High-Resolution Mapping of Japanese Microplastic and Macroplastic Emissions from the Land Into the Sea
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Biogeography and Evolution of the Carassius Auratus-Complex in East
Takada et al. BMC Evolutionary Biology 2010, 10:7 http://www.biomedcentral.com/1471-2148/10/7 RESEARCH ARTICLE Open Access Biogeography and evolution of the Carassius auratus-complex in East Asia Mikumi Takada1,2*, Katsunori Tachihara1, Takeshi Kon2, Gunji Yamamoto2, Kei’ichiro Iguchi3, Masaki Miya4, Mutsumi Nishida2 Abstract Background: Carassius auratus is a primary freshwater fish with bisexual diploid and unisexual gynogenetic triploid lineages. It is distributed widely in Eurasia and is especially common in East Asia. Although several genetic studies have been conducted on C. auratus, they have not provided clear phylogenetic and evolutionary descriptions of this fish, probably due to selection bias in sampling sites and the DNA regions analysed. As the first step in clarifying the evolutionary entity of the world’s Carassius fishes, we attempted to clarify the phylogeny of C. auratus populations distributed in East Asia. Results: We conducted a detailed analysis of a large dataset of mitochondrial gene sequences [CR, 323 bp, 672 sequences (528 sequenced + 144 downloaded); CR + ND4 + ND5 + cyt b, 4669 bp in total, 53 sequences] obtained from C. auratus in East Asia. Our phylogeographic analysis revealed two superlineages, one distributed mainly among the Japanese main islands and the other in various regions in and around the Eurasian continent, including the Ryukyus and Taiwan. The two superlineages include seven lineages with high regional specificity that are composed of endemic populations indigenous to each region. The divergence time of the seven lineages was estimated to be 0.2 million years ago (Mya) by a fossil-based method and 1.0-1.9 Mya by the molecular clock method. -
Building Urban Resilience Through Spatial Planning Following Disasters
BUILDING URBAN RESILIENCE THROUGH SPATIAL PLANNING FOLLOWING DISASTERS THE GREAT EAST JAPAN EARTHQUAKE AND TSUNAMI DISSERTATION BY NADINE MÄGDEFRAU SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF ENGINEERING (DR.-ING.) AT THE FACULTY OF SPATIAL PLANING OF THE TECHNICAL UNIVERSITY OF DORTMUND DECEMBER 2016 Front Cover: Own illustration | Photo by author (October 2015) Doctoral Committee Supervisors PROF. DR. STEFAN GREIVING Technical University of Dortmund, Germany Faculty of Spatial Planning Institute of Spatial Planning PROF. DR. MICHIO UBAURA Tohoku University Department of Architecture and Building Science Urban and Regional Planning System Lab Examiner PROF. DR. SABINE BAUMGART Technical University of Dortmund, Germany Faculty of Spatial Planning Department of Urban and Regional Planning Dissertation at the Faculty of Spatial Planning of the Technical University of Dortmund, Dortmund. BUILDING URBAN RESILIENCE THROUGH SPATIAL PLANNING FOLLOWING DISASTERS THE GREAT EAST JAPAN EARTHQUAKE AND TSUNAMI DISSERTATION BY NADINE MÄGDEFRAU SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF ENGINEERING (DR.-ING.) AT THE FACULTY OF SPATIAL PLANING OF THE TECHNICAL UNIVERSITY OF DORTMUND DECEMBER 2016 ACKNOWLEDGMENT “It is complicated.” This is one of the phrases that I heard most frequently throughout my research in Tohoku Region. It referred to the reconstruction process, but can equally be applied to the endeavor of writing a dissertation. It was complicated to find an appropriate research topic. It was complicated to collect and understand the required data (mainly written in a foreign language) and to comprehend the complex processes that took and take place in Tohoku Region to recover from the Great East Japan Earthquake and Tsunami. -
Geography & Climate
Web Japan http://web-japan.org/ GEOGRAPHY AND CLIMATE A country of diverse topography and climate characterized by peninsulas and inlets and Geography offshore islands (like the Goto archipelago and the islands of Tsushima and Iki, which are part of that prefecture). There are also A Pacific Island Country accidented areas of the coast with many Japan is an island country forming an arc in inlets and steep cliffs caused by the the Pacific Ocean to the east of the Asian submersion of part of the former coastline due continent. The land comprises four large to changes in the Earth’s crust. islands named (in decreasing order of size) A warm ocean current known as the Honshu, Hokkaido, Kyushu, and Shikoku, Kuroshio (or Japan Current) flows together with many smaller islands. The northeastward along the southern part of the Pacific Ocean lies to the east while the Sea of Japanese archipelago, and a branch of it, Japan and the East China Sea separate known as the Tsushima Current, flows into Japan from the Asian continent. the Sea of Japan along the west side of the In terms of latitude, Japan coincides country. From the north, a cold current known approximately with the Mediterranean Sea as the Oyashio (or Chishima Current) flows and with the city of Los Angeles in North south along Japan’s east coast, and a branch America. Paris and London have latitudes of it, called the Liman Current, enters the Sea somewhat to the north of the northern tip of of Japan from the north. The mixing of these Hokkaido. -
Report on Rebuilding Flood-Conscious Societies in Small
Report on Rebuilding Flood-Conscious Societies in Small and Medium River Basins January 2017 Council for Social Infrastructure Development 1 Contents 1. Introduction - Accelerate Rebuilding Flood-Conscious Societies ............................... 3 2. Typhoons in the Hokkaido and Tohoku regions in August 2016 .................................. 5 2.1 Outline of Torrential Rains ........................................................................................ 5 2.2 Outline of Disaster Damage ....................................................................................... 6 2.3 Features of the Disasters ............................................................................................ 7 3. Small and Medium River Basins under Changing Climate and Declining Populations ................................................................................................................................................ 9 4. Key Activities Based on the Report of December 2015 ................................................ 11 5. Key Challenges to be addressed..................................................................................... 13 6. Measures Needed in Small and Medium River Basins ................................................ 15 6.1 Basic Policy ................................................................................................................ 15 6.2 Measures to be taken ................................................................................................ 17 7. Conclusion ...................................................................................................................... -
March 2011 Earthquake, Tsunami and Fukushima Nuclear Accident Impacts on Japanese Agri-Food Sector
Munich Personal RePEc Archive March 2011 earthquake, tsunami and Fukushima nuclear accident impacts on Japanese agri-food sector Bachev, Hrabrin January 2015 Online at https://mpra.ub.uni-muenchen.de/61499/ MPRA Paper No. 61499, posted 21 Jan 2015 14:37 UTC March 2011 earthquake, tsunami and Fukushima nuclear accident impacts on Japanese agri-food sector Hrabrin Bachev1 I. Introduction On March 11, 2011 the strongest recorded in Japan earthquake off the Pacific coast of North-east of the country occurred (also know as Great East Japan Earthquake, 2011 Tohoku earthquake, and the 3.11 Earthquake) which triggered a powerful tsunami and caused a nuclear accident in one of the world’s largest nuclear plant (Fukushima Daichi Nuclear Plant Station). It was the first disaster that included an earthquake, a tsunami, and a nuclear power plant accident. The 2011 disasters have had immense impacts on people life, health and property, social infrastructure and economy, natural and institutional environment, etc. in North-eastern Japan and beyond [Abe, 2014; Al-Badri and Berends, 2013; Biodiversity Center of Japan, 2013; Britannica, 2014; Buesseler, 2014; FNAIC, 2013; Fujita et al., 2012; IAEA, 2011; IBRD, 2012; Kontar et al., 2014; NIRA, 2013; TEPCO, 2012; UNEP, 2012; Vervaeck and Daniell, 2012; Umeda, 2013; WHO, 2013; WWF, 2013]. We have done an assessment of major social, economic and environmental impacts of the triple disaster in another publication [Bachev, 2014]. There have been numerous publications on diverse impacts of the 2011 disasters including on the Japanese agriculture and food sector [Bachev and Ito, 2013; JA-ZENCHU, 2011; Johnson, 2011; Hamada and Ogino, 2012; MAFF, 2012; Koyama, 2013; Sekizawa, 2013; Pushpalal et al., 2013; Liou et al., 2012; Murayama, 2012; MHLW, 2013; Nakanishi and Tanoi, 2013; Oka, 2012; Ujiie, 2012; Yasunaria et al., 2011; Watanabe A., 2011; Watanabe N., 2013]. -
Japan Geoscience Union Meeting 2009 Presentation List
Japan Geoscience Union Meeting 2009 Presentation List A002: (Advances in Earth & Planetary Science) oral 201A 5/17, 9:45–10:20, *A002-001, Science of small bodies opened by Hayabusa Akira Fujiwara 5/17, 10:20–10:55, *A002-002, What has the lunar explorer ''Kaguya'' seen ? Junichi Haruyama 5/17, 10:55–11:30, *A002-003, Planetary Explorations of Japan: Past, current, and future Takehiko Satoh A003: (Geoscience Education and Outreach) oral 301A 5/17, 9:00–9:02, Introductory talk -outreach activity for primary school students 5/17, 9:02–9:14, A003-001, Learning of geological formation for pupils by Geological Museum: Part (3) Explanation of geological formation Shiro Tamanyu, Rie Morijiri, Yuki Sawada 5/17, 9:14-9:26, A003-002 YUREO: an analog experiment equipment for earthquake induced landslide Youhei Suzuki, Shintaro Hayashi, Shuichi Sasaki 5/17, 9:26-9:38, A003-003 Learning of 'geological formation' for elementary schoolchildren by the Geological Museum, AIST: Overview and Drawing worksheets Rie Morijiri, Yuki Sawada, Shiro Tamanyu 5/17, 9:38-9:50, A003-004 Collaborative educational activities with schools in the Geological Museum and Geological Survey of Japan Yuki Sawada, Rie Morijiri, Shiro Tamanyu, other 5/17, 9:50-10:02, A003-005 What did the Schoolchildren's Summer Course in Seismology and Volcanology left 400 participants something? Kazuyuki Nakagawa 5/17, 10:02-10:14, A003-006 The seacret of Kyoto : The 9th Schoolchildren's Summer Course inSeismology and Volcanology Akiko Sato, Akira Sangawa, Kazuyuki Nakagawa Working group for -
Durham E-Theses
Durham E-Theses Transience and durability in Japanese urban space ROBINSON, WILFRED,IAIN,THOMAS How to cite: ROBINSON, WILFRED,IAIN,THOMAS (2010) Transience and durability in Japanese urban space, Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/405/ Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in Durham E-Theses • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk Iain Robinson Transience and durability in Japanese urban space ABSTRACT The thesis addresses the research question “What is transient and what endures within Japanese urban space” by taking the material constructed form of one Japanese city as a primary text and object of analysis. Chiba-shi is a port and administrative centre in southern Kanto, the largest city in the eastern part of the Tokyo Metropolitan Region and located about forty kilometres from downtown Tokyo. The study privileges the role of process as a theoretical basis for exploring the dynamics of the production and transformation of urban space. -
Zootaxa, Japanese Pseudosmittia Edwards (Diptera: Chironomidae)
Zootaxa 1198: 21–51 (2006) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ ZOOTAXA 1198 Copyright © 2006 Magnolia Press ISSN 1175-5334 (online edition) Japanese Pseudosmittia Edwards (Diptera: Chironomidae) OLE A. SÆTHER The Natural History Collections, Bergen Museum, University of Bergen, N-5020 Bergen, Norway. E-mail: [email protected] Abstract The types of species previously placed in Pseudosmittia Edwards and some related genera in the Sasa collection at The National Museum of Sciences, Tokyo, Japan, have been examined. Twenty- four new synonyms are given: Pseudosmittia ogasatridecima Sasa et Suzuki, 1997a is a synonym of P. bifurcata (Tokunaga, 1936); P. jintuvicesima Sasa, 1996, and P. seiryupequea Sasa, Suzuki et Sakai, 1998 of P. danconai (Marcuzzi, 1947); P. mongolzeaea Sasa et Suzuki, 1997b of P. f orc ipa ta (Goetghebuer, 1921); P. hachijotertia Sasa, 1994 of P. holsata Thienemann et Strenzke, 1940; P. itachibifurca Sasa et Kawai, 1987, P. furudobifurca Sasa et Arakawa, 1994, P. hibaribifurca Sasa, 1993, and P. (Nikismittia) shofukuundecima Sasa, 1998 of P. mathildae Albu, 1968; P. yakymenea Sasa et Suzuki, 2000a, and P. yakyneoa Sasa et Suzuki, 2000a of P. nishiharaensis Sasa et Hasegawa, 1988; P. kurobeokasia Sasa et Okazawa, 1992a, P. togarisea Sasa et Okazawa, 1992b, P. hachijosecunda Sasa, 1994, P. to ya m a re s e a Sasa, 1996, P. yakyopea Sasa et Suzuki, 2000a, P. yakypequea Sasa et Suzuki, 2000a, Parakiefferiella hidakagehea Sasa et Suzuki, 2000b, and Parakiefferiella hidakaheia Sasa et Suzuki, 2000b of Pseudosmittia oxoniana (Edwards, 1922); P. famikelea Sasa, 1996a of P. tokaraneoa Sasa et Suzuki, 1995; P. -
Flood Loss Model Model
GIROJ FloodGIROJ Loss Flood Loss Model Model General Insurance Rating Organization of Japan 2 Overview of Our Flood Loss Model GIROJ flood loss model includes three sub-models. Floods Modelling Estimate the loss using a flood simulation for calculating Riverine flooding*1 flooded areas and flood levels Less frequent (River Flood Engineering Model) and large- scale disasters Estimate the loss using a storm surge flood simulation for Storm surge*2 calculating flooded areas and flood levels (Storm Surge Flood Engineering Model) Estimate the loss using a statistical method for estimating the Ordinarily Other precipitation probability distribution of the number of affected buildings and occurring disasters related events loss ratio (Statistical Flood Model) *1 Floods that occur when water overflows a river bank or a river bank is breached. *2 Floods that occur when water overflows a bank or a bank is breached due to an approaching typhoon or large low-pressure system and a resulting rise in sea level in coastal region. 3 Overview of River Flood Engineering Model 1. Estimate Flooded Areas and Flood Levels Set rainfall data Flood simulation Calculate flooded areas and flood levels 2. Estimate Losses Calculate the loss ratio for each district per town Estimate losses 4 River Flood Engineering Model: Estimate targets Estimate targets are 109 Class A rivers. 【Hokkaido region】 Teshio River, Shokotsu River, Yubetsu River, Tokoro River, 【Hokuriku region】 Abashiri River, Rumoi River, Arakawa River, Agano River, Ishikari River, Shiribetsu River, Shinano -
Japan: Tokai Heavy Rain (September 2000)
WORLD METEOROLOGICAL ORGANIZATION THE ASSOCIATED PROGRAMME ON FLOOD MANAGEMENT INTEGRATED FLOOD MANAGEMENT CASE STUDY1 JAPAN: TOKAI HEAVY RAIN (SEPTEMBER 2000) January 2004 Edited by TECHNICAL SUPPORT UNIT Note: Opinions expressed in the case study are those of author(s) and do not necessarily reflect those of the WMO/GWP Associated Programme on Flood Management (APFM). Designations employed and presentations of material in the case study do not imply the expression of any opinion whatever on the part of the Technical Support Unit (TSU), APFM concerning the legal status of any country, territory, city or area of its authorities, or concerning the delimitation of its frontiers or boundaries. WMO/GWP Associated Programme on Flood Management JAPAN: TOKAI HEAVY RAIN (SEPTEMBER 2000) Ministry of Land, Infrastructure and Transport, Japan 1. Place 1.1 Location Positions in the flood inundation area caused by the Tokai heavy rain: Nagoya City, Aichi Prefecture is located at 35° – 35° 15’ north latitude, 136° 45’ - 137° east longitude. The studied area is Shonai and Shin river basin- hereinafter referred to as the Shonai river system. It locates about the center of Japan including Nagoya city area, 5th largest city in Japan with the population about 3millions. Therefore, two rivers flow through densely populated area and into the Pacific Ocean and are typical city-type rivers in Japan. Shin Riv. Border of basin Shonai Riv. Flooding area Point of breach ●Peak flow rate in major points on Sept. 12 (app. m3/s) ← Nagoya City, ← ← ino ino Aichi Prefecture j Ku ← 1,100 Shin Riv. ← 720 ← → ← ima Detention j Basin Shinkawa Araizeki Shidami Biwa (Fixed dam) Shin Riv. -
Japanese Geography Quiz What Prefecture Is Located in the Northernmost Part in Japan?
Japanese Geography Quiz What prefecture is located in the northernmost part in Japan? ① Hokkaido ② Aomori ③ Akita ④ Ishikawa What prefecture is located in the northernmost part in Japan? ① Hokkaido ② Aomori ③ Akita ④ Ishikawa What prefecture is located in the westernmost part in Japan? ① Okinawa ② Nagasaki ③ Osaka ④ Kagoshima What prefecture is located in the westernmost part in Japan? ① Okinawa ② Nagasaki ③ Osaka ④ Kagoshima What is the name of the island located in the southernmost part of Japan? ① Yaku Island ② Marcus Island ③ Okinawa Island ④ Okinotori Islands What is the name of the island located in the southernmost part of Japan? ① Yaku Island ② Marcus Island ③ Okinawa Island ④ Okinotori Islands What is the name of the island located in the easternmost part of Japan? ① Father Island ② Okinotori Islands ③ Marcus Island ④ Mother Island What is the name of the island located in the easternmost part of Japan? ① Father Island ② Okinotori Islands ③ Marcus Island ④ Mother Island What mountain is the second highest in Japan following Mt. Fuji? ① Yatsugatake Mountains ② Mt. Hotaka ③ Monte Yari ④ Mt. Kita (Shirane) What mountain is the second highest in Japan following Mt. Fuji? ① Yatsugatake Mountains ② Mt. Hotaka ③ Monte Yari ④ Mt. Kita (Shirane) How high is Mt.Fuji, the highest mountain in Japan? ① 1,776 meters ② 2,776 meters ③ 3,776 meters ④ 4,776 meters How high is Mt.Fuji, the highest mountain in Japan? ① 1,776 meters ② 2,776 meters ③ 3,776 meters ④ 4,776 meters What is the longest river in Japan? ① Shinano River ② Tone River ③ Ishikari -
Major Damage & Recovery in MLIT Tohoku Regional Bureau
青森県 Major Damage & Recovery in MLIT Tohoku Regional Bureau (as of 14:00 23 March 2011) Rivers under MLIT’s jurisdiction Coast ・ Severe damages requiring emergent ・Coastal levees of 190 km recovery before next flood Mabuchi R. 12 points Inundated area on 12-13 March fully/partially destroyed ・ 22 points, including 11 under survey and (among 300km) Iwate Pref. 11 under recovering works (The numbers Sendai Bay South Area (MLIT) may increase around river mouth areas) 3km2 coastal area in Iwate Abukuma R. 6 under survey Kitamkami R. 10 on recovering Naruse R. 6 Kitakami R. river水系名 system 被災箇所数damage 419 points ・Totally 718 Mabechi馬淵川 R. 12 damages 阿武隈川 123 Abukuma R. Recovered quickly to rescue an isolated in Tohoku Natori名取川 R. 27 赤川 settlement Kitakami R. Right Bank 4km from the sea 北上川 最上川419 Miyagi region Kitakami R. (Ishinomaki City, Miyagi Pref.) Naruse鳴瀬川 R. 137 Pref. total計 718 Naruse R. 137 points Sabo ・13 sediment disaster points, recovered temporarily on outstanding deformations Natori R. 2 Prefecture県名 被災件数points 27 points 113km coastal area in Miyagi Completed on 青森県Aomori 1 14 March 宮城県Miyagi 1 Fukushima福島県 11 total計 13 37km2 coastal area in Fukushima Hanokidaira (Shirakawa City, Fukushima Pref.) Abukuma R. Naruse R. Left Bank 30km from the sea Landslide 123 points (Osaki City, Miyagi Pref.) Severe damage to be recovered quiklickly (River ) Fukushima Severe damage to be recovered quickly (Sabo) Pref. to reduce flood risk on lives/assets Dike deformation Sediment disaster 12 dead and 1 missed on 11 march Inundation area (on 12‐13 March) 1 Major Damage & Recovery in MLIT Kanto Regional Bureau (as of 14:00 23 March 2011) Kawanishi (Nasukarasuma City, Tochigi) Rivers under MLIT’s jurisdiction Sabo 地すべり ・Severe damages requiring emergent ・25 sediment disaster points, recovered temporarily on recovery before next flood Naka R.