Correlation between GNSS-TEC and eruption magnitude supports the use of ionospheric sensing to complement volcanic hazard assessment

Despite the global threat posed by large-scale eruptions to communities, to the climate, and to the consequent impacts on the world economy, many active volcanoes still lack of adequate ground-based instrumentation. Satellite-based remote sensing has been used to complement volcano monitoring and ri...

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Main Authors: Manta, Fabio, Occhipinti, Giovanni, Hill, Emma M., Perttu, Anna, Assink, Jelle, Taisne, Benoit
Other Authors: Asian School of the Environment
Format: Article
Language:English
Published: 2021
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Online Access:https://hdl.handle.net/10356/151807
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Institution: Nanyang Technological University
Language: English
id sg-ntu-dr.10356-151807
record_format dspace
institution Nanyang Technological University
building NTU Library
continent Asia
country Singapore
Singapore
content_provider NTU Library
collection DR-NTU
language English
topic Science::Geology
Correlation
Earthquake Magnitude
spellingShingle Science::Geology
Correlation
Earthquake Magnitude
Manta, Fabio
Occhipinti, Giovanni
Hill, Emma M.
Perttu, Anna
Assink, Jelle
Taisne, Benoit
Correlation between GNSS-TEC and eruption magnitude supports the use of ionospheric sensing to complement volcanic hazard assessment
description Despite the global threat posed by large-scale eruptions to communities, to the climate, and to the consequent impacts on the world economy, many active volcanoes still lack of adequate ground-based instrumentation. Satellite-based remote sensing has been used to complement volcano monitoring and risk assessment for volcanic ash, but this technique is often limited by weather conditions. In this work, we explore the ionospheric total electron content (TEC) perturbations measured by GNSS to provide additional information and complement conventional monitoring systems. To this end, we measure the GNSS TEC perturbation associated with the acoustic-gravity waves generated by 22 volcanic explosions. We introduce a new metric—the Ionospheric Volcanic Power Index (IVPI)—to quantify the energy transferred to the ionosphere by volcanic explosions. We evaluate the IVPI against several well-established metrics from seismic and infrasonic volcano monitoring as well as satellite remote sensing. Our results show that the IVPI successfully correlates with the Volcanic Explosivity Index (VEI) for events larger than VEI 2. Moreover, the IVPI shows strong correlation with both the acoustic source power and the ash plume height, from which depends the style of volcanic activity. Moderate correlation between IVPI and peak ground velocity (PGV) requires further study in order to evaluate the role of different parameters (seismic magnitude, attenuation, style of faulting, crustal structure, etc.). Our results suggest that ionospheric monitoring by GNSS TEC can help to characterize volcanic eruptions, opening new exciting avenues for continuous volcano monitoring and warning systems by remote sensing.
author2 Asian School of the Environment
author_facet Asian School of the Environment
Manta, Fabio
Occhipinti, Giovanni
Hill, Emma M.
Perttu, Anna
Assink, Jelle
Taisne, Benoit
format Article
author Manta, Fabio
Occhipinti, Giovanni
Hill, Emma M.
Perttu, Anna
Assink, Jelle
Taisne, Benoit
author_sort Manta, Fabio
title Correlation between GNSS-TEC and eruption magnitude supports the use of ionospheric sensing to complement volcanic hazard assessment
title_short Correlation between GNSS-TEC and eruption magnitude supports the use of ionospheric sensing to complement volcanic hazard assessment
title_full Correlation between GNSS-TEC and eruption magnitude supports the use of ionospheric sensing to complement volcanic hazard assessment
title_fullStr Correlation between GNSS-TEC and eruption magnitude supports the use of ionospheric sensing to complement volcanic hazard assessment
title_full_unstemmed Correlation between GNSS-TEC and eruption magnitude supports the use of ionospheric sensing to complement volcanic hazard assessment
title_sort correlation between gnss-tec and eruption magnitude supports the use of ionospheric sensing to complement volcanic hazard assessment
publishDate 2021
url https://hdl.handle.net/10356/151807
_version_ 1735491258459095040
spelling sg-ntu-dr.10356-1518072022-06-07T06:14:57Z Correlation between GNSS-TEC and eruption magnitude supports the use of ionospheric sensing to complement volcanic hazard assessment Manta, Fabio Occhipinti, Giovanni Hill, Emma M. Perttu, Anna Assink, Jelle Taisne, Benoit Asian School of the Environment Earth Observatory of Singapore Science::Geology Correlation Earthquake Magnitude Despite the global threat posed by large-scale eruptions to communities, to the climate, and to the consequent impacts on the world economy, many active volcanoes still lack of adequate ground-based instrumentation. Satellite-based remote sensing has been used to complement volcano monitoring and risk assessment for volcanic ash, but this technique is often limited by weather conditions. In this work, we explore the ionospheric total electron content (TEC) perturbations measured by GNSS to provide additional information and complement conventional monitoring systems. To this end, we measure the GNSS TEC perturbation associated with the acoustic-gravity waves generated by 22 volcanic explosions. We introduce a new metric—the Ionospheric Volcanic Power Index (IVPI)—to quantify the energy transferred to the ionosphere by volcanic explosions. We evaluate the IVPI against several well-established metrics from seismic and infrasonic volcano monitoring as well as satellite remote sensing. Our results show that the IVPI successfully correlates with the Volcanic Explosivity Index (VEI) for events larger than VEI 2. Moreover, the IVPI shows strong correlation with both the acoustic source power and the ash plume height, from which depends the style of volcanic activity. Moderate correlation between IVPI and peak ground velocity (PGV) requires further study in order to evaluate the role of different parameters (seismic magnitude, attenuation, style of faulting, crustal structure, etc.). Our results suggest that ionospheric monitoring by GNSS TEC can help to characterize volcanic eruptions, opening new exciting avenues for continuous volcano monitoring and warning systems by remote sensing. Ministry of Education (MOE) Nanyang Technological University National Research Foundation (NRF) Published version This research was supported by the Dr. Stephen Riady Geoscience Scholars Fund, The Earth Observatory of Singapore, the Singapore Ministry of Education under the Research Centres of Excellence initiative, and by the National Research Foundation Singapore under its NRF Investigator scheme (Award No. NRF-NRFI05-2019-0009 to E.H.). F.M. post-doc is supported by the CNES. G.O. is supported by Programme National de Télédétection Spatiale (PNTS), grant No. PNTS-2020-16; by the CNES, project Global Ionospheric Seismology Network & Background; and by the Institut Universitaire de France (IUF). This work is based on freely available GNSS data from the following web-resources: UNAVCO (www.unavco.org); and The Sumatran GPS Array (SuGAr) (ftp://ftp.earthobservatory.sg/SugarData). SuGAr is jointly owned and operated by the EOS and the Indonesian Institute of Sciences (LIPI), and we are grateful to many scientists and field technicians who helped install and maintain the SuGAr network, including Jeffrey Encillo, Iwan Hermawan, Paramesh Banerjee, Imam Suprihanto, Danny Natawidjaja, Bambang Suwargadi, and Dudi Prayudi. This is EOS contribution 341 and IPGP contribution 4181. 2021-08-05T13:03:21Z 2021-08-05T13:03:21Z 2021 Journal Article Manta, F., Occhipinti, G., Hill, E. M., Perttu, A., Assink, J. & Taisne, B. (2021). Correlation between GNSS-TEC and eruption magnitude supports the use of ionospheric sensing to complement volcanic hazard assessment. Journal of Geophysical Research: Solid Earth, 126(2), e2020JB020726-. https://dx.doi.org/10.1029/2020JB020726 2169-9313 0000-0001-5170-6132 0000-0001-9323-3185 0000-0003-0231-5818 0000-0003-3590-1549 0000-0002-4990-6845 0000-0002-3205-6485 https://hdl.handle.net/10356/151807 10.1029/2020JB020726 2-s2.0-85101542518 2 126 e2020JB020726 en NRF-NRFI05-2019-0009 Journal of Geophysical Research: Solid Earth 10.21979/N9/GIP5TJ © 2020 The Authors.This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. application/pdf