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  1. 防災科研関係論文

Magma discharge variations during the 2011 eruptions of Shinmoe-dake volcano, Japan, revealed by geodetic and satellite observations

https://nied-repo.bosai.go.jp/records/2759
https://nied-repo.bosai.go.jp/records/2759
9e24ba8a-8f8d-4dc2-8166-08b1eacdb5a7
Item type researchmap(1)
公開日 2023-04-27
タイトル
言語 ja
タイトル Magma discharge variations during the 2011 eruptions of Shinmoe-dake volcano, Japan, revealed by geodetic and satellite observations
タイトル
言語 en
タイトル Magma discharge variations during the 2011 eruptions of Shinmoe-dake volcano, Japan, revealed by geodetic and satellite observations
言語
言語 eng
著者 T. Kozono

× T. Kozono

ja T. Kozono

en T. Kozono

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H. Ueda

× H. Ueda

ja H. Ueda

en H. Ueda

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T. Ozawa

× T. Ozawa

ja T. Ozawa

en T. Ozawa

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T. Koyaguchi

× T. Koyaguchi

ja T. Koyaguchi

en T. Koyaguchi

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E. Fujita

× E. Fujita

ja E. Fujita

en E. Fujita

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A. Tomiya

× A. Tomiya

ja A. Tomiya

en A. Tomiya

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Y. J. Suzuki

× Y. J. Suzuki

ja Y. J. Suzuki

en Y. J. Suzuki

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抄録
内容記述タイプ Other
内容記述 We present precise geodetic and satellite observation-based estimations of the erupted volume and discharge rate of magma during the 2011 eruptions of Kirishima-Shinmoe-dake volcano, Japan. During these events, the type and intensity of eruption drastically changed within a week, with three major sub-Plinian eruptions on January 26 and 27, and a continuous lava extrusion from January 29 to 31. In response to each eruptive event, borehole-type tiltmeters detected deflation of a magma chamber caused by migration of magma to the surface. These measurements enabled us to estimate the geodetic volume change in the magma chamber caused by each eruptive event. Erupted volumes and discharge rates were constrained during lava extrusion using synthetic aperture radar satellite imaging of lava accumulation inside the summit crater. Combining the geodetic volume change and the volume of lava extrusion enabled the determination of the erupted volume and discharge rate during each sub-Plinian event. These precise estimates provide important information about magma storage conditions in magma chambers and eruption column dynamics, and indicate that the Shinmoe-dake eruptions occurred in a critical state between explosive and effusive eruption. © 2013 Springer-Verlag Berlin Heidelberg.
言語 en
書誌情報 en : Bulletin of Volcanology

巻 75, 号 3, p. 695-13, 発行日 2013-02
ISSN
収録物識別子タイプ EISSN
収録物識別子 1432-0819
DOI
関連識別子 10.1007/s00445-013-0695-4
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