Award Abstract # 1914526
Collaborative Research: Lahar dynamics and Monitoring: A multiparametric approach grounded in infrasound

NSF Org: EAR
Division Of Earth Sciences
Recipient: MICHIGAN TECHNOLOGICAL UNIVERSITY
Initial Amendment Date: July 19, 2019
Latest Amendment Date: February 25, 2021
Award Number: 1914526
Award Instrument: Standard Grant
Program Manager: Eva Zanzerkia
EAR
 Division Of Earth Sciences
GEO
 Directorate for Geosciences
Start Date: August 1, 2019
End Date: July 31, 2024 (Estimated)
Total Intended Award Amount: $294,662.00
Total Awarded Amount to Date: $294,662.00
Funds Obligated to Date: FY 2019 = $294,662.00
History of Investigator:
  • Gregory Waite (Principal Investigator)
    gpwaite@mtu.edu
  • Rudiger Escobar Wolf (Former Principal Investigator)
Recipient Sponsored Research Office: Michigan Technological University
1400 TOWNSEND DR
HOUGHTON
MI  US  49931-1200
(906)487-1885
Sponsor Congressional District: 01
Primary Place of Performance: INSIVUMEH
7 Av. 14-57 Zona 13
Guatemala City
 GT
Primary Place of Performance
Congressional District:
Unique Entity Identifier (UEI): GKMSN3DA6P91
Parent UEI: GKMSN3DA6P91
NSF Program(s): Petrology and Geochemistry,
Geophysics
Primary Program Source: 01001920DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 9150
Program Element Code(s): 157300, 157400
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Lahars, or volcanic mud flows, produce infrasound (low-frequency acoustic energy) that can be detected from distances of many kilometers. As such, it is possible to remotely characterize these hazardous mud flows by tracking their flow positions and energetics through time. This work seeks to develop infrasound analytical tools to locate where lahars initiate, how far and fast they move, and estimate their mass flow. Toward these goals the project will deploy and maintain seismic and infrasonic instruments at Fuego Volcano (Guatemala), where lahars are common during the rainy season (April through September). Rain gauges and time lapse cameras will be installed at locations along the lahar paths to understand how lahars initiate and to validate flow characteristics through direct observation. Fuego volcano is an ideal candidate for this study because of its frequent lahars and relatively easy access and because information learned will be applicable for mitigating risks. Lessons learned at Fuego may then be applied to dozens of volcanoes in the US and around the world where lahar activity is common. The project aims to train several graduate and undergraduate students from the US and result in scientific publication. Important capacity building in Guatemala will result from the training of Guatemalan scientists and technology transfer to observatory staff.

This project will improve our understanding of the seismo-acoustic source mechanisms associated with lahars, and to develop methods that can be used to track such sources and other rapid gravity-driven mass movements. Through multi-parametric observations this study will contribute to our fundamental understanding of how lahars are triggered during precipitation events and where material is incorporated along the lahar flow path. Infra-acoustic arrays and broadband seismic sensors will be deployed at Fuego Volcano (Guatemala) with the intent to remotely monitor the most frequent channels that carry lahars during the rainy season. Signal processing techniques using data from an integrated network of arrays will be used to track and quantify flow energetics. Fuego provides an ideal field site where seismo-acoustic data will be combined with contemporaneous rainfall and geomorphologic (terrain and channel slope) observations. Computer vision techniques will be used to quantify timing, mass flow, and velocities of lahars at various positions along channels. This work merges geomorphology and geophysical approaches to study hazardous lahar phenomena. Broader impacts include development of applied technology for hazard mitigation and training of both US-based and Guatemala-based students and professionals.

This award is cofunded by the PredicMon of and Resilience against Extreme Events (PREEVENTS) program.

This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Bosa, Ashley_R and Bejar, Gustavo and Waite, Gregory_P and Mock, Jerry_C and Pineda, Armando and Anderson, Jacob_F "Dynamics of rain-triggered lahars and destructive power inferred from seismo-acoustic arrays and time-lapse camera correlation at Volcán de Fuego, Guatemala" Natural Hazards , v.121 , 2024 https://doi.org/10.1007/s11069-024-06926-1 Citation Details
Johnson, J. B. and Roca, A. and Pineda, A. and Mérida, R. and Escobar-Wolf, R. and Anderson, J. F. and Mock, J. and Bosa, A. and Bejar, G. and P. Waite, G. "Infrasound detection of approaching lahars" Scientific Reports , v.13 , 2023 https://doi.org/10.1038/s41598-023-32109-2 Citation Details

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

Lahars are a type of volcanic debris flow that occurs when water from rain or other sources mixes with volcanic debris sitting on the flanks of volcanoes. The often violent flows can damage infrastructure and threaten human lives. This project’s original proposal aimed to use infrasound (a form of sound at frequencies below human hearing range) as a way to gain insights of sound generation by lahars. As a complementary objective, the proposed study seeked to compare infrasound-derived lahar data with real-time rainfall distribution. This complementary objective was developed by the team at Michigan Technological University.

During the first field campaign in April-May 2021, the researchers installed a network of rain gauges on one of the active lahar channels on Volcan de Fuego, known as Las Lajas. A seismometer to measure ground vibrations generated by lahar activity was also installed. This deployment complemented the efforts by collaborators at Boise State University who installed infrasound sensors and video cameras for lahar monitoring, and the current surveillance operations by the local monitoring institute, INSIVUMEH. By the end of the first lahar season, it became evident that seismometers had the potential to provide valuable data on lahar initiation and propagation.

Over the following years, we employed seismometers and rain gauges to monitor lahars on Las Lajas and another lahar channel called Ceniza. Seismic data was spatially limited (few stations) prior to our deployment, but allowed us to retrieve a catalog of lahars for these two channels on Volcan de Fuego. This catalog was enhanced with observations from seismometers installed during this project. With this catalog, we are now able to describe what characteristics are common in seismic waves generated by lahar activity on Volcan de Fuego. Moreover, this allows us to track the changes these lahars incur as they propagate downstream.

With the rapid development of artificial intelligence-based (AI) techniques and their power for analyzing large data sets, we pivoted to incorporating AI techniques into an automated detection system into our objectives. To put this into scale, one of our seismometers running for a year and collecting 200 samples every second was capable of generating over 50 billion data points measuring lahar-generated ground vibrations (seismic waves) in three dimensions. While seismic data used in this project was obtained from seismometers with different specifications, these datasets all had the potential to be used in machine learning model (ML) training. With these, we developed LaharML, a machine learning-based algorithm that identifies portions of a seismic signal that were generated by lahar activity. This algorithm is in the process of being deployed into VICTOR, an NSF-funded platform that provides cyberinfrastructure for computational volcanology tools. These seismic datasets also made possible the development of a seismically-derived estimate of the size of lahars from ground rotation (caused by the mass of these flows moving along the channel and depressing the ground adjacent to the channel). In addition, students have used these datasets to get training in advanced processing techniques of seismic signals through this project.

Lahars on Volcan de Fuego are almost exclusively triggered by precipitation, so rain gauges are a critical component of this study. Our rain gauge network focuses on the same active lahar channels targeted by our seismic deployment: Las Lajas and Ceniza. We also included rainfall data from the summit of neighboring Volcan de Agua to constrain high elevation data at a volcano that is not erupting. On Volcan de Fuego, high elevation rain data from ground stations is virtually impossible to obtain given the dense vegetation and the persistent eruptive activity affecting the areas above the treeline. For this reason, we complemented our ground-based rainfall monitoring with radar measurements. The equipment, a portable micro-rain radar, was provided in collaboration with the National Center for Atmospheric Research (NCAR), a research center sponsored by the NSF. The radar allowed us to obtain first-ever remote measurements of precipitation in the high reaches of the Ceniza channel. Additional ML approaches will enable us to identify the common characteristics of rainfall that are associated with lahar activity. Rainfall data will also be instrumental to our ongoing efforts to model flow processes.

Overall, these project results have great potential to improve mitigation strategies in the form of alert systems and better hazard assessments. While this could be impactful to the communities surrounding Volcan de Fuego who are exposed to this type of hazard, we also expect these results and techniques to be widely applicable to other volcanic contexts and to non-volcanic debris flows as well.

 

 


Last Modified: 11/29/2024
Modified by: Gregory P Waite

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