Acute Appendicitis Associated with the Presence of Schistosome Eggs in A
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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]. -
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 -
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 -
Damage Patterns of River Embankments Due to the 2011 Off
Soils and Foundations 2012;52(5):890–909 The Japanese Geotechnical Society Soils and Foundations www.sciencedirect.com journal homepage: www.elsevier.com/locate/sandf Damage patterns of river embankments due to the 2011 off the Pacific Coast of Tohoku Earthquake and a numerical modeling of the deformation of river embankments with a clayey subsoil layer F. Okaa,n, P. Tsaia, S. Kimotoa, R. Katob aDepartment of Civil & Earth Resources Engineering, Kyoto University, Japan bNikken Sekkei Civil Engineering Ltd., Osaka, Japan Received 3 February 2012; received in revised form 25 July 2012; accepted 1 September 2012 Available online 11 December 2012 Abstract Due to the 2011 off the Pacific Coast of Tohoku Earthquake, which had a magnitude of 9.0, many soil-made infrastructures, such as river dikes, road embankments, railway foundations and coastal dikes, were damaged. The river dikes and their related structures were damaged at 2115 sites throughout the Tohoku and Kanto areas, including Iwate, Miyagi, Fukushima, Ibaraki and Saitama Prefectures, as well as the Tokyo Metropolitan District. In the first part of the present paper, the main patterns of the damaged river embankments are presented and reviewed based on the in situ research by the authors, MLIT (Ministry of Land, Infrastructure, Transport and Tourism) and JICE (Japan Institute of Construction Engineering). The main causes of the damage were (1) liquefaction of the foundation ground, (2) liquefaction of the soil in the river embankments due to the water-saturated region above the ground level, and (3) the long duration of the earthquake, the enormity of fault zone and the magnitude of the quake. -
Chiba Travel
ChibaMeguri_sideB Leisure Shopping Nature History&Festival Tobu Noda Line Travel All Around Chiba ChibaExpressway Joban Travel Map MAP-H MAP-H Noda City Tateyama Family Park Narita Dream Farm MITSUI OUTLET PARK KISARAZU SHISUI PREMIUM OUTLET® MAP-15 MAP-24 Express Tsukuba Isumi Railway Naritasan Shinshoji Temple Noda-shi 18 MAP-1 MAP-2 Kashiwa IC 7 M22 Just within a stone’s throw from Tokyo by the Aqua Line, Nagareyama City Kozaki IC M24 Sawara Nagareyama IC Narita Line 25 Abiko Kozaki Town why don’t you visit and enjoy Chiba. Kashiwa 26 Sawara-katori IC Nagareyama M1 Abiko City Shimosa IC Whether it is for having fun, soak in our rich hot springs, RyutetsuNagareyamaline H 13 Kashiwa City Sakae Town Tobu Noda Line Minami Nagareyama Joban Line satiate your taste bud with superior products from the seas 6 F Narita City Taiei IC Tobu Toll Road Katori City Narita Line Shin-Matsudo Inzai City Taiei JCT Shiroi City Tonosho Town and mountains, Chiba New Town M20 Shin-Yahashira Tokyo Outer Ring Road Higashikanto Expressway Hokuso Line Shibayama Railway Matsudo City Inba-Nichi-idai Narita Sky Access Shin-Kamagaya 24 you can enjoy all in Chiba. Narita Narita Airport Tako Town Tone Kamome Ohashi Toll Road 28 34 Narita IC Musashino Line I Shibayama-Chiyoda Activities such as milking cows or making KamagayaShin Keisei City Line M2 All these conveniences can only be found in Chiba. Naritasan Shinshoji Temple is the main temple Narita International Airport Asahi City butter can be experienced on a daily basis. Narita Line Tomisato IC Ichikawa City Yachiyo City of the Shingon Sect of Chizan-ha Buddhism, Funabashi City Keisei-Sakura Shisui IC You can enjoy gathering poppy , gerbera, Additionally, there are various amusement DATA 398, Nakajima, Kisarazu-City DATA 689 Iizumi, Shisui-Town Sobu LineKeisei-Yawata Shibayama Town M21 Choshi City Isumi and Kominato railroad lines consecutively run across Boso Peninsula, through a historical Choshi 32 and antirrhinum all the year round in the TEL:0438-38-6100 TEL:043-481-6160 which was established in 940. -
Water Resource Assessment of Yodo River Basin Using Coupled Hydrometeorological Modeling Approach
Water Resource Assessment of Yodo River Basin Using Coupled Hydrometeorological Modeling Approach (気気気象象象水水水文文文統統統合合合モモモデデデルルル手手手法法法ををを用用用いいいたたた淀淀淀川川川流流流域域域ののの水水水循循循環環環評評評価価価) A Thesis Submitted to the Graduate School of Engineering, Osaka University in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Engineering Kundan Lal Shrestha (クククンンンダダダンンン ラララルルル セセセレレレスススタタタ) January 2010 Division of Sustainable Energy and Environmental Engineering, Graduate School of Engineering, Osaka University, Japan CONTENTS 1 introduction1 1.1 Background 1 1.2 Purpose of research 8 1.2.1 Major objectives 8 1.2.2 Importance of the study 9 1.3 Methodology 10 1.4 Chapter organization 11 2 literature review 15 2.1 Mesocale meteorological modeling approach 15 2.2 Effect of urban heat island on basin hydroclimate 19 2.3 Hydrological modeling for river basins 22 2.4 Coupled hydrometeorological modeling approach 26 2.5 Impact of climate change on water cycle 33 2.6 Integrated approach for water resource assessment of Yodo River basin 36 3 model descriptions 37 3.1 Meteorological models 37 3.1.1 MM5 mesoscale model 39 3.1.2 WRF mesoscale model 39 3.2 Urban canopy model 40 3.3 Hydrological model 40 3.3.1 Distributed hydrological model 40 3.3.2 Surface energy balance model 42 3.3.3 HydroBEAM runoff model 44 3.3.4 Snowfall and Snowmelt 49 3.3.5 Dam operation model 49 4 validation and analysis of meteorological models 53 4.1 Introduction 53 4.2 Domain and grid structures 54 iii iv contents 4.3 Input data 54 4.3.1 Observation stations 54 -
Dispersion of Cs-134 and Cs-137 in River Waters from Fukushima And
DOI: 10.15669/pnst.4.9 Progress in Nuclear Science and Technology Volume 4 (2014) pp. 9-13 ARTICLE Dispersion of Cs-134 and Cs-137 in river waters from Fukushima and Gunma prefectures at nine months after the Fukushima Daiichi NPP accident Seiya Nagaoa*, Masaki Kanamorib, Shinya Ochiaia, Kyuma Suzukic and Masayoshi Yamamotoa a Low Level Radioactivity Laboratory, Kanazawa University, 24 O, Wake, Nomi-shi, Ishikawa-ken, 923-1224, Japan; b Graduate School of Nature and Environmental Technology, Kanazawa University, Kakuma, Kanazawa-shi, Ishikawa-ken, 920-1192, Japan; c Gunma Prefectural Fisheries Experimental Station, 13 Shikishima, Maebashi-shi, Gunma-ken, 371-1036, Japan To estimate short-term and long-term impacts of radiation dose, dynamics of 134Cs and 137Cs in river watershed environments were studied in Fukushima and Gunma prefectures at nine months after the Fukushima Daiichi Nuclear Power Plant (NPP) accident. Radioactivity of 134Cs and 137Cs in the river waters ranged respectively from 0.007 Bq/l to 0.149 Bq/l and 0.008 Bq/l to 0.189 Bq/l. Their horizontal distributions were consistent with those of material that had been deposited on the ground surface. The percentages of particulate forms of 134Cs and 137Cs were 56–89% for the Fukushima river samples. Results show that the transport of 134Cs and 137Cs from the watershed to the river waters occurred mainly as particulate forms and that their radioactivity depends on the levels of radioactivity at the watersheds of the respective river systems. Keywords: 134Cs; 137Cs; radiocesium; existence forms; lake waters; transport behavior 1. Introduction1 2. -
Topographic Mapping Using Satellite Images • Total: 4,355 Sheets
1:25,000 scale topographic maps • Largest scale base maps that cover whole land of Japan Topographic mapping using satellite images • Total: 4,355 sheets • 1 sheet covers: longitude 7.5 min. latitude 5 min. (about 100km2) Geospatial Information Authority of Japan 3 Fundamental maps in Japan Photogrammetry Paper-based maps - Scale: 1:10,000 ~ 1:5,000,000 - Mainly: 1:25,000 scale topographic map Digital maps “Kunikaze III” - Digital Japan Basic Maps (Map Information) - Map image - Spatial data framework (2500, 25000) - Etc. Providing - Publishing (paper, CD-ROM, etc.) - Browse via the Internet - Download through the Internet (Map Image) 2 Aerial photographs (with 60% overwrapping) 4 1 2 Flight course Advanced Land Observing Satellite(ALOS) 㻢㻜㻑㻌㼛㼢㼑㼞㼣㼞㼍㼜㻌㼎㼑㼠㼣㼑㼑㼚㻌㼚㼑㼕㼓㼔㼎㼛㼞㼕㼚㼓㻌㼜㼔㼛㼠㼛 PRISM 2.5m-spatial resolution 㻟㻜㻑㻌㼛㼢㼑㼞㼣㼞㼍㼜㻌㼎㼑㼠㼣㼑㼑㼚㻌㼚㼑㼕㼓㼔㼎㼛㼞㼕㼚㼓㻌㼏㼛㼡㼞㼟㼑 three optical system 㻢㻜㻑 Panchromatic sensor Launch : January 24th in 2006 AVNIR-2 Missions 10m-spatial resolution •cartography Multi-band(BGRNIR䠅sensor 㻟㻜㻑 •regional observation •disaster monitoring •resource surveying PALSAR 10m-spatial resolution L-band SAR From JAXA HP 5 7 Photogrammetry -Principle- Comparison of aerial photo & satellite image Using Aerial Photograph ALOS PRISM plotter Resolution 40cm 2.5m Interval of 1-5 year (GSI) 46 days Images Shooting Shooting 5km㽢5km 35km X 35km Area 䠄Scale 1:20,000䠅 35km X 70km Others Hard to take at Hard to interpret isolated islands, small structures & volcanoes etc. point features 3D model (lighthouses, towers, road dividers etc.) 6 8 3 4 Example -
A New Subspecies of Anadromous Far Eastern Dace, Tribolodon Brandtii Maruta Subsp
Bull. Natl. Mus. Nat. Sci., Ser. A, 40(4), pp. 219–229, November 21, 2014 A New Subspecies of Anadromous Far Eastern Dace, Tribolodon brandtii maruta subsp. nov. (Teleostei, Cyprinidae) from Japan Harumi Sakai1 and Shota Amano2 1 Department of Applied Aquabiology, National Fisheries University, 2–7–1 Nagata-honmachi, Shimonoseki, Yamaguchi 759–6595, Japan E-mail: sakaih@fish-u.ac.jp 2 Alumnus, Graduate School of National Fisheries University, 2–7–1 Nagata-honmachi, Shimonoseki, Yamaguchi 759–6595, Japan E-mail: fi[email protected] (Received 7 July 2014; accepted 24 September 2014) Abstract Tribolodon brandtii maruta subsp. nov. is described from the holotype and 29 para- types. The subspecies differs from congeners and the other subspecies in the following combina- tion of characters: preoperculo-mandibular canal of the cephalic lateral line system extended dor- sally and connected with postocular commisure, dorsal profile of snout gently rounded, lateral line scales 73–87, scales above lateral line 12–17, scales below lateral line 9–14, predorsal scales 34–41. The new subspecies is distributed on the Pacific coast of Honshu Island from Tokyo Bay to Ohfunato Bay, Iwate Prefecture, Japan. Key words : new subspecies, taxonomy, morphology, anadromy, cephalic lateral line system. the former having fewer scales and being sug- Introduction gested to have a greater salinity tolerance than The Far Eastern dace genus Tribolodon (Tele- the latter (Nakamura, 1969). An allozyme allelic ostei, Cyprinidae), well-known for exhibiting displacement with no hybridization trait between both freshwater and anadromous modes of life the Maruta form from Tokyo Bay and Ohfunato (Berg, 1949; Aoyagi, 1957; Nakamura, 1963, Bay, Iwate Prefecture and the Jusan-ugui form 1969; Kurawaka, 1977; Sakai, 1995), includes from Hokkaido, Yamagata and Niigata Prefec- four species, two freshwater [T. -
A Study of Earthquake-Caused Liquefaction: the Case of Urayasu City
Earthquake–Soil Interaction 149 A study of earthquake-caused liquefaction: the case of Urayasu City S. Kamao1, M. Takezawa1, K. Yamada1, S. Jinno1, T. Shinoda1 & E. Fukazawa2 1Department of Civil Engineering, Nihon University, Japan 2Environmental Control Center Co. Ltd., Japan Abstract Soil liquefaction describes a phenomenon whereby saturated soil loses a substantial part of its strength and stiffness in response to an applied stress, usually from earthquake shaking or another sudden change in stress conditions, causing it to behave like a liquid. Liquefaction caused by the Great East Japan Earthquake of 2011 occurred on reclaimed land around the Tokyo Bay area. Urayasu City suffered extensive damage from liquefaction triggered by the earthquake, and effects of the disaster are still ongoing. This paper describes some remarkable damage to structures produced by liquefaction induced by the earthquake and indicates the potential for liquefaction using current determination methods on published soil profiles and N values from standard penetration tests, and introduces a measurement method (the grid-form underground wall method) that will be adopted in Urayasu City. The authors also conducted a series of laboratory liquefaction tests (cyclic undrained triaxial testing) to clarify the area’s liquefaction characteristics using sand taken from a site in Urayasu City that experienced liquefaction. Keywords: earthquake, liquefaction, Urayasu City, damage types, liquefaction strength, measure for liquefaction. 1 Introduction The Great East Japan Earthquake (Mw = 9.0) occurred on March 11, 2011. Its epicentre was about 130 km away from the coast of Tohoku. Fig. 1 shows the seismic intensity observed in various parts of Japan. It illustrates that the earthquake was felt over much of Japan.