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Titlebook: Natural Disaster and Coastal Geomorphology; Shigeko Haruyama,Toshihiko Sugai Book 2016 Springer International Publishing Switzerland 2016

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发表于 2025-3-21 20:05:02 | 显示全部楼层 |阅读模式
书目名称Natural Disaster and Coastal Geomorphology
编辑Shigeko Haruyama,Toshihiko Sugai
视频video
概述Written by three experts in coastal risks management, specifically for the 2011 Tohoku earthquake and tsunami.Compares studies about previous tsunami damages to the ones from the 2011 Tohoku earthquak
图书封面Titlebook: Natural Disaster and Coastal Geomorphology;  Shigeko Haruyama,Toshihiko Sugai Book 2016 Springer International Publishing Switzerland 2016
描述.This book deals with the Tsunami intrusion in the lower plain in the Tohoku region and role played by the coastal and fluvial landforms in the damages. The land-use patterns and the recent urbanization has also been partly responsible for a risk level enhancement. The 2011 East Japan Earthquake and Tsunami has violently hit the coastal plain in the Tohoku and Kanto regions. The coastal geomorphology of these regions have played an important role in the impacts of this natural disaster. The authors introduce tectonic settings, explain and assess these different risks, and discuss future disaster prevention and mitigation planning..
出版日期Book 2016
关键词Disaster Reduction; Earthquake Impacts; Japanese Coastal Geomorphology; Natural Disaster; Tsunami Impact
版次1
doihttps://doi.org/10.1007/978-3-319-33814-9
isbn_softcover978-3-319-81609-8
isbn_ebook978-3-319-33814-9
copyrightSpringer International Publishing Switzerland 2016
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Shizuka Hashimototo smart cities viewed as cyber-physical systems (CPS). Such CPSs are based on data of various types used for different purposes (Prioritetnyye napravleniya vnedreniya tekhnologiy umnogo goroda v rossiyskikh gorodakh. Ekspertno-analiticheskiy doklad, M.: Tsentr strategicheskikh razrabotok «Severo-Za
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Geomorphology and Tectonic Setting of the Sanriku Coast, Northeastern Japan, and Introduction of Rebsidence of up to 1.3 m was recorded along the Sanriku Coast. However, well-preserved Middle to Late Pleistocene marine terraces along the northern Sanriku Coast have been interpreted to indicate uplift since the Late Quaternary. This discrepancy between long-term uplift and short-term subsidence ha
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