The World Bank Group and Japan" Falls Naturally Into Two Compart Ments
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Outdoor Club Japan (OCJ) 国際 アウトドア・クラブ・ジャパン Events
Outdoor Club Japan (OCJ) 国際 アウトドア・クラブ・ジャパン Events Norikuradake Super Downhill 10 March Friday to 12 March Monday If you are not satisfied ski & snowboard in ski area. You can skiing from summit. Norikuradake(3026m)is one of hundred best mountain in Japan. This time is good condition of backcountry ski season. Go up to the summit of Norikuradake by walk from the top of last lift(2000m). Climb about 5 hours and down to bottom lift(1500m) about 50 min. (Deta of last time) Transport: Train from Shinjuku to Matsumoto and Taxi from Matsumoto to Norikura-kogen. Return : Bus from Norikura-kogen to Sinshimashima and train to Shinjuku. Meeting Time & Place : 19:30 Shijuku st. platform 5 car no.1 for super Azusa15 Cost : About Yen30000 Train Shinjuku to matsumoto Yen6200(ow) but should buy 4coupon ticket each coupon Yen4190 or You can buy discount ticket shop in town price is similar. (price is non-reserve seat) Taxi about Yen13000 we will share. Return bus Yen1300 and local train Yen680. Inn Yen14000+tax 2 overnight 2 breakfast 1 dinner (no dinner Friday) Japanese room and hot spring! Necessary equipment : Skiers & Telemarkers need a nylon mohair skin. Snowboarders need snowshoes. Crampons(over 8point!) Clothes: Gore-tex jacket and pants, fleece, hut, musk, gloves, sunglasses, headlamp, thermos, lunch, sunscreen If you do not go up to the summit, you can enjoy the ski area and hot springs. 1 day lift pass Yen4000 Limit : 12persons (priority is downhill from summit) In Japanese : 026m)の頂上からの滑降です。 ゲレンデスキーに物足りないスキーヤー、スノーボーダー向き。 山スキーにいいシーズンですが、天気次第なので一応土、日と2日間の時間をとりました。 -
Vol2 Case History English(1-206)
Renewal & Upgrading of Hydropower Plants IEA Hydro Technical Report _______________________________________ Volume 2: Case Histories Report March 2016 IEA Hydropower Agreement: Annex XI AUSTRALIA USA Table of contents㸦Volume 2㸧 ࠙Japanࠚ Jp. 1 : Houri #2 (Miyazaki Prefecture) P 1 㹼 P 5ۑ Jp. 2 : Kikka (Kumamoto Prefecture) P 6 㹼 P 10ۑ Jp. 3 : Hidaka River System (Hokkaido Electric Power Company) P 11 㹼 P 19ۑ Jp. 4 : Kurobe River System (Kansai Electric Power Company) P 20 㹼 P 28ۑ Jp. 5 : Kiso River System (Kansai Electric Power Company) P 29 㹼 P 37ۑ Jp. 6 : Ontake (Kansai Electric Power Company) P 38 㹼 P 46ۑ Jp. 7 : Shin-Kuronagi (Kansai Electric Power Company) P 47 㹼 P 52ۑ Jp. 8 : Okutataragi (Kansai Electric Power Company) P 53 㹼 P 63ۑ Jp. 9 : Okuyoshino / Asahi Dam (Kansai Electric Power Company) P 64 㹼 P 72ۑ Jp.10 : Shin-Takatsuo (Kansai Electric Power Company) P 73 㹼 P 78ۑ Jp.11 : Yamasubaru , Saigo (Kyushu Electric Power Company) P 79 㹼 P 86ۑ Jp.12 : Nishiyoshino #1,#2(Electric Power Development Company) P 87 㹼 P 99ۑ Jp.13 : Shin-Nogawa (Yamagata Prefecture) P100 㹼 P108ۑ Jp.14 : Shiroyama (Kanagawa Prefecture) P109 㹼 P114ۑ Jp.15 : Toyomi (Tohoku Electric Power Company) P115 㹼 P123ۑ Jp.16 : Tsuchimurokawa (Tokyo Electric Power Company) P124㹼 P129ۑ Jp.17 : Nishikinugawa (Tokyo Electric Power Company) P130 㹼 P138ۑ Jp.18 : Minakata (Chubu Electric Power Company) P139 㹼 P145ۑ Jp.19 : Himekawa #2 (Chubu Electric Power Company) P146 㹼 P154ۑ Jp.20 : Oguchi (Hokuriku Electric Power Company) P155 㹼 P164ۑ Jp.21 : Doi (Chugoku Electric Power Company) -
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. -
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 -
Toyama Bay, Japan
A Case Study Report on Assessment of Eutrophication Status in Toyama Bay, Japan Northwest Pacific Region Environmental Cooperation Center July 2011 Contents 1. Scope of the assessment........................................................................................................................................................... 1 1.1 Objective of the assessment .................................................................................................................................... 1 1.2 Selection of assessment area................................................................................................................................... 1 1.3 Collection of relevant information.......................................................................................................................... 3 1.4 Selection of assessment parameters........................................................................................................................ 4 1.4.1 Assessment categories of Toyama Bay case study ....................................................................................4 1.4.2 Assessment parameters of Toyama Bay case study...................................................................................4 1.5 Setting of sub-areas .................................................................................................................................................. 4 2. Data processing........................................................................................................................................................................ -
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 -
Translation Series No.1039
r,ARCHIVES FISHERIES RESEARCH BOARD OF CANADA Translation Series No. 1039 Artificial propagation of salmon in Japan By T. Mihara, S. Sano and H. Eguchi °evesYI,d0111 Yleletle i at-ti seeçsseneto, g. Gees, OeteNt Original title: Sake, Masu Jinkoo-fuka Jigyo. From: Booklet No. 5. Vol. 5 of the series on the propagation of the marine products. Published by: Nihon Suisanshigen Hogo Kyookai (The Japan , Soc. of the marine products protection), Vol. 5, July 25, pp. 2-60, 1964. Translated by the Translation Bureau(TM) Foreign Languages Division Department of the Secretary of State of Canada Fisheries Research Board of Canada Biological Station, Nanaimo, B.C. 1968 87 pages typescript F.L. i of,43zf 771-1. .:,emorandum (memorandum 1) To the Client r/\)/(-22N2 From the translator: 1) I could not find reasonable corresponding English f'or the following Japanese. iuseiha p. 27 (original p. 27) mihooshutsuran p.29 ( p. 28) tamasuling=22 (fishing net) p.57 ( p. 46) T isada (fishing implement) p. 57 ( p. 46) am now asking for the right translation to the author and as soon as I g et a answer I shall be glad to inform you. 2) Recently I found a new booklet (published in Dec. 1967), which you might be interest in it, ai the library of the Fisheries Department. This booklet is the vol. 14 of the same series of books. The vol.5 is rather introductly and vol. 14 imore scientific. The title and contents a:.- e as follows; T.LAkita, S. Sano and K. Taguchi: Propaqation of the Chum Salmon in Japan I. -
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. -
Abstruct (PDF 78KB)
Report of Riverfront Research Institute No.18 ABSTRUCT September, 2007 Foundation for Riverfront Improvement and Restoration Experimental research on restoration of the gravel bed of the Makomanai River, Sapporo Hokkaido (interim report) Hiroki TAKAHASHI/Noboru MARUOKA/Kiyoshi TAKEUCHI/Keizou WATANABE The Makomanai River has many rock-bedded sections where the bedrock has been exposed as a result riverbed degradation. This is thought to have been caused by a combined effect of the narrow valley flat, soft rock, decreases in sediment supply due to the check dams constructed in the 1980s, and the fixed water route of the river due to the river improvement carried out in the 1960s. The rock-bedded river channel, lacks river structures created by gravel (sediment) transport and scour–deposition processes and does not have shallows or pools suitable as habitat for benthos and fishes. Flood control problems caused by the scouring of revetment foundations are another matter of concern. This study is underway, therefore, on technical measures to restore the gravel bed of the Makomanai River based on adaptive management approach. In this study, a series of model experiments was conducted on various structures and configurations of facilities for accelerating gravel deposition, and, according to the experiment results, possible structures and configurations of experimental facilities were narrowed down and on-site experiments were conducted. Then, after monitoring-based verification, measures to be taken to restore the gravel bed of the Makomanai -
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 -
A Synopsis of the Parasites from Cyprinid Fishes of the Genus Tribolodon in Japan (1908-2013)
生物圏科学 Biosphere Sci. 52:87-115 (2013) A synopsis of the parasites from cyprinid fishes of the genus Tribolodon in Japan (1908-2013) Kazuya Nagasawa and Hirotaka Katahira Graduate School of Biosphere Science, Hiroshima University Published by The Graduate School of Biosphere Science Hiroshima University Higashi-Hiroshima 739-8528, Japan December 2013 生物圏科学 Biosphere Sci. 52:87-115 (2013) REVIEW A synopsis of the parasites from cyprinid fishes of the genus Tribolodon in Japan (1908-2013) Kazuya Nagasawa1)* and Hirotaka Katahira1,2) 1) Graduate School of Biosphere Science, Hiroshima University, 1-4-4 Kagamiyama, Higashi-Hiroshima, Hiroshima 739-8528, Japan 2) Present address: Graduate School of Environmental Science, Hokkaido University, N10 W5, Sapporo, Hokkaido 060-0810, Japan Abstract Four species of the cyprinid genus Tribolodon occur in Japan: big-scaled redfin T. hakonensis, Sakhalin redfin T. sachalinensis, Pacific redfin T. brandtii, and long-jawed redfin T. nakamuraii. Of these species, T. hakonensis is widely distributed in Japan and is important in commercial and recreational fisheries. Two species, T. hakonensis and T. brandtii, exhibit anadromy. In this paper, information on the protistan and metazoan parasites of the four species of Tribolodon in Japan is compiled based on the literature published for 106 years between 1908 and 2013, and the parasites, including 44 named species and those not identified to species level, are listed by higher taxon as follows: Ciliophora (2 named species), Myxozoa (1), Trematoda (18), Monogenea (0), Cestoda (3), Nematoda (9), Acanthocephala (2), Hirudinida (1), Mollusca (1), Branchiura (0), Copepoda (6 ), and Isopoda (1). For each taxon of parasite, the following information is given: its currently recognized scientific name, previous identification used for the parasite occurring in or on Tribolodon spp.; habitat (freshwater, brackish, or marine); site(s) of infection within or on the host; known geographical distribution in Japan; and the published source of each locality record.