TY - GEN
T1 - Impact of the 2011 tsunami on the littoral system around offshore breakwaters on Sendai Coast
AU - Tanaka, H.
AU - Mitobe, Yuta
AU - Mori, A.
N1 - Publisher Copyright:
© 2016 Taylor & Francis Group, London.
PY - 2016
Y1 - 2016
N2 - After the 2011 Great East Japan Earthquake Tsunami, littoral system on Sendai Coast have been changing due to tsunami-induced highly non-equilibrium condition along the coast. In order to clarify the modification of littoral environment and its subsequent recovery on Sendai Coast, analysis of shoreline change has been carried out. In this study, the shoreline was extracted from frequently captured aerial photographs from 2009 until now, and analysis using an empirical orthogonal function (EOF) method was conducted. It is seen that the shoreline retreated greatly due to tsunami event. In particular, tombolo which existed behind the offshore breakwater completely disappeared due to the tsunami. Total of contribution of the 1st and 2nd EOF components is more than 70%. It is concluded that the 1st component originated from cross-shore sediment movement, while the 2nd component represents longshore sediment transport. Although the 1st component shows only slight modification after the tsunami, the 2nd component resulting from a longshore sediment transport shows distinct change after the tsunami around the offshore breakwaters.
AB - After the 2011 Great East Japan Earthquake Tsunami, littoral system on Sendai Coast have been changing due to tsunami-induced highly non-equilibrium condition along the coast. In order to clarify the modification of littoral environment and its subsequent recovery on Sendai Coast, analysis of shoreline change has been carried out. In this study, the shoreline was extracted from frequently captured aerial photographs from 2009 until now, and analysis using an empirical orthogonal function (EOF) method was conducted. It is seen that the shoreline retreated greatly due to tsunami event. In particular, tombolo which existed behind the offshore breakwater completely disappeared due to the tsunami. Total of contribution of the 1st and 2nd EOF components is more than 70%. It is concluded that the 1st component originated from cross-shore sediment movement, while the 2nd component represents longshore sediment transport. Although the 1st component shows only slight modification after the tsunami, the 2nd component resulting from a longshore sediment transport shows distinct change after the tsunami around the offshore breakwaters.
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U2 - 10.1201/9781315375045-42
DO - 10.1201/9781315375045-42
M3 - Conference contribution
AN - SCOPUS:85018607460
SN - 9781138029798
T3 - Scour and Erosion - Proceedings of the 8th International Conference on Scour and Erosion, ICSE 2016
SP - 349
EP - 353
BT - Scour and Erosion - Proceedings of the 8th International Conference on Scour and Erosion, ICSE 2016
A2 - Harris, John
A2 - Whitehouse, Richard
A2 - Moxon, Sarah
PB - CRC Press/Balkema
T2 - 8th International Conference on Scour and Erosion, ICSE 2016
Y2 - 12 September 2016 through 15 September 2016
ER -