Effects of the 2011 Tohoku earthquake and tsunami on the abundance and composition of anthropogenic marine debris on the continental slope off the Pacific coast of northeastern Japan

2021 ◽  
Vol 164 ◽  
pp. 112039
Author(s):  
Tomoaki Goto ◽  
Haruka Shibata ◽  
Takahiro Murakami
2012 ◽  
Vol 7 (sp) ◽  
pp. 485-490
Author(s):  
Chiharu Mizuki ◽  
◽  
Kazuomi Hirakawa ◽  

Many aspects affect local tsunami behavior. A drastic change in behavior in the 2011 Tohoku Earthquake at specific sites in relation to coastal conditions in Hokkaido. These include coastal constructions such as jetty ports, digging formula ports, types of seawall, etc., in addition to land use for fisheries. Examples of site-specific behavior in the 2011 Tohoku Earthquake along the Pacific coast of Hokkaido are introduced in order to help future tsunami disasters.


2016 ◽  
Vol 11 (6) ◽  
pp. 1253-1270 ◽  
Author(s):  
Hao Wu ◽  
◽  
Kazuaki Masaki ◽  
Kojiro Irikura ◽  
Susumu Kurahashi ◽  
...  

In this study, empirical fragility curves expressed in terms of relationship between damage ratio indices of buildings and ground motion indices were developed in northern Miyagi prefecture located in near-field areas during the 2011 off the Pacific coast of Tohoku Earthquake. The ground motion indices were evaluated from observed ground motions at strong-motion stations and estimated at sites at which no strong-motion accelerometers were deployed during the mainshock. The ground motions at the non-instrumental sites were estimated using the empirical Green’s function method based on bedrock motions inverted from observed records on surfaces from small events that occurred inside the source fault, transfer functions due to underground velocity structures identified from microtremor H/V spectral ratios, and a short-period source model of the mainshock. The findings indicated that the empirical fragility curves as functions of Japan Meteorological Agency (JMA) instrumental seismic intensity during the 2011 Tohoku Earthquake almost corresponded to those during the 1995 Kobe Earthquake and the seven disastrous earthquakes that occurred between 2003 and 2008. However, the empirical fragility curves as functions of peak ground velocity were the lowest. A possible reason for this is that the response spectra of the ground motions in the period ranging from 1.0 s to 1.5 s were small during the 2011 Tohoku Earthquake. Another reason could be the seismic resistant capacities of buildings in the studied districts involved during the 2011 Tohoku Earthquake exceeded those in the cities affected during the 1995 Kobe Earthquake.


2012 ◽  
Vol 54 (1) ◽  
pp. 1250002-1-1250002-17 ◽  
Author(s):  
Yasunori Watanabe ◽  
Yuta Mitobe ◽  
Ayumi Saruwatari ◽  
Tomohito Yamada ◽  
Yasuo Niida

2014 ◽  
Vol 123 (6) ◽  
pp. 835-853 ◽  
Author(s):  
Takahiro WATANABE ◽  
Noriyoshi TSUCHIYA ◽  
Shin-ichi YAMASAKI ◽  
Ryoichi YAMADA ◽  
Nobuo HIRANO ◽  
...  

2021 ◽  
Author(s):  
Yuji Sano ◽  
Tomoyo Okumura ◽  
Naoko Murakami-Sugihara ◽  
Kentaro Tanaka ◽  
Takanori Kagoshima ◽  
...  

Abstract We report here hourly variations of Mg/Ca, Sr/Ca and Ba/Ca ratios in a Mediterranean mussel shell (Mytilus galloprovincialis) collected at the Otsuchi bay, on the Pacific coast of northeastern Japan. This bivalve was living in the intertidal zone, where such organisms are known to form a daily or bidaily growth line comprised of abundant organic matter. Mg/Ca ratios of the inner surface of the outer shell layer, corresponding to the most recent date, show cyclic changes at 25-90 mm intervals, while no valuable variations are observed in Sr/Ca and Ba/Ca ratios. High Mg/Ca ratios were probably established when the bivalve was located at low tide with a reduced supply of Ca from seawater. Immediately following the great tsunami induced by the 2011 Tohoku earthquake, Mg/Ca enrichment occurred, up to 10 times that of normal low tide, while apparent Ba/Ca enrichment was observed for only a few days following the event, implementing a proxy of the past tsunami. Following the tsunami, periodic peaks and troughs in Mg/Ca continued, perhaps due to a biological memory effect as an endogenous clock.


2015 ◽  
Vol 72 (1) ◽  
pp. 39-52 ◽  
Author(s):  
Hideki Fukuda ◽  
Ryosuke Katayama ◽  
Yanhui Yang ◽  
Hiroyuki Takasu ◽  
Yuichiro Nishibe ◽  
...  

2015 ◽  
Vol 72 (1) ◽  
pp. 77-90 ◽  
Author(s):  
Yuichiro Nishibe ◽  
Hiroshi Isami ◽  
Hideki Fukuda ◽  
Shuhei Nishida ◽  
Toshi Nagata ◽  
...  

2012 ◽  
Vol 7 (sp) ◽  
pp. 491-499 ◽  
Author(s):  
Gaku Shoji ◽  
◽  
Dai Takahashi ◽  
Takuya Tsukiji ◽  
Satoshi Naba ◽  
...  

We collected data on the March 11, 2011, Great East Japan Earthquake by surveying web sites related to power failures during 2011 off the Pacific coast of Tohoku (northeastern Japan) and, in addition, by interviewing local government sectors and Tokyo Electric Power Company (TEPCO) branch office personnel. We quantify two damage ratios for power failures for subject municipalities defined by the ratio of the number of affected households and houses in a city to the number of related households and houses. This revealed the dependence of damage ratios on seismic intensities induced in subject municipalities. Damage functions related to power failures are then developed.


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