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  1. 防災科研関係論文

Development and Operation of an Ocean Bottom Cable Seismic and Tsunami (OBCST) Observation System in the Source Region of the Tohoku‐oki Earthquake

https://nied-repo.bosai.go.jp/records/2872
https://nied-repo.bosai.go.jp/records/2872
f127d353-f800-46db-a0c2-eded230e08ad
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Development and Operation of an Ocean Bottom Cable Seismic and Tsunami (OBCST) Observation System in the Source Region of the Tohoku‐oki Earthquake
著者 Masanao Shinohara

× Masanao Shinohara

en Masanao Shinohara

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Tomoaki Yamada

× Tomoaki Yamada

en Tomoaki Yamada

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Kenji Uehira

× Kenji Uehira

en Kenji Uehira

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Shin'ichi Sakai

× Shin'ichi Sakai

en Shin'ichi Sakai

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Hajime Shiobara

× Hajime Shiobara

en Hajime Shiobara

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Toshihiko Kanazawa

× Toshihiko Kanazawa

en Toshihiko Kanazawa

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抄録
内容記述タイプ Other
内容記述 Cabled seafloor seismic and tsunami observation systems are ideal for marine geophysical monitoring because the data can be obtained in real time. We have developed a new compact seafloor-cable seismic and tsunami observation system using Information and Communication Technology (ICT). Our system achieves reliability through redundancy using ICT. A software-based system using up-to-date electronics technology contributes to cost reduction and production sustainability. The system named the Ocean Bottom Cable Seismic and Tsunami (OBCST) observation system was installed on the Pacific Ocean floor off Sanriku, northeast Japan, in September 2015, in the source area of the 2011 Tohoku-oki earthquake. The purpose of the installation is to monitor seismic activity better and to observe tsunami activity through spatially dense observation. The system has been continuously collecting the seismic and pressure data since the deployment. For the seismic data, ambient seismic noise is comparable to that from a previous cable observation system. One observation node is buried 1?m below the seafloor and has a lower noise level compared to nodes on the seafloor. Because the noise levels are stable, many local earthquakes and teleseismic events have been recorded by the system. The data obtained by high-precision pressure gauges have a resolution of <1?hPa which is limited to environmental noise. The effectiveness of the buried pressure gauge is demonstrated by a recording of a tsunami. The system also continuously monitors its operating environment. The operating temperature is reasonably low and stable, which is optimal for long-term operation.
言語 en
書誌情報 en : Earth and Space Science

巻 8, 号 3, 発行日 2021-03
出版者
言語 en
出版者 American Geophysical Union (AGU)
ISSN
収録物識別子タイプ EISSN
収録物識別子 2333-5084
DOI
関連識別子 10.1029/2020ea001359
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