Airfall volume of the 15 January 2022 eruption of Hunga volcano estimated from ocean color changes

IF 3.6 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Bulletin of Volcanology Pub Date : 2024-05-29 DOI:10.1007/s00445-024-01744-6
Liam J. Kelly, Kristen E. Fauria, Michael Manga, Shane J. Cronin, Folauhola Helina Latu’ila, Joali Paredes-Mariño, Tushar Mittal, Ralf Bennartz
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Abstract

On 15 January 2022, Hunga volcano erupted, creating an extensive and high-reaching umbrella cloud over the open ocean, hindering traditional isopach mapping and fallout volume estimation. In MODIS satellite imagery, ocean surface water was discolored around Hunga following the eruption, which we attribute to ash fallout from the umbrella cloud. By relating intensity of ocean discoloration to fall deposit thicknesses in the Kingdom of Tonga, we develop a methodology for estimating airfall volume over the open ocean. Ash thickness measurements from 41 locations are used to fit a linear relationship between ash thickness and ocean reflectance. This produces a minimum airfall volume estimate of \({1.8}_{-0.4}^{+0.3}\) km3. The whole eruption produced > 6.3 km3 of uncompacted pyroclastic material on the seafloor and a caldera volume change of 6 km3 DRE. Our fall estimates are consistent with the interpretation that most of the seafloor deposits were emplaced by gravity currents rather than fall deposits. Our proposed method does not account for the largest grain sizes, so is thus a minimum estimate. However, this new ocean-discoloration method provides an airfall volume estimate consistent with other independent measures of the plume and is thus effective for rapidly estimating fallout volumes in future volcanic eruptions over oceans.

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根据海洋颜色变化估算 2022 年 1 月 15 日洪加火山爆发的降气量
2022 年 1 月 15 日,洪加火山爆发,在公海上空形成了大范围、高覆盖度的伞状云,阻碍了传统的等高线测绘和火山灰沉降量估算。在 MODIS 卫星图像中,洪加火山爆发后周围的海洋表层水变色,我们将其归因于伞状云的火山灰沉降物。通过将海洋变色强度与汤加王国的火山灰沉积厚度联系起来,我们开发出了一种估算公海上空火山灰体积的方法。我们利用 41 个地点的火山灰厚度测量结果,拟合出火山灰厚度与海洋反射率之间的线性关系。由此得出的最小降尘量估计值为({1.8}_{-0.4}^{+0.3}\) km3。整个喷发过程在海底产生了 6.3 km3 未压实的火成碎屑物质,火山口体积变化为 6 km3 DRE。我们的坠落估计值与大部分海底沉积物是由重力流而不是坠落沉积物堆积而成的解释相一致。我们提出的方法没有考虑到最大的粒度,因此只是一个最低估计值。不过,这一新的海洋降解方法提供的降尘量估计值与其他独立的羽流测量方法一致,因此可用于快速估计未来海洋上空火山爆发的降尘量。
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来源期刊
Bulletin of Volcanology
Bulletin of Volcanology 地学-地球科学综合
CiteScore
6.40
自引率
20.00%
发文量
89
审稿时长
4-8 weeks
期刊介绍: Bulletin of Volcanology was founded in 1922, as Bulletin Volcanologique, and is the official journal of the International Association of Volcanology and Chemistry of the Earth’s Interior (IAVCEI). The Bulletin of Volcanology publishes papers on volcanoes, their products, their eruptive behavior, and their hazards. Papers aimed at understanding the deeper structure of volcanoes, and the evolution of magmatic systems using geochemical, petrological, and geophysical techniques are also published. Material is published in four sections: Review Articles; Research Articles; Short Scientific Communications; and a Forum that provides for discussion of controversial issues and for comment and reply on previously published Articles and Communications.
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