A History of Water Issues
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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. -
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 -
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 -
Cycle Train in Service! Rental Cycle Izu Vélo Shuzenji Station L G *The Required Time Shown Is the Estimated Time for an Electrical Assist Bicycle
Required time: about 4hours and 20minutes (not including sightseeing/rest time) Mishima Station Exploring in Mishima City - Hakone Pass - Numazu Station Atami Station Challenging Cyc Daiba Station course - Jukkoku Pass - Daiba Station Course START o lin Cycle Train in Service! Rental Cycle izu vélo Shuzenji Station l g *The required time shown is the estimated time for an electrical assist bicycle. é Izuhakone Railway 28 minutes Izuhakone Railway v M Izu-Nagaoka Station Cycle Train Service Zone JR Ito Line Izu City will host the cycling competition Mishima-Futsukamachi Station *Can be done in the opposite direction a Japan Cycle at the Olympic and Paralympic Games Tokyo 2020 ↑Ashinoko Lake u Sports Center About 1.3 km ( Track Race and Mountain Bicycle ) Hakone Pass z p Mishima Taisha Shrine i Hakone Ashinoko-guchi ◇Track Race Venue: Izu Velodrome ★ Minami Ito Line Izu City Susono About 2.2 km ★ ly the Heda Shuzenji Station Mountain Bicycle Venue: Izu Mountain Bicycle Course Grand Fields On ◇ p Country Club a i Nishikida Ichirizuka Historic Site z est u St b Nakaizu M u Toi Port Yugashima Gotemba Line nn Kannami Primeval Forest About 13.5 km v ing ♪ g s Izu Kogen Station é The train is National Historic Site: n V l i seat Joren Falls i ews! Hakone Pass o Enjoy the Izu l Mishima-Hagi Juka Mishima Skywalk Yamanaka Castle Ruins c n now departing! Lover’s Cape Ex ★ Izu Peninsula p About 8.7 km y Find the re C s bicycle that a s Children’s Forest Park Izukyu Express w Jukkoku Pass Rest House to the fullest! best for a Kannami Golf Club Tokai -
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 -
Y Azaki Corporation Social & Environmental Report 2015
For inquiries, please contact: Environment Department, Quality Management Division Mishuku 1500, Susono City, Shizuoka 410-1194 Japan TEL: +81-55-965-3782 FAX: +81-55-965-3736 Published: September 2015 The next report is scheduled for publication in autumn 2016. Yazaki Corporation Social & Environmental Report 2015 Yazaki URL: http://www.yazaki-group.com/global/ E-mail: [email protected] コーポレートシンボル Report Outline Contents Editorial policy Business Outline and Scale of Business 3 The Yazaki Group has been publishing its Social & Environmental Report annually since fiscal 2002 for the The Yazaki Group’s Business Segments 5 purpose of sharing information on its corporate activities with stakeholders and encouraging employees to take 余白規定(暫定) part in social and environmental contribution programs. A Message from the President 7 ●印刷物等に使用する場合 ●サイン・ステッカー等に使用する場合(新規作成の場合は W:H=5:1) 500 The report covers our activities during the past 12 months 1/2H以上 1/2H以上 2 0( c) 450 30(d) 1/2H以上 25(a) and their results, centered primarily on the five 100 H 62.5 Yazaki Group Corporate12.5(b) Policy 1/2H以上 stakeholders, namely: customers, business partners, local 限定されたプロポーションへの表示基準は、左図の各スペース(a~d)を 最小スペースとし、 1: 2.75 ~1: 5の場合は、左右幅を基準とする。 a : b = 2 : 1 c : d = 1 : 1.5 communities, employees, and the global environment. Special Feature A Corporation in Step with the World Additionally, environmental reports have also been Toward Coexistence with Nature published by each factory in Japan since fiscal 2005. These Local recycling of forest 9 site reports are available on our website. resources with Yusuhara Town, Kochi A Corporation Needed by Society Please visit our website While this report provides an outline of activities of the Yazaki Group, our website presents more detailed information and data. -
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. -
Final 94254-Wasje.Xps
World Applied Sciences Journal 33 (7): 1079-1088, 2015 ISSN 1818-4952 © IDOSI Publications, 2015 DOI: 10.5829/idosi.wasj.2015.33.07.94254 Genetic Population Structure of the Aburahaya (Rhynchocypris lagowskii) Based on Mitochondrial DNA Sequence C.M.M. Hassan, Takanori Ishikawa, Singo SEKI and A. Mahmuda Laboratory of Aquatic Ecology, Faculty of Agriculture, Kochi University, B-200 Nankoku, Kochi 783-8502, Japan Abstract: Analyses of partial mitochondrial DNA (mtDNA) sequences support the classification of Aburahaya (Rhynchocypris lagowskii) from the Sea of Japan and Pacific Ocean. To investigate genetic population structure, we examine nucleotide sequence of the cytochrome b region. In this study we found three major geographical groups. Molecular phylogenetic analysis revealed that the population of the group 3 differentiation is 0.8759 ± 0.0333. The group 2 differentiation is 0.5333 ± 0.1801 which is collected from the Kamishyou River (Toyama Prefecture) and Hakui River (Ishikawa Prefecture) populations. The neighbor-joining tree of the mitochondrial DNA haplotypes for all specimens constructed from the Kimura’s two parameter. Among these 24 localities being clustered into 3 major geographic groups in NJ tree mtDNA segment and NJ tree mtDNA haplotype. No significant difference for the population pair wise FST was detected among these localities (P>0.05). The most parsimonious network of mtDNA haplotype of aburahaya 24 localities, estimated using the TCS algorithm. In this network showed three geographical groups. Halpotype 1-29 is one group, haplotype 30-33 is group 2 and haplotype 34-54 is group 3. Key words: Population genetic mtDNA Cyprinide Aburahaya Geographic groups Haplotype network INTRODUCTION entire range have been fragmentary. -
Development and Management of River Flood Controls
Proceedings of the 22nd IAHR-APD Congress 2020, Sapporo, Japan DEVELOPMENT AND MANAGEMENT OF RIVER FLOOD CONTROLS AND WATER UTILIZATION FACILITIES IN THE MIDDLE AND LOWER REACHES OF THE ISHIKARI RIVER OVER 100 YEARS - TRANSFORMATION OF COLD REGION PEATLANDS INTO ONE OF JAPAN’S TOP RICE CULTIVATION AREAS, LEADING TO THE FORMATION OF A MAJOR ECONOMIC ZONE - HIDETO KON Hokkaido University, Faculty of Engineering, Sapporo, Japan, [email protected] TAKASHI INOUE Hokkaido University, Research Faculty of Agriculture, Hokkaido University, Sapporo, Japan, [email protected] YASUYUKI HIRAI Civil Engineering Research Institute for Cold Region, Sapporo, Japan, [email protected] KAZUMASA NAKAMURA Civil Engineering Research Institute for Cold Region, Sapporo, Japan, [email protected] SATOMI KAWAMURA Civil Engineering Research Institute for Cold Region, Sapporo, Japan, [email protected] ABSTRACT In Hokkaido, a cold region in northern Japan, full-scale land reclamation started when the local headquarters of the Hokkaido Development Commission was established in Sapporo in 1871. The center of land reclamation in Hokkaido was the Ishikari River Basin, the second largest river in Japan, where the city of Sapporo is now located. In particular, the middle and lower reaches of the Ishikari River basin downstream from Kamuikotan was a primeval swamp and peatland at that time, which hindered its reclamation. However, the development and appropriate management of river flood control and water utilization facilities in the middle and lower reaches resulted in changes. The peatland in this cold region were transformed into one of Japan’s leading rice cultivation areas. The transformation of this region into a major economic zone was realized in a relatively short period of one hundred-odd years.