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Tsunami Runup and Inundation in Tonga from the January 2022 Eruption of Hunga Volcano

On January 15th, 2022, at approximately 4:47 pm local time (0347 UTC), several weeks of heightened activity at the Hunga volcano 65 km northwest of Tongatapu, culminated in an 11-h long violent eruption which generated a significant near-field tsunami. Although the Kingdom of Tonga lies astride a la...

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Autores principales: Borrero, Jose C., Cronin, Shane J., Latu’ila, Folauhola Helina, Tukuafu, Pupunu, Heni, Nikolasi, Tupou, Ana Maea, Kula, Taaniela, Fa’anunu, Ofa, Bosserelle, Cyprien, Lane, Emily, Lynett, Patrick, Kong, Laura
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer International Publishing 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9795157/
https://www.ncbi.nlm.nih.gov/pubmed/36590884
http://dx.doi.org/10.1007/s00024-022-03215-5
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author Borrero, Jose C.
Cronin, Shane J.
Latu’ila, Folauhola Helina
Tukuafu, Pupunu
Heni, Nikolasi
Tupou, Ana Maea
Kula, Taaniela
Fa’anunu, Ofa
Bosserelle, Cyprien
Lane, Emily
Lynett, Patrick
Kong, Laura
author_facet Borrero, Jose C.
Cronin, Shane J.
Latu’ila, Folauhola Helina
Tukuafu, Pupunu
Heni, Nikolasi
Tupou, Ana Maea
Kula, Taaniela
Fa’anunu, Ofa
Bosserelle, Cyprien
Lane, Emily
Lynett, Patrick
Kong, Laura
author_sort Borrero, Jose C.
collection PubMed
description On January 15th, 2022, at approximately 4:47 pm local time (0347 UTC), several weeks of heightened activity at the Hunga volcano 65 km northwest of Tongatapu, culminated in an 11-h long violent eruption which generated a significant near-field tsunami. Although the Kingdom of Tonga lies astride a large and tsunamigenic subduction zone, it has relatively few records of significant tsunami. Assessment activities took place both remotely and locally. Between March and June 2022, a field team quantified tsunami runup and inundation on the main populated islands Tongatapu and Eua, along with several smaller islands to the north, including the Ha’apai Group. Peak tsunami heights were ~ 19 m in western Tongatapu, ~ 20 m on south-eastern Nomuka Iki island and ~ 20 m on southern Tofua, located ~ 65 km S and E and 90 km N from Hunga volcano, respectively. In western Tongatapu, the largest tsunami surge overtopped a 13–15 m-high ridge along the narrow Hihifo peninsula in several locations. Analysis of tide gauge records from Nukualofa (which lag western Tongatapu arrivals by ~ 18–20 min), suggest that initial tsunami surges were generated prior to the largest volcanic explosions at ~ 0415 UTC. Further waves were generated by ~ 0426 UTC explosions that were accompanied by air-pressure waves. Efforts to model this event are unable to reproduce the timing of the large tsunami wave that toppled a weather station and communication tower on a 13 m-high ridge on western Tongatapu after 0500 UTC. Smaller tsunami waves continued until ~ 0900, coincident with a second energetic phase of eruption, and noted by eyewitnesses on Tungua and Mango Islands. Despite an extreme level of destruction caused by this tsunami, the death toll was extraordinarily low (4 victims). Interviews with witnesses and analysis of videos posted on social media suggest that this can be attributed to the arrival of smaller ‘pre tsunami’ waves that prompted evacuations, heightened tsunami awareness due to tsunami activity and advisories on the day before, the absence of tourists and ongoing tsunami education efforts since the 2009 Niuatoputapu, Tonga tsunami. This event highlights an unexpectedly great hazard from volcanic tsunami worldwide, which in Tonga’s case overprints an already extreme level of tectonic tsunami hazard. Education and outreach efforts should continue to emphasize the ‘natural warning signs’ of strong ground shaking and unusual wave and current action, and the importance of self-evacuation from coastal areas of low-lying islands. The stories of survival from this event can be used as global best practice for personal survival strategies from future tsunami. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1007/s00024-022-03215-5.
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spelling pubmed-97951572022-12-28 Tsunami Runup and Inundation in Tonga from the January 2022 Eruption of Hunga Volcano Borrero, Jose C. Cronin, Shane J. Latu’ila, Folauhola Helina Tukuafu, Pupunu Heni, Nikolasi Tupou, Ana Maea Kula, Taaniela Fa’anunu, Ofa Bosserelle, Cyprien Lane, Emily Lynett, Patrick Kong, Laura Pure Appl Geophys Article On January 15th, 2022, at approximately 4:47 pm local time (0347 UTC), several weeks of heightened activity at the Hunga volcano 65 km northwest of Tongatapu, culminated in an 11-h long violent eruption which generated a significant near-field tsunami. Although the Kingdom of Tonga lies astride a large and tsunamigenic subduction zone, it has relatively few records of significant tsunami. Assessment activities took place both remotely and locally. Between March and June 2022, a field team quantified tsunami runup and inundation on the main populated islands Tongatapu and Eua, along with several smaller islands to the north, including the Ha’apai Group. Peak tsunami heights were ~ 19 m in western Tongatapu, ~ 20 m on south-eastern Nomuka Iki island and ~ 20 m on southern Tofua, located ~ 65 km S and E and 90 km N from Hunga volcano, respectively. In western Tongatapu, the largest tsunami surge overtopped a 13–15 m-high ridge along the narrow Hihifo peninsula in several locations. Analysis of tide gauge records from Nukualofa (which lag western Tongatapu arrivals by ~ 18–20 min), suggest that initial tsunami surges were generated prior to the largest volcanic explosions at ~ 0415 UTC. Further waves were generated by ~ 0426 UTC explosions that were accompanied by air-pressure waves. Efforts to model this event are unable to reproduce the timing of the large tsunami wave that toppled a weather station and communication tower on a 13 m-high ridge on western Tongatapu after 0500 UTC. Smaller tsunami waves continued until ~ 0900, coincident with a second energetic phase of eruption, and noted by eyewitnesses on Tungua and Mango Islands. Despite an extreme level of destruction caused by this tsunami, the death toll was extraordinarily low (4 victims). Interviews with witnesses and analysis of videos posted on social media suggest that this can be attributed to the arrival of smaller ‘pre tsunami’ waves that prompted evacuations, heightened tsunami awareness due to tsunami activity and advisories on the day before, the absence of tourists and ongoing tsunami education efforts since the 2009 Niuatoputapu, Tonga tsunami. This event highlights an unexpectedly great hazard from volcanic tsunami worldwide, which in Tonga’s case overprints an already extreme level of tectonic tsunami hazard. Education and outreach efforts should continue to emphasize the ‘natural warning signs’ of strong ground shaking and unusual wave and current action, and the importance of self-evacuation from coastal areas of low-lying islands. The stories of survival from this event can be used as global best practice for personal survival strategies from future tsunami. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1007/s00024-022-03215-5. Springer International Publishing 2022-12-28 2023 /pmc/articles/PMC9795157/ /pubmed/36590884 http://dx.doi.org/10.1007/s00024-022-03215-5 Text en © The Author(s) 2022 https://creativecommons.org/licenses/by/4.0/Open AccessThis article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) .
spellingShingle Article
Borrero, Jose C.
Cronin, Shane J.
Latu’ila, Folauhola Helina
Tukuafu, Pupunu
Heni, Nikolasi
Tupou, Ana Maea
Kula, Taaniela
Fa’anunu, Ofa
Bosserelle, Cyprien
Lane, Emily
Lynett, Patrick
Kong, Laura
Tsunami Runup and Inundation in Tonga from the January 2022 Eruption of Hunga Volcano
title Tsunami Runup and Inundation in Tonga from the January 2022 Eruption of Hunga Volcano
title_full Tsunami Runup and Inundation in Tonga from the January 2022 Eruption of Hunga Volcano
title_fullStr Tsunami Runup and Inundation in Tonga from the January 2022 Eruption of Hunga Volcano
title_full_unstemmed Tsunami Runup and Inundation in Tonga from the January 2022 Eruption of Hunga Volcano
title_short Tsunami Runup and Inundation in Tonga from the January 2022 Eruption of Hunga Volcano
title_sort tsunami runup and inundation in tonga from the january 2022 eruption of hunga volcano
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9795157/
https://www.ncbi.nlm.nih.gov/pubmed/36590884
http://dx.doi.org/10.1007/s00024-022-03215-5
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