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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. -
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. -
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. -
River and Wetland Restoration: Lessons from Japan
Articles River and Wetland Restoration: Lessons from Japan KEIGO NAKAMURA, KLEMENT TOCKNER, AND KUNIHIKO AMANO River and wetland restoration has emerged as a worldwide phenomenon and is becoming a highly profitable business. Although researchers worldwide know a lot about restoration practices in Europe and the United States, we have only scant information about the activities in Japan, where more than 23,000 river restoration projects have been conducted during the past 15 years. In Japan, restoration is a daunting business because of the high human population density, urbanization, and harsh environmental conditions. Here we provide an overview of the various restoration activities in Japan and discuss the lessons that we can draw from them. Keywords: conservation, rehabilitation, biodiversity, floodplain, lake s the 21st century begins, the issue of sustainable article, we present a brief characterization of the country’s en- Aecosystem management is providing humanity with vironmental settings, provide a historic overview of river one of its greatest challenges. The problem is particularly and wetland management in Japan, introduce recent agendas complex for freshwater systems, where humans and natural for restoration, and present three key case studies in more systems are inherently linked. Increasing water demands for detail. Finally, we discuss some general lessons that can be an expanding human population competes with protecting drawn from the various restoration activities in Japan. aquatic ecosystems and ecological services (MEA 2005). To- day, rivers and wetlands are among the most threatened A unique environmental setting ecosystems worldwide (Brinson and Malvarez 2002, Embedded within the circum-Pacific volcanic belt called the Malmqvist and Rundle 2002, Tockner and Stanford 2002). -
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. -
Transport Behavior of Particulate Organic Matter in River Water During Snow Melting in the Ishikari, Tokachi, Teshio and Kushiro Rivers, Japan
J. Asiat. Soc. Bangladesh, Sci. 38(2): 163-173, December 2012 TRANSPORT BEHAVIOR OF PARTICULATE ORGANIC MATTER IN RIVER WATER DURING SNOW MELTING IN THE ISHIKARI, TOKACHI, TESHIO AND KUSHIRO RIVERS, JAPAN M. JAHANGIR ALAM a,b, S. NAGAO a, AND M. EMRAN QUAYUM* a Graduate School of Environmental Earth Science, Hokkaido University, Sapporo, 060-0810, Japan. b School of Geographical Sciences, Southwest University, China. *Department of Chemistry, University of Dhaka, Dhaka-1000, BANGLADESH Abstract Both ∆14C and δ13C were used to study the transport behavior of particulate organic matter (POM) in the Ishikari, Tokachi, Teshio and Kushiro rivers in Japan. Water samples were collected once a month in April and May in 2004 and 2005 during snow melting. Positive correlations were found between ∆14C and particulate organic carbon (POC) content. Negative correlations were found between ∆14C and increased water level. These results indicate that the river systems showed similar transportation behavior during snow melting because of the variation of water level and water discharge. Keywords: Rivers, Carbon Isotopes, POM, Turbidity, AMS, Japan Introduction The annual load of riverine particulate organic carbon (POC) from land to ocean corresponds to half the total organic carbon (Meybeck 1982). Transportation of POC in river systems one pathway of the carbon cycle in terrestrial ecosystems is important for the carbon cycle. Geographical, hydrological and land use features control carbon discharge and transport patterns in rivers (Hope et al. 1994 and Torn et al. 1994). The hydrological situation must be considered in sub-arctic and arctic areas because the watershed environments vary from spring to summer because of snow melt. -
Japanese Experience on Structural Measures for Flood Management
Japanese experience on Structural Measures for Flood Management Kazuhiko FUKAMI Hydrologic Engineering Research Team, Public Works Research Institute (PWRI), Japan Kenji KANAO and Katsuhisa SHIOJI River Bureau, Ministry of Land, Infrastructure and Transport (MLIT), Japan Rivers in Japan are steep. Rivers in Japan tend to be steep, short and rapid flowing. Rhine River Loire River Joganji River Colorado River Abe River Shinano River Tone River Chikugo River Seine River Yoshino River Kitakami River Mekong River Elevation River mouth Distance from river mouth (km) Comparison of the longitudinal profiles of rivers in Japan and other countries -1- Fifty percent of population and 75% of property are concentrated in floodplains accounting for only 10% of total land area. Alluvial plains Other areas (areas lower than river stage in times of flood) Property Population Land area -2- Land use changes in the left-bank area of the Ara River Floodway in the past 100 years 明治188215年 Present現在 Adachi Ward Adachi足立区 Ward Katsushika Katsushika葛飾区 Ward Ward Edogawa Edogawa江戸川区 Ward Ward -3- Major storm and flood disaster after WWII ~ Typhoon Kathleen (September, 1947) ~ Number of persons killed: 1077 Number of persons missing: 853 Number of persons injured: 1,547 Number of houses completely or partially destroyed: 9,298 Above-floor-level/below-floor-level inundation: 384,743 Katsuhika Ward, Tokyo Areas inundated by the September 1947 flood Failure of the levee along the Tone River in the Tone River System (134.5km from river mouth) -4- Changes in the number of persons killed by storms and floods Disaster o Nishi Nihon T I Kano I Disaster o T Nishi NihonHeav Second M Nag Sanin T T M Ky Har Rain Fukushim Rain Disaster Hiroshi Tokai He s s o ah e y y y t y phoon No.