Seawater-magma interactions sustained the high column during the 2021 phreatomagmatic eruption of Fukutoku-Oka-no-Ba

Fukashi Maeno; Takayuki Kaneko; Mie Ichihara; Yujiro J. Suzuki; Atsushi Yasuda; Kiwamu Nishida; Takao Ohminato

doi:10.1038/s43247-022-00594-4

Communications Earth & Environment (Nov 2022)

Seawater-magma interactions sustained the high column during the 2021 phreatomagmatic eruption of Fukutoku-Oka-no-Ba

Fukashi Maeno,
Takayuki Kaneko,
Mie Ichihara,
Yujiro J. Suzuki,
Atsushi Yasuda,
Kiwamu Nishida,
Takao Ohminato

Affiliations

Fukashi Maeno: Earthquake Research Institute, the University of Tokyo
Takayuki Kaneko: Earthquake Research Institute, the University of Tokyo
Mie Ichihara: Earthquake Research Institute, the University of Tokyo
Yujiro J. Suzuki: Earthquake Research Institute, the University of Tokyo
Atsushi Yasuda: Earthquake Research Institute, the University of Tokyo
Kiwamu Nishida: Earthquake Research Institute, the University of Tokyo
Takao Ohminato: Earthquake Research Institute, the University of Tokyo

DOI: https://doi.org/10.1038/s43247-022-00594-4
Journal volume & issue: Vol. 3, no. 1
pp. 1 – 9

Abstract

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High eruption plumes during submarine eruptions are promoted by seawater vaporisation and decoupled from erupted mass, according to combination of satellite remote sensing observations and plume modelling.

Published in Communications Earth & Environment

ISSN: 2662-4435 (Online)
Publisher: Nature Portfolio
Country of publisher: United Kingdom
LCC subjects: Science: Geology; Geography. Anthropology. Recreation: Environmental sciences
Website: https://www.nature.com/commsenv/

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