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  1. 防災科研関係論文

Meteotsunami observed by the deep-ocean seafloor pressure gauge network off northeastern Japan

https://nied-repo.bosai.go.jp/records/2877
https://nied-repo.bosai.go.jp/records/2877
9c6bf287-76e8-44f3-b6af-3730701cb9d9
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 ja
タイトル Meteotsunami observed by the deep-ocean seafloor pressure gauge network off northeastern Japan
タイトル
言語 en
タイトル Meteotsunami observed by the deep-ocean seafloor pressure gauge network off northeastern Japan
言語
言語 eng
著者 Tatsuya Kubota

× Tatsuya Kubota

ja Tatsuya Kubota

en Tatsuya Kubota

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Tatsuhiko Saito

× Tatsuhiko Saito

ja Tatsuhiko Saito

en Tatsuhiko Saito

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Naotaka Y. Chikasada

× Naotaka Y. Chikasada

ja Naotaka Y. Chikasada

en Naotaka Y. Chikasada

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Osamu Sandanbata

× Osamu Sandanbata

ja Osamu Sandanbata

en Osamu Sandanbata

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抄録
内容記述タイプ Other
内容記述 This study reports an ocean-bottom pressure gauge (OBP) network, S-net, which captured meteotsunamis with amplitudes as small as a few cm, and investigates its validity and limitation for meteotsunami research studies through data analyses and numerical simulations. On July 1, 2020, S-net recorded tsunami-like signals, although no earthquake was reported. These waves, propagating northward with a velocity of ?110 m/s, were explained by an atmospheric low pressure with a maximum amplitude of ?0.5 ± 0.1 hPa moving northeastward at a speed of 45?50 m/s. The maximum amplitudes of the sea-surface height during the low-pressure passing were up to twice larger than those directly converted from the ocean-bottom pressure without considering the effect of the atmospheric pressure. Our results suggest that the S-net with numerical simulations can detect the generation and propagation of meteotsunamis, which could not be achieved in the past when dense OBP networks were not available.
言語 ja
抄録
内容記述タイプ Other
内容記述 This study reports an ocean-bottom pressure gauge (OBP) network, S-net, which captured meteotsunamis with amplitudes as small as a few cm, and investigates its validity and limitation for meteotsunami research studies through data analyses and numerical simulations. On July 1, 2020, S-net recorded tsunami-like signals, although no earthquake was reported. These waves, propagating northward with a velocity of ?110 m/s, were explained by an atmospheric low pressure with a maximum amplitude of ?0.5 ± 0.1 hPa moving northeastward at a speed of 45?50 m/s. The maximum amplitudes of the sea-surface height during the low-pressure passing were up to twice larger than those directly converted from the ocean-bottom pressure without considering the effect of the atmospheric pressure. Our results suggest that the S-net with numerical simulations can detect the generation and propagation of meteotsunamis, which could not be achieved in the past when dense OBP networks were not available.
言語 en
書誌情報 ja : Geophysical Research Letters
en : Geophysical Research Letters

巻 48, 号 21, p. e2021GL094255, 発行日 2021-10-25
出版者
言語 ja
出版者 American Geophysical Union
出版者
言語 en
出版者 American Geophysical Union
ISSN
収録物識別子タイプ EISSN
収録物識別子 1944-8007
DOI
関連識別子 10.1029/2021GL094255
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