書誌事項
- タイトル別名
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- Decay Process of the Tsunami due to the 2011 Great off the Pacific Coast of Tohoku Earthquake along the Pacific Coast of Japan
- 2011ネン トウホク チホウ タイヘイヨウオキ ジシン ツナミ ニ オケル ニホン レットウ タイヘイヨウ エンガン ノ ツナミ ゲンスイ カテイ
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We analyzed the process decay of tsunami waveform based on the observed one due to the 2011 Tohoku-Oki earthquake. The observed waveforms at 31 stations along the Pacific coast of Japan were divided into four domains with periods and were evaluated respectively for each physical parameter such as the arrival time, the amplification time of tsunami of the later phase, the maximum tsunami amplitude of the later phase and the decay time. We found out that the decay time of the long period component is generally longer than the short period, but in some cases the time of short period component becomes longer than the others, which may be affected by radiation wave due to large scale bathymetric structure such as the Emperor seamount.
収録刊行物
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- 土木学会論文集Ｂ２（海岸工学）
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土木学会論文集Ｂ２（海岸工学） 70 (2), I_276-I_280, 2014
公益社団法人 土木学会
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詳細情報 詳細情報について
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- CRID
- 1390282680295760768
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- NII論文ID
- 130004706874
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- NII書誌ID
- AA12508551
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- ISSN
- 18838944
- 18842399
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- NDL書誌ID
- 025931282
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- 本文言語コード
- ja
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- データソース種別
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- JaLC
- NDL
- Crossref
- CiNii Articles
- KAKEN
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- 抄録ライセンスフラグ
- 使用不可
