WP8 - Anthropogenic geophysical extremes
OverviewDevelop and implement 1 DTC for Anthropogenic Geophysical Extreme Forecasting (AGEF) with 4 workflow outcomes: forecasting of long-range responses of georeservoirs (TC-AGEF1), forecasting of late responses of georeservoirs (TC-AGEF2), modelling of the largest magnitude (TC-AGEF3), and induced seismic hazard map estimation (TC-AGEF4).
Test the DTC-A through demonstrators at 2 relevant European sites: Strasbourg geothermal site in France (SD12) and KGHM copper ore mine in Poland (SD13).
Space: A Digital Twin for GEOphysical extremes (DT-GEO)
SEEK ID: https://workflowhub.eu/projects/182
Funding codes:- 101058129
Public web page: https://dtgeo.eu/
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Team created: 1st Aug 2023
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Teams: WP8 - Anthropogenic geophysical extremes
Organizations: Centre National de la Recherche Scientifique (CNRS)
Teams: WP8 - Anthropogenic geophysical extremes
Organizations: ACC Cyfronet AGH
https://orcid.org/0000-0002-9824-7962
Working on: A Digital Twin for GEOphysical extremes (DT-GEO) ~ https://workflowhub.eu/programmes/36
Teams: Cluster Emergent del Cervell Humà, Workflows and Distributed Computing, WP6 - Tsunamis, WP7 - Earthquakes, WP8 - Anthropogenic geophysical extremes, WP5 - Volcanoes, Pillar I: Manufacturing, Pillar II: Climate, Pillar III: Urgent computing for natural hazards, eFlows4HPC general, COMPSs Tutorials
Organizations: Barcelona Supercomputing Center
https://orcid.org/0000-0003-0606-2512
Established Researcher at Workflows and Distributed Computing Group, Computer Sciences department, Barcelona Supercomputing Center.
With present computational capabilities and data volumes entering the Exascale Era, digital twins of the Earth system will be able to mimic the different system components (atmosphere, ocean, land, lithosphere) with unrivaled precision, providing analyses, forecasts, and what if scenarios for natural hazards and resources from their genesis phases and across their temporal and spatial scales. DT-GEO aims at developing a prototype for a digital twin on geophysical extremes including earthquakes, ...
Teams: WP5 - Volcanoes, WP6 - Tsunamis, WP7 - Earthquakes, WP8 - Anthropogenic geophysical extremes
Web page: https://dtgeo.eu/
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Spain
City: Barcelona
Web page: https://www.bsc.es/
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United Kingdom
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Web page: https://www.bgs.ac.uk
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France
City: Montpellier
Web page: https://www.cnrs.fr/en
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Italy
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Web page: https://www.ingv.it/
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City: Warsaw
Web page: http://www.english.pan.pl/
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Country: Spain
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Web page: https://www.csic.es
The workflow DT-AGEF4 will produce seismic hazard maps related to the nearfuture anthropogenic seismicity (induced or triggered seismicity). The anthropogenic seismicity hazard maps will be related to the time-varying technological factors. The rationales behind the proposed workflow are (Lasocki, S., Proc. Sixth Int. Symp. on Rockburst and Seismicity in Mines, 2005; Lasocki, S. and Orlecka-Sikora, B., Tectonophys., 2008; Orlecka-Sikora, B., Tectonophys., 2008; Lasocki, S., Rockburst Mechanisms, ...
The workflow will primarily focus on estimation of the maximum magnitude using various deterministic and statistical models available in the literature. The workflow consists of 5 steps. The first four steps belong to the CB-AGEF1 and ultimately aim at creation of the advanced seismic catalog. The last 5th step (belonging to the CBAGEF3-1) takes the available hydraulic data and advanced seismicity catalog derived in steps 1-4 and performs the actual assessment of the maximum magnitude. Step 1 is ...
The advanced earthquake catalog is built from existing applications on the EPISODES platform (steps 1, 3, 4) and a newly developed application for phase association (step 2) and an application for catalog homogenization (step 5).
The advanced earthquake catalog is built from existing applications on the EPISODES platform (step 1,3, 4 in Figure 4.2) and a newly developed application for phase association (step 2) and an application for catalog homogenization (step 5). The last application is designed to facilitate the creation of a homogenized earthquake catalog, ensuring consistency across key parameters such as location (X, Y, Z), time (T), and magnitude (M). This is achieved by standardizing various magnitude measurements, ...
