain chains from the Betics-Atlas to Anatolia are characterized by intense seismic activity. Wide-spread intraplate and subduction related volcanism indicates magma rising from the lower crust and mantle through the lithosphere. The geodynamic drivers of these active tectonic processes remain however controversial. For example, the relevance of delamination of continental mantle, of slab windows, asthenospheric flow, or mantle upwelling are discussed. Methodical advances and the deployment of dense regional seismic arrays and networks provide new options for passive seismic imaging of the lithospheric deep structure. Seismic anisotropy may reveal three-dimensional patterns of asthenospheric flow and lithospheric deformation. Seismically active zones are resolved by homogeneous catalogues of seismic events with decreasing magnitudes of completeness. Geodetic measurements give new insight into plate kinematics and uplift. Data driven geodynamic modelling aims at simulating tectonic processes with increasing resolution and spatial complexity. In this symposium, new observations and multidisciplinary studies shedding light on the geodynamic causes of active plate deformation in the circum-Mediterranean are presented and discussed.
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S18 Integrating Seismic Tomography With Mineral Physics and Potential Fields to Describe the Crust and Upper Mantle Physical State
Convener(s): Judith Bott (Germany)Co-Convener(s): Ajay Kumar (Germany) Magdalena Scheck-Wenderoth (Germany) Ulrich Achauer (France)
Description
To understand plate tectonics as driven by mantle thermodynamics and gravitational forces at interplay with rock rheology, we need comprehensive images of the in-situ physical properties (density, viscosity) and underlying state conditions (pressure, temperature) of the lithospheric plate and its transition into the upper mantle. Once the present-day physical state of such a system is defined, the intrinsic deviatoric stress field and the mantle sources of heat contributing to active plate deformation can be calculated. One key insight into the crust and upper mantle physical state is provided by seismology, namely tomography imaging of seismic velocity perturbations. Their interpretation in terms of composition and temperature conditions, however, is highly non-unique. Despite an ever-growing amount of laboratory-derived relationships between the seismic velocity of mantle minerals and their pressure and temperature derivatives of density and elastic constants, inversion of seismological information for in-situ bulk rock temperature is an ill-posed problem. In addition, effects of anelasticity, e.g., frequency-dependent wave velocity, grain size and fluid content, are important, but less well explored. To reduce the number of potential solutions, additional independent information on crustal configuration and mantle composition, temperature, pressure and density can help. As alternative to thermodynamics-based inversions, empirical approaches to calculate mantle temperature from seismic tomography models implicitly assume some fixed mantle composition or calibrate tomography models with respect to thermal models of the lithosphere and/or pressure-temperature estimates from mantle xenoliths. With this session, we intend to resume an open discussion on how to best exploit mantle seismic velocity models to derive conclusions on the composition and pressure-temperature conditions within the upper (including lithospheric) mantle. We invite contributions integrating multidisciplinary data on the crust and mantle (geological, seismic, heat flow, potential fields, xenoliths) with tomographic models to identify rheological variability exerting the most significant impacts on crustal and surface deformatio
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S19 Fabrics and Dynamics of the Lithosphere-Asthenosphere System Imaged by Seismic Anisotropy and Integrated Studies
Convener(s): Jaroslava Plomerova (Czech Republic)Co-Convener(s): Juan Carlos Afonso (Netherlands) Ulrich Achauer (France)
Description
Seismic anisotropy retrieved from all types of seismic waves provides crucial information on the structure and dynamics of the Earth’s interior at multiple scales. Due to its importance, significant advances have recently been made in the acquisition and numerical modelling of 2D and 3D anisotropy strength and orientation in different tectonic settings. Concurrent progress in laboratory experiments and integrated studies (geophysical-geodynamic-geochemical) is also helping to clarify the relationships between deformation, physical state and seismic anisotropy. In this symposium, we invite single- and multi-method presentations contributing to the understanding of all aspects of seismic anisotropy in the lithosphere (both in the crust and in the mantle lithosphere) and/or the sub-lithospheric upper mantle. We also encourage contributions from multi-disciplinary modelling of the lithosphere-asthenosphere system aiming at understanding how present-day seismic fabrics relate to past and on-going deformation processes. We will discuss the current state of affairs in seismic anisotropy as well as ways forward to advance the field.
Solicited speakers: Ana Ferreira (University College London, UK), Frederik Link (Yale University, USA)
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S20 Education & Outreach to Ensure Success of Earthquake Early Warning Programmes
Convener(s): Raju Sarkar (Bhutan)Co-Convener(s): Xyoli Pérez-Campos (Mexico)
Description
While Earthquake Early Warning (EEW) systems have the potential to greatly reduce the impact of major seismic events, this can only be achieved if: 1) technical recipients of alerts have in place automated technologies to enact protective measures for their systems and facilities, and 2) people are aware of and prepared to take safe response actions, such as to Drop, Cover, and Hold on. To establish the necessary culture of awareness and preparedness, EEW organizations must work with emergency measures organizations, federal public safety campaigns, and others to ensure a broad, consistent, and authoritative EEW education and outreach effort is successful. Such initiatives should take special care to address particularly vulnerable populations, such as low income, new immigrants, Indigenous, and elderly.
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S21 Seismology Education and Inclusive Environments
Convener(s): Raju Sarkar (Bhutan)Co-Convener(s): Aaron Velasco (USA) Xyoli Pérez-Campos (Mexico)
Description
Worldwide, earthquakes represent a substantial hazard, especially to underdeveloped countries. Social preparedness and community response can be improved through awareness and understanding of seismology. They represent a global challenge that can be overcome by improving education in seismology and involvement of the local communities. There are new initiatives to improve seismology awareness through education and citizen participation in various countries around the world. For some countries, resources and infrastructure are a limitation; however, creative strategies can be implemented. Researches on the following topics are welcome, but not limited: a) Educational programs in seismology. b) Strategies on public outreach in seismology.
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JOINT
JA01 Machine Learning in Geo-, Ocean and Space Sciences (IAGA, IAVCEI, IAHS, IASPEI, IAMAS, IAPSO)
Convener(s): Peter Wintoft (Sweden, IAGA)Co-Convener(s): Hristos Tyralis (Greece, IAHS), Dave Reusch (USA, IAMAS), Istvan Szunyogh (USA, IAMAS), Fatma Jebri (UK, IAPSO), Gesa Maria Petersen (USA, IASPEI), Silvia Massaro (Italy, IAVCEI)
Description
Modern artificial intelligence (AI), machine learning (ML) and deep learning (DL) techniques are in the process of transforming many different fields of geosciences including for example seismology, the modelling of hydrological systems, space weather studies and oceanography. The progress in the development of ML algorithms combined with the increasing availability of geophysical data and computational power deliver a great promise for transformational advancements with the novel computational techniques. In this joined session, we invite presentations on a broad variety of AI, ML and DL methods, that both, establish new or improve commonly performed data processing, detection, clustering, interpretation, prediction and imaging tasks. In particular, we welcome contributions on the integration of ML techniques to improve the quality of oceanographic, geosciences and space sciences research approaches. The goal of the session is to establish the state of AI, ML and DL across multiple geoscientific fields, and to pave the path forward in taking full advantage of the exciting developments in ML/DL.
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JA02 Data Assimilation and Statistical Learning in Earth and Space Sciences (IAGA, IACS, IAHS, IAMAS, IASPEI)
Convener(s): Tomoko Matsuo (USA)Co-Convener(s): Patricia de Rosnay (UK, IACS), Julien Aubert (France, IAGA), Larry Kepko (USA,IAGA), Salvatore Grimaldi (Italy, IAHS), Craig Bishop (Australia, IAMAS)
Description
This symposium will serve as a forum on the latest research and development in data assimilation and statistical learning across Earth and Space Science community. Data assimilation is a powerful statistical learning framework that combines models, observations, and their respective uncertainties, allowing us to unify data-driven scientific induction with first principle-based deductions. The framework in the general form can be applied to any geophysical system, providing the common ground for our forum. On the other hand, applications of data assimilation and statistical learning techniques to sparsely observed geophysical systems (such as the core, mantle, cryosphere, hydrosphere, thermosphere and ionosphere, and magnetosphere) face considerable challenges, requiring innovative adaptation of methods to maximize the use of sparse observations, and considerable research efforts to quantify model and observational uncertainties. This symposium solicits papers that address unique application challenges faced by different disciplines so that we can learn from each other and further our common interest in advancing data assimilation and statistical learning applications in the Earth and Space Sciences.
Solicited speakers: Takemasa Miyoshi (RIKEN, Japan), Stephan Grant (Johns Hopkins University Applied Physics Laboratory, USA), Hristos Tyralis (National Technical University of Athens, Greece)
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JA03 Analogue Data for the Future: Preservation and Present-Day Utilization of Historical Data in the Geosciences (IAGA, IACS, IASPEI, IAHS, IAG, IAPSO)
Convener(s): Ciarán Beggan (UK, IAGA)Co-Convener(s): Lauren Vargo (New Zealand, IACS), Kirsten Elger (Germany, IAG), Hisashi Hayakawa (Japan/UK, IAGA), Alberto Viglione (Italy, IAHS), Satheesh S.C. Shenoi (India, IAPSO), Josep Batlló Ortiz (Spain, IASPEI), Kristine Harper (Denmark, IAMAS), Roberto Carniel (Italy, IAVCEI)
Description
In many areas of geophysical and geological studies, long running measurements at a fixed location or over a wider region exist in analogue (physical) form including, amongst others, on photographic paper, in journals or as published tables. It is highly advantageous to convert analogue records to digital values, allowing modern computational techniques and analysis to be applied. However, it is often challenging to convert analogue records as formatting, the type of information recorded, accompanying metadata, and unit metrics change over time. Campaigns to digitize temperature or climate-related measurements have been very successful, especially with the recruitment of keen citizen scientists. However, more scientific formats, such as graphs with technical information or notation, are less amenable to generalist help. Historic analogue records frequently offer significant scientific implications, forming a baseline for analyses of long-term variability and/or short-term extreme hazards in multiple scientific aspects. In this context, it is important to compare these analogue records with one another and document their individual instrumental details for cross-calibrations. This session looks at methods for preservation, extraction, and analysis of historic analogue records, including by manual, image processing or machine learning techniques. This session also accommodates documentation of instrument detail and calibration methods for historical observations. This session welcomes new analyses using data that have previously been in analogue form, and case studies of long-term geophysical variability or individual short-term extreme events. We seek submissions from across all associations.
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JA04 Marine Geodesy and Geophysics – Opportunities & Hazards (IAGA, IAG, IASPEI, IAVCEI)
Convener(s): Sebastian Hölz (Germany, IAGA)Co-Convener(s): Valérie Ballu (France, IAG), Heidrun Kopp (Germany, IASPEI), Paraskevi Nomikou (Greece, IAVCEI)
Description
More than 70% of the Earth surface is covered by ocean. The seafloor is the critical interface where geology, climate, ecosystems, and human activities converge. Yet, a high percentage of the ocean’s seafloor and the subsurface below the seafloor remain unexplored and is both a source of opportunities in terms of unexplored resources (e.g. massive sulfides and hydrothermal fluids) as well as hazards (e.g. due to earthquakes, tsunamis, volcanoes or the exploitation of marine mineral resources). A responsible and sustainable use of resources and mitigation of geohazards require an enhanced knowledge about short- and long-term processes that shape the current sea floor, as well as about its role in the Earth System. Innovative methods help us to better identify and monitor structures, which can be related to geohazards as well as resources. This session invites all contributions of marine geophysical and geodetic research ranging from small to large scales aimed at characterizing structures and dynamics of the Earth’s interior and the seafloor. Solicited fields of research include instrumentation, survey design, data acquisition and novel data processing, visualization, modeling and interpretation procedures. We invite contributions from various fields of offshore geophysical investigations including seismological and seismic, electromagnetic methods as well as contributions from seafloor geodesy.
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JA07 Interdisciplinary Observations of Pre-Earthquake Processes. The Concept of Lithosphere- Atmosphere- Ionosphere Coupling (IAGA, IASPEI (EMSEV))
Convener(s): Mala Bagiya (India, IAGA)Co-Convener(s): Dimitar Ouzounov (USA, IASPEI/EMSEV), Sergey Pulinets (Russia, IASPEI/EMSEV), Katsumi Hattori (Japan, IASPEI/EMSEV), Patrick Taylor (USA, IASPEI/EMSEV)
Description
This symposium concerns the multidisciplinary observations that could lead to understanding processes preceding earthquakes. New results were obtained from seismometers, magnetometers, magnetotelluric stations, GNSS receivers, and Low-Earth-orbiting satellites: DEMETER, Swarm, CSES, etc. This joined analysis of atmosphere-ionosphere connection, seismic records (foreshocks /aftershocks), geochemical, electromagnetic, and thermodynamic processes related to stress changes in the lithosphere established the foundation for the new lithosphere-atmosphere-ionosphere coupling (LAIC) mechanism. This multi-instrumental approach can help support the missing data of the LAIC tools before, during, and after large earthquakes. Presentations will include but are not limited to: observations, modeling; analyses, seismic; geochemical, electromagnetic; and thermodynamic processes; and histories related to stress changes in the lithosphere and their statistical and physical validation. Presentations on the latest developments in earthquake predictability are welcomed.
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JA08 Ground and Satellite Electromagnetic Observations Related to Earthquakes, Tsunami's and Volcanic Activity (IAGA, IASPEI (EMSEV), IAVCEI)
Convener(s): Ramesh Singh (India/USA, EMSEV)Co-Convener(s): Ken'ichi Yamazaki (Japan, EMSEV), Qingjua Huang (China, IASPEI/EMSEV), Takeshi Hasimoto (Japan, IAVCEI/EMSEV)
Description
The earthquakes, tsunamis, and volcanic eruptions are associated with deep ground and the ocean, and the effects are observed through various observing systems deployed on the ground surface, in the borehole, and the ocean. The multispectral satellites and airborne and drone sensors provide information at a high spatial and temporal resolution of the Earth, Ocean, meteorological, atmosphere, and ionosphere. The global navigation satellite system (GNSS) has proved an added advantage globally to observe signals associated with these natural hazards. Recent observations and data analysis has shown a strong coupling between land, ocean, atmosphere, meteorological and ionospheric parameters with earthquakes, tsunamis, and volcanic eruptions. The changing climate system is believed to play an important role in the slow deformation and stress changes and frequency of these disasters. The session invites contributions based on laboratory, modeling, all kinds of ground and field, borehole, and satellite data analysis to understand the physical mechanism associated with these natural hazards.
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JC06 Mountain Cryosphere Hazards (IACS, IAVCEI, IASPEI)
Convener(s): Holger Frey (Switzerland, IACS/GAPHAZ)Co-Convener(s): Michele Koppes (Canada, IACS/GAPHAZ), Mylene Jacquemart (Switzerland, IACS/GAPHAZ), Fabian Walter (Switzerland, IASPEI), Roberto Sulpizio (Italy, IAVCEI)
Description
High mountains across the globe have been undergoing significant changes in natural hazards over the last few decades. Rapid warming has caused changes in the mountain cryosphere at unprecedented rates, affecting geomorphic processes beyond the ice, with significant impacts on landscapes and ecosystems. Cryospheric hazards are also undergoing rapid changes in mountains worldwide, often beyond historical precedence. Risks associated with all types of mass movements in mountain regions are increasing due to changes in the magnitude and frequency of hazards and increasing socio-economic development, which affects both exposure to and vulnerability of people and infrastructure. In this session, we invite contributions on all forms of hazards and risks from the mountain cryosphere, including avalanches, landslides, lake outbursts, volcano-ice interactions, earthquakes, permafrost thaw, debris flows, cascading process-chains, and impacts on mountain communities. We welcome case studies; theoretical and conceptual process models; mapping and modelling past, present and future hazards and risks; as well as aspects of disaster risk reduction and management. Contributions that also address the socio-economic drivers of risks are encouraged.
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JG01 Interactions of the Solid Earth With Ice Sheets and Sea Level (IAG, IACS, IASPEI)
Convener(s): Rebekka Steffen (Sweden, IAG/IASPEI)Co-Convener(s): Bert Wouters (Netherlands, IACS), Natalya Gomez (Canada, IAG/IACS), Lambert Caron (US, IAG), Doug Wiens (US, IASPEI)
Description
Measurements of solid Earth, sea-level and ice-sheet changes are influenced by a complex interaction of processes occurring over a large range of spatial and temporal scales. Present-day observations of solid Earth deformation in a given location are influenced by present and past changes in global surface loading, and these deformations play an important role in controlling ice-sheet changes in turn. Furthermore, observations that constrain past ice sheets are affected not only by glacial isostatic adjustment, but also by changing mantle dynamic topography and tectonic processes. In addition, applied geophysical investigations are revealing crucial spatial variations in Earth rheology, which again affect the deformation of the solid Earth. In this symposium, we showcase model- and data-driven efforts to understand feedbacks between surface load changes and the solid Earth over all timescales and observation types.
Topics covered by the Symposium:
- observations of mass changes in the cryosphere and oceans, and their interaction with solid Earth deformation
- influence of glacial isostatic adjustment on paleo and modern observations of sea level or ice sheet behavior
- seismicity induced by ice-mass and sea-level changes
- geophysical studies of the rheology of the solid Earth in the context of sea-level and ice-sheet studies
Solicited speakers: Tanghua Li (Earth Observatory of Singapore) and Terry Wilson (Ohio State University)
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JG07 Modern Gravimetric Techniques for Geosciences (IAG, IAVCEI, IAPSO, IASPEI)
Convener(s): Jürgen Müller (Germany, IAG)Co-Convener(s): Chris Hughes (UK, IAPSO), Rudolf Widmer-Schnidrig (Germany, IASPEI), Emily Montgomery-Brown (USA, IAVCEI)
Description
New tools for gravimetric Earth observation on ground and in space are being developed in quantum physics that enable novel applications and measurement concepts in the geosciences. We invite presentations to illustrate the principles and state of the art of these novel techniques, like quantum gravimetry, relativistic geodesy with clocks or chronometric levelling, advanced intersatellite tracking and others. These advanced techniques will open a door to a vast bundle of applications. Terrestrial mass variations can be monitored at various scales providing unique information on the related climate change processes. We especially welcome presentations on further applications of those new methods in the geosciences. For example, quantum gravimeters are beneficial for monitoring mass changes, e.g. at volcanos or of the local groundwater. Clock networks provide differences of physical heights and can monitor mass and height variations, e.g., at tide gauges, to disentangle land deformation and sea level rise. Based on that advanced quantum technology, improved observation of mass changes from space will give access to smaller (but relevant) effects like those related to permafrost thawing.
Solicited speaker: Daniele Carbone (INGV - Sezione di Catania, Osservatorio Etneo, Italy) - Experimentation of new technologies for volcano gravimetry at Mt. Etna
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JH01 New, Large, and Open Data for the Earth and Environmental Science Community (IAHS, IAPSO, IACS, IAGA, IASPEI)
Convener(s): Heidi Kreibich (Germany, IAHS)Co-Convener(s): Charles Fierz (Switzerland, IACS), Masahito Nosé (Japan, IAGA), Elena Tel Pérez (Spain, IAPSO), Florian Haslinger (Switzerland, IASPEI)
Description
Data is essential for understanding, modeling and managing earth and environmental processes, their interactions and their dynamics. Therefore, the acquisition, management and use of data is a central component of all earth and environmental sciences. New data sources and advanced monitoring methods, including new sensors and instruments on the ground, at sea and in the air, web crawling technology and citizen science, as well as the strong trend towards open data and data sharing, open up fantastic opportunities but also bring challenges. There are concerns, for example, about ensuring and appropriately documenting data quality in particular with respect to ‘new data’, as well as about creating sufficient incentives for monitoring, data sharing and monitoring downstream usage (attribution) with persistent identifiers, or about adequate long-term curation of raw data and derived products. The aim of this symposium is to present and discuss new opportunities, but also challenges of these developments. We want to learn from each other how to support and implement the UNESCO recommendation for open science, the WMO Unified Data Policy, and the IOC/IODE recommendations in the framework of the UN Ocean Decade. For example, issuing and managing persistent identifiers throughout the data lifecycle, building FAIR and CAREful 'open' services, enforcing proper citation, are approaches that help achieving the vision of FAIR (Findable, Accessible, Interoperable and Reusable) and CARE (Collective benefit, Authority to control, Responsibility and Ethics) data that support quality action and research in the open science environment.
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JH04 Anthropocene: Perspectives From and Within Geophysics (IAHS, IAMAS, IACS, IASPEI, IAVCEI, IAG, IAPSO)
Convener(s): Christophe Cudennec (France, IAHS)Co-Convener(s): Richard Essery (UK,IACS), Melita Keywood (Australia, IAMAS/iCACGP), Mark Lawrence (Germany, IAMAS/iCACGP), Domenico Giardini (Switzerland, IASPEI), Roberto Sulpizio (Italy, IAVCEI), Catia Domingues (UK, IAPSO)
Description
As the International Union of Geological Sciences considers the Anthropocene from a stratigraphic perspective, and as other communities are considering a wider definition (see the ICSU-ICS intermediate synthesis in 2016, https://www.sciencedirect.com/journal/global-environmental-change/vol/39/suppl/C) IUGG has to reconsider the concept and to renew its contribution. This session welcomes any communication in that perspective, including about great acceleration, planetary boundaries, change detection and attribution, climate change and other changes to the atmosphere-ocean-cryosphere-hydrosphere system, such as erosion-sedimentation, man-induced seismicity and man-driven geomorphology, along with related farther-reaching topics such as One Health; and assessing these issues and science-informed policy options for mitigation and adaptation together with the socio-geosciences.
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JH05 Citizen Science, Crowdsourcing and Innovative Monitoring for Advancing Geo-Sciences (IAHS, IASPEI, IAGA, IACS, IAMAS)
Convener(s): Fernando Nardi (Italy, IAHS)Co-Convener(s): Ryan Crumley (USA, IACS), Manoj Nair (USA, IAGA), Thomas Spengler (Norway, IAMAS), Rémy Bossu (France, IASPEI)
Description
Citizen involvement in science has been transformed in the last decade by new and widely accessible data acquisition and processing tools as well as by pervasive low-cost and portable technology. Geospatial technologies and affordable equipment (smart phones, cameras, drones, etc.) allow students, researchers, and citizens to gather, analyze, visualize, and share a wealth of earth system data at different spatial and temporal scales. New opportunities are, thus, arising for addressing the uncertainties and inaccuracies of geophysical models and risk management within different fields, for a better understanding, monitoring, and forecasting of geophysical extremes. Citizen science is supporting a new paradigm for geosciences, where active citizens and crowdsourcing of data have a pivotal role for risk mitigation, communication, and awareness. This transition requires multi-disciplinary and trans-sectoral knowledge, analytical approaches, and data processing methods, spanning from earth-, geo-, hydro-, cryo- sciences to humanities as well as social and communication sciences, to synergistically define the guidelines and procedures that support effective use of human-sensed data. A key challenge in using citizen-science data is the significant noise content in the data collected by untrained users. Recent advances in Machine-Learning (ML) could allow us to build noise-filtering algorithms that can take advantage of high volumes of data created by citizen-science projects. In this framework, the use of unintended technology along with do-it-yourself and low cost equipment is opening novel observational avenues. This joint symposium seeks contributions on data, tools, methods, and procedures that explore the role, value, and performances of citizen science and innovative sensing for earth science research.
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JH06 Education & Outreach in Geosciences (IAHS, IASPEI, IAGA, IAG, IAVCEI, IACS, IAMAS, IAPSO)
Convener(s): Christophe Cudennec (France, IAHS)Co-Convener(s): Fabien Maussion (Austria, IACS), Markku Poutanen (Finland, IAG), Katia Pinheiro (Brasil, IAGA), Tereza Kameníková (Czech Republic, IAGA), Thomas Spengler (Norway, IAMAS), Angela Pomaro (Italy, IAPSO), Raju Sarkar (Bhutan, IASPEI), Natalia Pardo (Colombia, IAVCEI)
Description
Sharing scientific knowledge and methods through education and outreach is of high importance to support the societal transition in terms of sustainability, development, and security. Initial and life-long education, training in operational services, and capacity development within institutions and society are facing many challenges, when dealing with environmental and societal changes, disaster risk reduction, and the evolution of techniques along the data – information – knowledge – decision support chain. This symposium welcomes conceptual developments as well as practical study cases from geoscientists, as well as from didacticians and knowledge brokers. The variety of approaches across disciplines and across the diversity of the geosciences will provide a collective overview on education and outreach activities the basics and variants in our fields. The symposium also encourages sharing of lessons learned from the enhanced digitization induced by the pandemic and from the ongoing digital revolution, showcasing perspectives of the knowledge society and the Open Science paradigm.
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JM03 Polar Regions Instrumentation (IAMAS, IACS, IASPEI)
Convener(s): Tracy Moffat-Griffin (United Kingdom, IAMAS)Co-Convener(s): Alexis Berne (Switzerland, IACS), Matthew Lazzara (USA, IAMAS), Adam T. Ringler (USA, IASPEI)
Description
There are many ways to study and characterize the atmosphere, from the use of ground-based instrumentation and balloons to satellite observations. This symposium welcomes submissions that cover different atmospheric instrument approaches to studying the depth of the polar atmosphere: the surface, the troposphere and beyond. New atmospheric instrumentation and their results, new analysis techniques or planned projects/observational research campaigns will be highlighted. Observational studies that feature polar instrumentation applications are also encouraged in this symposium.
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JP01 Tides (IAPSO, IAHS, IAGA, IASPEI, IAG)
Convener(s): Joanne Williams (UK, IAPSO)Co-Convener(s): Jean-Paul Boy (France, IAG), Nick Pedatella (USA, IAGA), Christophe Cudennec (France, IAHS), Philip Woodworth (UK, IAPSO), Evgeny Podolskiy (Japan, IASPEI)
Description
The session will be open to submissions on any aspect of the tides of the ocean, estuaries, lakes, solid earth, and atmosphere. Tides are fundamental to many geophysical processes, driving ocean mixing, contributing to coastal erosion and sediment transport, and influencing ocean biogeochemistry and ecosystems. Tides affect port operations and coastal infrastructure and modulate the severity of storm surges and coastal flooding. Energy from ocean tides is harnessed for electricity generation. In the cryosphere, tides are also important, including for sea ice dynamics, transport and mixing processes. Icy worlds are not only affected by tides but also modulate them. For example, sea ice dampens tidal amplitudes and currents. At the same time, tides regulate the growth of sea ice, contribute to melting of glacial/sea ice, and can be a pacemaker of glacier flow, deformation, and fracture. Interannual variability in the tides may arise from variations in sea ice extent, changes in ocean stratification or regional climate processes. Tides also play an important role throughout Earth's atmosphere, as well as in other planetary atmospheres. Coastal, regional and global models of tides and internal tides continue to develop, as do techniques for observing tides and reconstructing historical tidal data. We welcome presentations on these methods, and discoveries about past and future long-term changes in tides, tidal variability, tidal dynamics, and the impacts of tides.
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JP04 Ice Sheet-Ocean Interactions: Challenges and Insights From Theory, Observations and Modelling (IAPSO, IACS, IASPEI)
Convener(s): Felicity McCormack (Australia, IAPSO), Isabel Nias (UK, IACS)Co-Convener(s): Donald Slater (UK, IACS), Sue Cook (Australia, IACS), Yoshihiro Nakayama (Japan, IAPSO), Helene Seroussi (USA, IACS/IAPSO), Rick Aster (USA, IASPEI)
Description
Ocean-driven melting of the Greenland and Antarctic Ice Sheets is accelerating and is a key process contributing to the significant uncertainty associated with estimates of future sea level rise. Ice sheet-ocean interactions range across spatial scales: from the microscale processes governing melt at the ice-ocean boundary layer, through the buoyancy-driven circulation beneath ice shelves and at tidewater glaciers, to large-scale fjord and open ocean circulation patterns; and across a range of timescales: in response to seasonal fluctuations in warm water supply to the ice-ocean front to multi-decadal and centennial oscillations in response to intrinsic ice and ocean dynamic processes. This symposium brings together researchers working in the areas of interactions between ice sheets, ice shelves, tidewater glaciers, icebergs, and the ocean, and covering a range of spatial and temporal scales that are relevant to ocean-driven melting of ice. The session will cover theoretical, observational, and modelling disciplines. Studies that offer new insights and technologies to improve understanding of ice-ocean interactions are particularly welcomed.
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JP05 Tsunamis (IAPSO, IASPEI, IAVCEI, IAMAS, IAG)
Convener(s): Yuichiro Tanioka (Japan, IASPEI)Co-Convener(s): Maitane Olabarrieta (USA, IAMAS), Diana Greenslade (Australia, IAPSO), Maria Ana Baptista (Portugal, IAPSO), Alexander Rabinovich (Russia, IASPEI), Mohammad Herdarzadeh (UK, IASPEI), Yuichi Nishimura (Japan, IAVCEI)
Description
Tsunamis are one of the most devastating natural disasters, with the potential to cause tremendous damage along coastlines around the world. Catastrophic tsunami events of this century, such as the 2004 Indian Ocean and 2011 Tohoku tsunamis, have demonstrated the increasing risk of disasters for coastal population and infrastructure. As a response to these deadly tsunamis, many new tsunami forecast and warning capabilities have been developed and implemented. The 2018 Sulawesi and Krakatau tsunamis have demonstrated that tsunamis caused by mechanisms other than great earthquakes must also be considered. The more recent 2022 large volcanic eruption in Tonga generated air-sea coupled wave causing damage along the coast around the Pacific. Sea-level rise caused by global warning also presents new challenges for tsunami science. The IUGG symposium will discuss all aspects of tsunami science including: theoretical and numerical research on tsunami generation and inundation; development of forecast and warning methods; investigation of geologic records of past events; response, mitigation, and recovery strategies; observational studies, including collation of historical observations; and hazard and risk studies from tsunamis generated by earthquakes, landslides, volcanic eruptions. The symposium will also include a special session on meteo-tsunamis, including the air-sea coupled wave due to the 2022 Tonga eruption, in association with IAMAS.
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JS01 Cryoseismology (IASPEI, IACS, IAG)
Convener(s): Andreas Köhler (Norway, IASPEI)Co-Convener(s): Alex Brisbourne (UK, IACS), Bernd Kulessa (UK, IACS), Mirko Scheinert (Germany, IAG), Masaki Kanao (Japan, IASPEI)
Description
The cryosphere, comprising the Earth’s glaciers, ice sheets, sea ice, permafrost, and snowpack, is undergoing rapid change in a warming climate. However, our understanding of the processes governing these changes is hindered by a lack of observations with sufficient temporal and spatial resolution in these generally remote and often inaccessible environments. Fortunately, many of the cryospheric processes of interest produce ground vibrations or cause variations in the seismic wave propagation properties. Analysis of these seismic signals and ground changes can yield essential insight into the relationship between environmental forcing and the response of ocean - cryosphere - solid earth systems. For example, impulsive events with small magnitudes (icequakes) and larger teleseismically detected glacial earthquakes can be generated by dynamic glacial processes such as calving or basal slip. Furthermore, ambient seismic noise interferometry allows us to monitor seasonal and long-term changes in permafrost, ice bodies, and the solid earth below ice sheets and glaciers. Continuous study of temporal and spatial variability of these processes improves our understanding of the cryosphere’s response to climate change. In this joint symposium between IASPEI and IACS, we invite submissions which cover the full gamut of “cryoseismology”. We encourage contributions treating the observation and modeling of seismic signals involving dynamics of ice sheets, sea ice, icebergs and glaciers, as well as changes to the thermal and physical structure of permafrost and snow. We invite submissions on case studies, development of survey techniques, advances in the processing, integration with other geophysical methods or in-situ observations, as well as new technologies such as distributed acoustic sensing (DAS) with fiber optics.
Solicited speaker: Fabian Walter (Switzerland)
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JS02 Seismo – Geodesy (IASPEI, IAG)
Convener(s): Takuya Nishimura (Japan, IASPEI)Co-Convener(s): Jean-Mathieu Noquet (France, IAG)
Description
Geodetic measurements contribute to the study of the different phases of the seismic cycle, as they allow recording coseismic, postseismic, and interseismic deformation. Together with seismology, geodetic data helps improving seismic hazard assessment and define new early warning systems for earthquakes. This symposium focuses on both theoretical aspects and observational challenges of earthquake-related deformation using geodetic measurements, as well as the joint use of seismology and geodesy to better understand the behavior of faults.
Solicited speakers: Prof. Tim Wright (University of Leeds, UK) Dr. Eiichiro Araki (JAMSTEC, Japan)
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JS03 Probing the Earth’s Lithosphere: Understanding Tectonic, Volcanic, Cryotonic and Geodynamic Processes Using Geophysical Methods (IASPEI, IAG, IAGA)
Convener(s): Uli Achauer (France, IASPEI)Co-Convener(s): Holger Steffen (Sweden, IAG), Foteini Vervelidou (France, IAGA)
Description
The emergence of many new high-resolution datasets in almost all different disciplines of geosciences over the last two decades further emphasized that most geoscientific objects are so complex, that only interdisciplinary efforts and combination of datasets provide a pathway to decipher their complex structures and variability with time.
Cratonic domaines, hotspot track systems, rifted continental margins, subduction zones, continental baby plumes, intraplate seismicity, coastal subsidence, and impact cratering are just few examples of such processes pertaining in particular to Earth's lithosphere. In this symposium we welcome studies which shed new light on the evolution and geodynamic development of complex geological processes and structures of Earth's lithosphere using geophysical methods. Terrestrial and space-borne studies making combined use of data from different fields in earth sciences, e.g., potential fields like magnetic field and gravity, tectonics, geochemistry, and structural geology, as well as studies including geodynamic modelling are especially welcome. We further invite presentation on multidisciplinary national and international research infrastructures for integrated use of data and their products.
Solicited speakers:
Magdala Tesauro (University of Trieste, Italy) will present her work on the collisional phase of young orogens using numerical simulations and observations in the Zagros Collisional Zone.
Hanjin Choe (Pusan National University, South Korea) will present his work on the effects of hydrothermal circulation at subduction zones on the magnetization of oceanic crust using geodynamic modeling.
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JS04 Monitoring, Imaging and Mapping of Volcanic Areas (IASPEI, IAG, IAVCEI, IAGA)
Convener(s): Thomas Walter (Germany, IASPEI)Co-Convener(s): Ronni Grapenthin (USA. IAG), Takeshi Hashimoto (Japan, IAGA), Federico Lucchi (Italy, IAVCEI)
Description
Over 1500 volcanoes are considered active, and are in reach of an estimated 10% of the global population. Volcanoes are curse and blessing for the population, as they are a source of significant hazards difficult to predict, and provide fertile soil and exploitable resources. Thanks to field-constrained eruptive histories of active centers and improved instrumental monitoring on the ground, complemented by high resolution remote sensing and complex modelling, the involved time scales, dimensions of volcanic processes and diversity in eruptive style are much better understood. All this allows identifying the internal structure and unrest, intrusion of magma in reservoirs and dikes, hydrothermal activity and degassing at the surface, and material transport processes to distance. Despite these advances, significant volcano eruptions and location is unpredictable, and the duration, rates, or scale remain largely speculative, as vividly demonstrated for the recent eruptions at Nyiragongo (DR Congo), at Hunga Tonga (SW Pacific), Fagradallsfjall (Iceland), or at La Palma (Canary Islands), and elsewhere. The aim of this joint symposium is to bring together scientists elaborating volcanic areas using monitoring, imaging and modelling techniques, to better understand the past, present, and future of volcanoes, and to access the hazards and benefits of volcanic areas. In particular, we invite contributions using broad techniques from geophysical imaging, seismology, geodesy, as well as from active and passive remote sensing, geochemistry, gas analysis and petrology, in order to exchange on how volcanoes prepare for eruptions, undergo unrest, hydrothermally exhalate during periods of quiescence, and evolve in the short and long term. Moreover, interaction of volcanoes and their surrounding will be discussed in this symposium, trying to better understand and exchange on the role of the tectonics, glaciers, earthquakes, ocean, and climate.
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JS05 Real-Time GNSS Data and Products Usage: Interoperability and Management Challenges (IASPEI, IAG, IAVCEI, IAPSO)
Convener(s): Angelo Strollo (Germany, IASPEI)Co-Convener(s): Antonio Avallone (Italy, IAG), Yuhe Tony Song (USA, IAPSO), Clinton John (Switzerland, IASPEI), Giuseppe Puglisi (Italy, IAVCEI)
Description
The Internet of Things continues to expand with reduced restrictions throughout the Urban Space and enables reliable and simple real-time data streaming even from very remote areas. Such technological developments, alongside the growth in cloud computing, have enabled real-time streaming of GNSS data and products. GNSS data today has mature standards (i.e. RTCM formats) for a wide spectrum of applications (civil and military navigation, science, commercial purposes). On the other hand, GNSS products are domain-specific, requiring expertise of scientists and technical personnel. In the last decade, real-time GNSS products have offered new opportunities for monitoring natural hazards in real-time (i.e. earthquakes, volcanoes, landscapes). To become widely available within existing domain specific processing pipelines these products must be available via standard formats and services. A typical example is real-time satellite orbit and clock data which enables several real-time positioning flavours, from standard precise point positioning and relative positioning to regional augmentation and seismic and geodetic data fusion. These products, available in real-time and via standard formats and services (e.g., seedlink and mseed for seismology) could be game changers within the context of early warning systems for tsunamis, landslides, volcanoes, and other natural disasters, as well as for infrastructural monitoring. This interdisciplinary symposium welcomes contributions outlining recent developments in real-time GNSS applications, in particular the usage of real-time data and products within the geophysics domain. This includes: processing techniques developed for real-time products, augmentation through the addition of new data; data management policies; use case examples, in particular those fostering interoperability; adoption or development of new standard formats. The aim of the symposia is to remove the barriers between scientific domains, foster interoperability, and to welcome discussions that lead towards interdisciplinary technical discussions around common formats and interoperability.
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JS06 Joint Inversion of Different Geophysical Data Sets (IASPEI, IAGA, IAG, IAVCEI)
Convener(s): Christel Tiberi (France, IASPEI)Co-Convener(s): Mareen Lösing, (Germany, IAG), Max Moorkamp (Germany, IASPEI/IAGA), Alexander Grayver (Switzerland, IAGA), Luca D'Auria (Spain, IAVCEI)
Description
The Earth is composed of various materials with different physical properties. Therefore understanding its structure and dynamics requires a combination of multiple observations and complementary tools. For decades now, the joint use of different geophysical and geological datasets in inversion or modelling has become a popular way of investigating Earth structure and dynamics at many different scales. In this symposium, we will address all aspects of research that utilize the combination of multiple datasets in multiple parameter inversion or modelling. This includes methodological concepts to improve the performance of integrative imaging, innovative applications and case studies of these techniques, theoretical developments and multi-scale approaches. We welcome contributions from all disciplines that use data integration for a better quantitative understanding of the structure and dynamics of the Earth, from the subsurface down to its core.
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JS07 Geophysical Constraints on the Earth’s Deep Interior Combining Modelling and Observations (IASPEI, IAGA, IAG, SEDI)
Convener(s): Jérémy Rekier (Belgia, IASPEI)Co-Convener(s): Carla Braintenberg (Italy, IAG), David Cebron (France, IAHS)
Description
This symposium aims to bring together contributions from different fields aiming to elucidate the physics of the deep Earth, in particular the Core-Mantle interactions. Recent satellite missions GRACE, GOCE and SWARM have provided invaluable data that can be used to constrain the planet’s deep interior dynamics and physical state. Combined with geodetic and seismic observations, these can be used to constrain the existence of density stratification in the outer core which would affect models of geodynamo, and long-term thermal evolution. With the addition of magnetic observations, magnetohydrodynamics models can be employed to constrain the electric conductivity near the CMB and its direct effect on the Earth’s nutation and length of Day. We also welcome contributions concerning the inner core composition and dynamical interactions with the outer core and mantle.
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JS08 Advances in Heat Flow Studies: From Fundamental Geodynamic Understanding to Geothermal Energy Applications (IASPEI, IAVCEI (IHFC))
Convener(s): Ben Norden (Germany, IAVCEI)Co-Convener(s): Ivone Jimenez Munt (Spain, IASPEI), Sukanta Roy (India, IASPEI)
Description
Until the 1950s, terrestrial heat flow was only documented in a few specific areas of the globe. Due to the importance of heat flow determinations in characterizing the Earth’s energy budget, geodynamic processes, and its role in geothermal energy exploration, the need for extensive heat-flow measurements and mapping became clear. Since 1963, the International Heat Flow Commission of IASPEI has been advising on the acquisition of heat-flow data through temperature-depth measurements and thermal properties of rocks in a variety of geologic environments and tectonic regimes. This effort has led to significant advances in heat flow studies that have positively influenced many disciplines, e.g. seismology, magnetism, volcanology, geodynamics, and hydrogeology. It is now widely recognized that understanding the mechanisms of heat transfer in continental and oceanic regions is crucial for better appreciation of the thermal structure of the lithosphere. For example, the depth distribution of earthquakes can be related to the brittle-ductile boundary which is thermally controlled. In polar regions heat flow can exert a key influence on ice-sheet temperature, ice rheology, basal melting, and the consequent mechanical decoupling at the ice-bedrock interface. Other contemporary topics that thermal studies address include climate change, permafrost thawing, and mineral resource evaluation. This symposium marks the 60th anniversary of the International Heat Flow Commission with the goal of highlighting the accomplishments of heat-flow studies, as well as the technological advances in borehole and rock thermo-physical measurements, and their relationship to a wide range of geodynamic processes related to the thermal state. We welcome contributions that describe the results of experimental and theoretical works of any geoscientific discipline and the symposium is designed to provide a platform for the exchange of ideas, methods, and concepts centered on the thermal aspects of the Earth’s interior.
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JS09 Early Warning Systems for Geohazards (IASPEI, IAVCEI, IAHS, IAG)
Convener(s): Elisa Zuccolo (Italy, IASPEI)Co-Convener(s): John LaBrecque (USA, IAG), Maria-Helena Ramos (France, IAHS), Roberto Sulpizio (Italy, IAVCEI)
Description
Natural disasters related to a variety of geohazards (e.g. earthquakes, landslides, volcanic eruptions, tsunamis and floods) constantly pose threats to humankind and ecosystems at large on a global scale. Exposure to geohazards has increased dramatically in recent decades, and climate change has already affected the frequency and severity of weather-related events in several regions of the world. Consequently, social vulnerability has also changed, prompting Civil Protection authorities and decision makers to increasingly focus on disaster mitigation and risk reduction strategies. In this context, Early Warning Systems (EWS) constitute a major tool to improve preparedness and response to geohazards, prevent loss of life, and reduce economic impacts. Increasing the availability and access to multi-hazard EWS and disaster risk information is also one of the global targets set by the Sendai Framework for Disaster Risk Reduction 2015-2030. This Symposium aims at bringing together scientific and operational advances on the development and demonstration of EWS for geohazards. It provides an opportunity for summarizing the progresses in the achievement of the Sendai Framework targets and reporting on latest trends in EWS for a broad range of geohazards. It also includes identifying current gaps and key challenges for the co-design of EWS with stakeholders and end users, and for their practical implementation. The symposium encourages original research and sharing of knowledge, lessons learned and emerging examples of good practice. The goal is to favor a multi-disciplinary discussion and synergies as a basis for commitments aimed at expanding EWS capacities for geohazards. Topics of interest include but are not limited to: (i) monitoring systems for geohazards, (ii) dynamic and evolutionary process modelling; (iii) treatment of epistemic uncertainty; (iv) decision-making strategies; (v) methodologies and tools for (near) real-time risk mitigation; (vi) cost-benefit analysis and evaluation of socio-economic impact; (vii) evaluation of cascading effects; (viii) practical case studies.
Solicited speakers: Simona Colombelli (University of Naples Federico II, Italy), Léo Martire (NASA Jet Propulsion Laboratory, California Institute of Technology, USA), Tim Melbourne (Central Washington University, USA)
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JV03 Hunga Tonga (IAVCEI, IAMAS, IASPEI, IAGA, IAG)
Convener(s): Roberto Sulpizio (Italy, IAVCEI)Co-Convener(s): Ronan Le Bras (Austria, IASPEI)
Description
The cataclysmic January 15 eruption of Hunga Tonga Hunga Ha’apai presents a rare opportunity for researchers to explore new problems in volcanology, petrology and geochemistry, seismology, tsunamigenesis, infrasonics, and atmospheric science.
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JV04 Volcano Seismology (IAVCEI, IASPEI)
Convener(s): Jürgen Neuberg (UK, IASPEI/IAVCEI)Co-Convener(s): Luca de Siena (Germany, IASPEI)
Description
Analysis of seismic signal is of paramount importance at volcanoes, because they allow to investigate the internal structure of volcanoes and, at the same time, they provide us information about changes in the geophysical state of the volcano. W e welcome in this session any contribution related to seismolgy applied to volcanoes and volcanic systems.
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JV05 Strain Localisation and Seismic and Volcanic Hazards (IAVCEI, IASPEI, IAG)
Convener(s): Jürgen Neuberg (UK, IASPEI/IAVCEI)Co-Convener(s): Philippe Jousset (Germany, IASPEI)
Description
The strain localization is a fundamental process for improving our understanding of the basic physics of earthquake rupture. It is an nterdisciplinary problem that draws on physics, seismology, materials science, engineering, etc. We welcome in this session contributions aimed at highlighting the importance of strain localization in seismology or new techniques in the field.
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JV06 Geophysics of Solar System Planets (IAVCEI, IASPEI, IAG, IAGA)
Convener(s): Alessandro Bonforte (Italy, IAVCEI)Co-Convener(s): Kumiko Hori (Japan, IAGA), Philippe Lognonné (France, IASPEI)
Description
Observations of the distribution, form, and composition of planetary bodies, where subduction, erosion, and vegetation does not obscure surface features. In this session we invite all contributions relating to planetary geology and geophysics, encompassing remote sensing, geomorphology, in-situ or orbital geophysics, sample-based, experimental and numerical modelling, and Earth-analogue studies that utilize planetary data to provide a deeper understanding of this fundamental planetary process.
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JV07 The Architecture of the Lithosphere in Volcanic Regions (IAVCEI, IASPEI, IAGA, ILP)
Convener(s): Luca Caricchi (Switzerland, IAVCEI)Co-Convener(s): Christine Thomas (Germany, IASPEI), Gabi Laske (USA, IASPEI)
Description
The chemical and physical properties of the Earth's lithosphere controls geodynamic processes, the distribution of seismicity and the accumulation and migration of magma to the surface. We welcome research contributions on observations and modeling of lithosphere architecture in volcanic regions as well as the determination of relationships with seismicity, magma chemistry and its transfer to the surface.
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