Accurate hindcasting of explosive eruptions at Whakaari, New Zealand

Phreatic eruptions are small, sudden events, commonly with few precursory signals. They are driven by interactions between magmatic and hydrothermal processes at shallow levels beneath the surface. Here we show that a sequence of banded tremor events, which occurred several weeks before the 9 Decemb...

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Published in:Volcanica
Main Authors: John Stix, Craig Miller, Yajing Liu
Format: Article in Journal/Newspaper
Language:English
Published: Volcanica 2024
Subjects:
Online Access:https://doi.org/10.30909/vol.07.01.153164
https://doaj.org/article/82ca9697c1064c3cb0f9228f1ae12d24
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spelling ftdoajarticles:oai:doaj.org/article:82ca9697c1064c3cb0f9228f1ae12d24 2024-09-09T20:13:20+00:00 Accurate hindcasting of explosive eruptions at Whakaari, New Zealand John Stix Craig Miller Yajing Liu 2024-03-01T00:00:00Z https://doi.org/10.30909/vol.07.01.153164 https://doaj.org/article/82ca9697c1064c3cb0f9228f1ae12d24 EN eng Volcanica https://www.jvolcanica.org/ojs/index.php/volcanica/article/view/217 https://doaj.org/toc/2610-3540 2610-3540 doi:10.30909/vol.07.01.153164 https://doaj.org/article/82ca9697c1064c3cb0f9228f1ae12d24 Volcanica, Vol 7, Iss 1, Pp 153-164 (2024) phreatic eruptions whakaari volcano banded tremor eruption forecasting Geology QE1-996.5 article 2024 ftdoajarticles https://doi.org/10.30909/vol.07.01.153164 2024-08-05T17:49:50Z Phreatic eruptions are small, sudden events, commonly with few precursory signals. They are driven by interactions between magmatic and hydrothermal processes at shallow levels beneath the surface. Here we show that a sequence of banded tremor events, which occurred several weeks before the 9 December 2019 eruption of Whakaari (White Island), New Zealand, can be used to hindcast this eruption. The banded tremor sequence reveals a progressively decreasing time interval between tremor bands. Extrapolating the tremor bands to a time interval of zero provides an accurate estimate, at least one week prior to the eruption, to within 10.2 hours of when the eruption would occur, with a 2.8-day range between 95 % confidence intervals. A similar set of tremor signals appeared before the 27 April 2016 eruption, and these signals provide a very accurate hindcast of this eruption to within 2.61 hours, with a 2.2-day range between 95 % confidence intervals. Our analysis indicates that this potential forecasting approach may prove useful for successfully and accurately forecasting future eruptions at Whakaari. The approach also may be applicable to other volcanoes similar to Whakaari which experience sudden phreatic and phreatomagmatic eruptions. Article in Journal/Newspaper White Island Directory of Open Access Journals: DOAJ Articles New Zealand White Island ENVELOPE(48.583,48.583,-66.733,-66.733) Volcanica 7 1 153 164
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic phreatic eruptions
whakaari volcano
banded tremor
eruption forecasting
Geology
QE1-996.5
spellingShingle phreatic eruptions
whakaari volcano
banded tremor
eruption forecasting
Geology
QE1-996.5
John Stix
Craig Miller
Yajing Liu
Accurate hindcasting of explosive eruptions at Whakaari, New Zealand
topic_facet phreatic eruptions
whakaari volcano
banded tremor
eruption forecasting
Geology
QE1-996.5
description Phreatic eruptions are small, sudden events, commonly with few precursory signals. They are driven by interactions between magmatic and hydrothermal processes at shallow levels beneath the surface. Here we show that a sequence of banded tremor events, which occurred several weeks before the 9 December 2019 eruption of Whakaari (White Island), New Zealand, can be used to hindcast this eruption. The banded tremor sequence reveals a progressively decreasing time interval between tremor bands. Extrapolating the tremor bands to a time interval of zero provides an accurate estimate, at least one week prior to the eruption, to within 10.2 hours of when the eruption would occur, with a 2.8-day range between 95 % confidence intervals. A similar set of tremor signals appeared before the 27 April 2016 eruption, and these signals provide a very accurate hindcast of this eruption to within 2.61 hours, with a 2.2-day range between 95 % confidence intervals. Our analysis indicates that this potential forecasting approach may prove useful for successfully and accurately forecasting future eruptions at Whakaari. The approach also may be applicable to other volcanoes similar to Whakaari which experience sudden phreatic and phreatomagmatic eruptions.
format Article in Journal/Newspaper
author John Stix
Craig Miller
Yajing Liu
author_facet John Stix
Craig Miller
Yajing Liu
author_sort John Stix
title Accurate hindcasting of explosive eruptions at Whakaari, New Zealand
title_short Accurate hindcasting of explosive eruptions at Whakaari, New Zealand
title_full Accurate hindcasting of explosive eruptions at Whakaari, New Zealand
title_fullStr Accurate hindcasting of explosive eruptions at Whakaari, New Zealand
title_full_unstemmed Accurate hindcasting of explosive eruptions at Whakaari, New Zealand
title_sort accurate hindcasting of explosive eruptions at whakaari, new zealand
publisher Volcanica
publishDate 2024
url https://doi.org/10.30909/vol.07.01.153164
https://doaj.org/article/82ca9697c1064c3cb0f9228f1ae12d24
long_lat ENVELOPE(48.583,48.583,-66.733,-66.733)
geographic New Zealand
White Island
geographic_facet New Zealand
White Island
genre White Island
genre_facet White Island
op_source Volcanica, Vol 7, Iss 1, Pp 153-164 (2024)
op_relation https://www.jvolcanica.org/ojs/index.php/volcanica/article/view/217
https://doaj.org/toc/2610-3540
2610-3540
doi:10.30909/vol.07.01.153164
https://doaj.org/article/82ca9697c1064c3cb0f9228f1ae12d24
op_doi https://doi.org/10.30909/vol.07.01.153164
container_title Volcanica
container_volume 7
container_issue 1
container_start_page 153
op_container_end_page 164
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