Environmental Engineering Reference
In-Depth Information
during the tsunami event. Namely, it was clarifi ed that (i) surging tsunami eroded
the land side of the seawalls and transported sediment landward, (ii) land sediment
was accreted in the sea area mainly due to return fl ow during backwash, and (iii)
deposition occurred in the vicinity of the breakwaters and headlands and erosion
due to backwash was suppressed by seawalls. It was estimated that more than half
of the total amount of shore sand above sea level was transported seaward on the
Yamamoto Coast where the erosion was especially severe. In addition to the charac-
teristics of coastal morphology changes and the mechanisms, post tsunami recon-
struction and restoration in the study area are shown. We hope that this study
contributes to further research for disaster reduction, post-disaster restoration, and
conservation of coasts.
In Japan, the Coast Act was established in 1956 to protect coasts from disasters,
and amended in 1999 to also conserve both the coastal environment and utilization.
In the study area, the seawalls are just being reconstructed for disaster prevention.
From the perspective of long-term coastal management, it is strongly required to
fi nd the vision of the future coast to also conserve the coastal environment and
utilization.
Acknowledgments The authors would like to thank Tohoku Regional Bureau for providing
topography data and aerial photographs used in this study. This research was supported by the
Special Project Research of IRIDeS (International Research Institute of Disaster Science), Tohoku
University and by the Environment Research and Technology Development Fund (S-8-1 (4)) of the
Ministry of the Environment, Japan.
References
Anawat S, Koshimura S, Imai K, Mas E, Gokon H, Muhari A, Imamura F (2012) Damage charac-
teristic and fi eld survey of the 2011 Great East Japan tsunami in Miyagi prefecture. Coastal Eng
J 54:1250005
Earth Environmental Engineering Group, Institute of Industrial Science, The University of Tokyo
(2011) Tsunami inundation line via broad-area ground control source prepared by aerial photos
and estimation. http://stlab.iis.u-tokyo.ac.jp/eq_data/ (in Japanese)
Geospatial Information Authority of Japan (2011) Crustal movements of permanent GPS stations
observed by GEONET System. http://www.gsi.go.jp/chibankansi/chikakukansi40005.html (in
Japanese)
Haraguchi T, Takahashi T, Hisamatsu R, Morishita Y, Sasaki I (2012) Field survey of geomorphic
change on Kesennuma Bay caused by the 2010 Chilean Tsunami and the 2011 Tohoku
Tsunami. J Jpn Soc Civil Eng Ser B2 (Coastal Eng) 68:I_231-I_235 (in Japanese)
Hirao R, Tanaka H, Umeda M, Adityawan MB, Mano A, Udo K (2012) Breaching of sandy coast
and spit due to the 2011 Tsunami and their recovery. J Jpn Soc Civil Eng Ser B2 (Coastal Eng)
68:I_581-I_585 (in Japanese)
Kato F, Suwa Y, Watanabe K, Hatogai S (2013) Mechanisms of coastal dike failure induced by the
Great East Japan Earthquake Tsunami. In: Proceedings of the 33rd international conference on
coastal engineering, structures, 40
Kawai H, Satoh M, Kawaguchi K, Seki K (2011) The 2011 off the Pacifi c Coast of Tohoku
Earthquake Tsunami observed by GPS buoys. Coastal Eng J 67:I_1291-I_1295 (in Japanese)
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