PICVOLC · DePICting the interior of active VOLCanoes to reduce volcanic hazards: application to the present unrest at Nevado del Ruiz (Colombia) - PICVOLC
Horizon 2020 — Marie Skłodowska-Curie Actions
- Duration
- 2019-02-01 → 2021-10-18
- EU contribution
- €168,277
- Participants
- 1
- Scheme
- MSCA-IF-EF-ST
Lines connect the coordinator with its partners.
Results in brief
DePICting the interior of active VOLCanoes to reduce volcanic hazards: application to the present unrest at Nevado del Ruiz (Colombia) - PICVOLC
The correct evaluation of hazards related to the prediction of volcano eruptions is essential to an effective preparedness of populations threatened by volcanoes. Our ability to predict future volcano eruptions is related to locating the source(s) of volcanic unrest and assess their evolution. This is why a better, more comprehensive understanding of changes/deviations of the magmatic system from the background activity is needed for better hazard preparedness. Recent advances in Global Navigation Satellite System (GNSS), tilt, and Interferometric Synthetic Aperture Radar (InSAR) have greatly increased the availability of volcano deformation data. These measurements, combined with appropriate source models, can be used to estimate magma movement that precedes eruptions by detecting variations in the location, depth and volume of the magma intrusion. However, the models used to interpret the data are mostly based on oversimplified a-priori assumptions and there is a clear need for new physics-based models. Often, models of volcanic deformation that do not integrate different geodetic and geophysical datasets, lead to non-unique interpretations of the source of volcanic unrest because they are not sufficiently constrained. Studies that integrate independent datasets can provide a more comprehensive understanding of the deformation sources, while leading towards a more unique solution/interpretation. PICVOLC project aims at combining many geophysical methodologies to reveal the internal structures of volcanoes, in particular of Nevado del Ruiz (Colombia), to support decisions to implement a monitoring network, and to identify possible sources of unrest signals that are detected at the surface. By integrating geodetic and geophysical data as well as advanced Finite Element Method (FEM) numerical models into an inverse exploratory approach, PICVOLC aims at creating more accurate and constrained estimations of the active, inaccessible, and geometrically complex sources that could feed future eruptions. The aim is to provide a more robust estimation of deformation source parameters with reduced ambiguity. A less ambiguous interpretation of the nature, size, and shape of the source of unrest, brings strong benefits for society because it boosts our ability to interpret volcanic activity and to predict impending eruptions, possible volcanic hazards, and related risks for the population.
Data: CORDIS, © European Union
Project objective
More than 500 million people live within the range of volcanoes whose activity can have disastrous economic and environmental impact. Being able to infer changes in the magmatic system during volcanic unrest is important for improving hazard preparedness and forecast future eruptions. PICVOLC aims to overcome the limitations in the current approach in the modeling of volcanic unrest by developing a new, original methodology that integrates seismic, gravity, and deformation data with 3D numerical inversion to create a detailed representation of the source of volcanic unrest. The current volcanic unrest at Nevado del Ruiz volcano will be the case study used to implement, calibrate, and verify this original approach. In 1985, a lahar generated by a modest eruption of Ruiz completely destroyed the town of Armero, killing 25,000 people. PICVOLC involves the integration of fieldwork with Finite Element Methods modeling and joint numerical inversions of geodetic and geophysical data. PICVOLC´s multi-/interdisciplinary nature aims to better constrain the conceptual and numerical models of volcanic unrest and reduce the ambiguity in the identification of the location, depth, volume change, and nature of the source of unrest. The project involves national and international collaboration; it is academic but has also important implications for the monitoring and reduction of volcanic hazards at Ruiz. In particular, it will provide the following innovative products: (a) definition of the subsurface structures with a new map of Bouguer anomalies; (b) 3D FEM model of the volcano; (c) 3D Image of the source(s) of volcanic unrest from inversion of geodetic data; (d) training of graduate students and the staff of the local volcano observatory in numerical modeling.Finally, PICVOLC will be a key step in achieving my professional maturity by extending and reinforcing my knowledge and skills in the design of, involvement in, and management of an international research project.
Original text from CORDIS.
Participants
- UNIVERSITA DEGLI STUDI DI ROMA LA SAPIENZA · RomaCoordinatorItaly
Links
Data: CORDIS, © European Union
