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  1. 防災科研関係論文

Extracting near-field seismograms from ocean-bottom pressure gauge inside the focal area: application to the 2011 Mw 9.1 Tohoku-Oki earthquake

https://nied-repo.bosai.go.jp/records/4602
https://nied-repo.bosai.go.jp/records/4602
331f98a7-2815-4152-ad1b-c3337197491a
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 ja
タイトル Extracting near-field seismograms from ocean-bottom pressure gauge inside the focal area: application to the 2011 Mw 9.1 Tohoku-Oki earthquake
タイトル
言語 en
タイトル Extracting near-field seismograms from ocean-bottom pressure gauge inside the focal area: application to the 2011 Mw 9.1 Tohoku-Oki earthquake
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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Hiroaki Tsushima

× Hiroaki Tsushima

ja Hiroaki Tsushima

en Hiroaki Tsushima

Search repository
Ryota Hino

× Ryota Hino

ja Ryota Hino

en Ryota Hino

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Yusaku Ohta

× Yusaku Ohta

ja Yusaku Ohta

en Yusaku Ohta

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Syuichi Suzuki

× Syuichi Suzuki

ja Syuichi Suzuki

en Syuichi Suzuki

Search repository
Daisuke Inazu

× Daisuke Inazu

ja Daisuke Inazu

en Daisuke Inazu

Search repository
抄録
内容記述タイプ Other
内容記述 Recent studies have shown that ocean‐bottom pressure gauges (OBPs) can record seismic waves in addition to tsunamis and seafloor permanent displacements, even if they are installed inside the focal area where the signals are extremely large. We developed a method to extract dynamic ground motion waveforms from near‐field OBP data consisting of a complex mixture of various signals, based on an inversion analysis along with a theory of tsunami generation. We applied this method to the OBP data of the 2011 Tohoku‐Oki earthquake. We successfully extracted the low‐frequency vertical seismograms inside the focal area (f < ?0.05 Hz), although those of the Mw ?9 megathrust earthquake had never previously been reported. The seismograms suggested two dominant energy releases around the hypocenter. The seismic wave signals recorded by the near‐field OBP will be important not only to reveal earthquake ruptures and tsunami generation processes but also to conduct real‐time tsunami forecasts.
言語 ja
抄録
内容記述タイプ Other
内容記述 Recent studies have shown that ocean‐bottom pressure gauges (OBPs) can record seismic waves in addition to tsunamis and seafloor permanent displacements, even if they are installed inside the focal area where the signals are extremely large. We developed a method to extract dynamic ground motion waveforms from near‐field OBP data consisting of a complex mixture of various signals, based on an inversion analysis along with a theory of tsunami generation. We applied this method to the OBP data of the 2011 Tohoku‐Oki earthquake. We successfully extracted the low‐frequency vertical seismograms inside the focal area (f < ?0.05 Hz), although those of the Mw ?9 megathrust earthquake had never previously been reported. The seismograms suggested two dominant energy releases around the hypocenter. The seismic wave signals recorded by the near‐field OBP will be important not only to reveal earthquake ruptures and tsunami generation processes but also to conduct real‐time tsunami forecasts.
言語 en
書誌情報 ja : Geophysical Research Letters
en : Geophysical Research Letters

巻 48, 号 7, p. e2020GL091664, 発行日 2021-03-11
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 10.1029/2020GL091664
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