日本地球惑星科学連合2025年大会

講演情報

[E] 口頭発表

セッション記号 S (固体地球科学) » S-VC 火山学

[S-VC30] International Volcanology

2025年5月28日(水) 09:00 〜 10:30 コンベンションホール (CH-B) (幕張メッセ国際会議場)

コンビーナ:Conway Chris(Geological Survey of Japan, AIST)、松本 恵子(産業技術総合研究所地質調査総合センター)、山田 大志(京都大学防災研究所 火山活動研究センター)、川口 允孝(東京大学地震研究所)、Chairperson:Chris Conway(Geological Survey of Japan, AIST)、山田 大志(京都大学防災研究所 火山活動研究センター)、村松 弾(東京大学地震研究所)、田中 良(北海道大学大学院理学研究院附属地震火山研究観測センター)


09:00 〜 09:15

[SVC30-01] How can we forecast eruptions from caldera systems? A case study from Taupō, New Zealand

★Invited Papers

*Finnigan Illsley-Kemp1、Simon Barker1、Eleanor Mestel1、Colin Wilson1 (1.Victoria University of Wellington, New Zealand)

キーワード:caldera, volcano, New Zealand, eruption

Forecasting the likelihood of volcanic eruptions is always challenging but it is particularly difficult at caldera systems. Often these volcanoes have had no observed eruptions, and the geological record shows that they can produce a large range of eruption sizes, from lava domes to supereruptions. In 2022 Taupō caldera, New Zealand, entered a period of unrest which featured heightened seismicity and ground deformation. This prompted Taupō’s Volcanic Alert Level to be raised for the first time in its history. Along with our colleagues in the NZ volcano science community, it was our responsibility to provide science advice on the likelihood of a range of eruption scenarios. This revealed fundamental gaps in our knowledge of how these systems operate in the lead up to eruption, even for a comparatively well-studied volcano like Taupō. In this talk I will discuss these knowledge gaps, draw comparisons to caldera systems in Japan, and suggest future avenues for research in this critical area.