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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 -
The Geobiology and Ecology of Metasequoia
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/37160841 The Geobiology and Ecology of Metasequoia. Article · January 2005 Source: OAI CITATIONS READS 11 457 3 authors: Ben LePage Christopher J. Williams Pacific Gas and Electric Company Franklin and Marshall College 107 PUBLICATIONS 1,864 CITATIONS 55 PUBLICATIONS 1,463 CITATIONS SEE PROFILE SEE PROFILE Hong Yang Massey University 54 PUBLICATIONS 992 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Conifer (Pinaceae and Cupressaceae (Taxodiaceae)) systematics and phylogeny View project All content following this page was uploaded by Ben LePage on 24 September 2014. The user has requested enhancement of the downloaded file. Chapter 1 The Evolution and Biogeographic History of Metasequoia BEN A. LePAGE1, HONG YANG2 and MIDORI MATSUMOTO3 1URS Corporation, 335 Commerce Drive, Suite 300, Fort Washington, Pennsylvania, 19034, USA; 2Department of Science and Technology, Bryant University, 1150 Douglas Pike, Smithfield, Rhode Island, 02917, USA; 3Department of Earth Sciences, Chiba University, Yayoi-cho 133, Inage-ku, Chiba 263, Japan. 1. Introduction .............................................................. 4 2. Taxonomy ............................................................... 6 3. Morphological Stasis and Genetic Variation ................................. 8 4. Distribution of Metasequoia Glyptostroboides ............................... 10 5. Phytogeography ......................................................... -
PHYLOGENY and ZOOGEOGRAPHY of the SUPERFAMILY COBITOIDEA (CYPRINOIDEI, Title CYPRINIFORMES)
PHYLOGENY AND ZOOGEOGRAPHY OF THE SUPERFAMILY COBITOIDEA (CYPRINOIDEI, Title CYPRINIFORMES) Author(s) SAWADA, Yukio Citation MEMOIRS OF THE FACULTY OF FISHERIES HOKKAIDO UNIVERSITY, 28(2), 65-223 Issue Date 1982-03 Doc URL http://hdl.handle.net/2115/21871 Type bulletin (article) File Information 28(2)_P65-223.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP PHYLOGENY AND ZOOGEOGRAPHY OF THE SUPERFAMILY COBITOIDEA (CYPRINOIDEI, CYPRINIFORMES) By Yukio SAWADA Laboratory of Marine Zoology, Faculty of Fisheries, Bokkaido University Contents page I. Introduction .......................................................... 65 II. Materials and Methods ............... • • . • . • . • • . • . 67 m. Acknowledgements...................................................... 70 IV. Methodology ....................................•....•.........•••.... 71 1. Systematic methodology . • • . • • . • • • . 71 1) The determinlttion of polarity in the morphocline . • . 72 2) The elimination of convergence and parallelism from phylogeny ........ 76 2. Zoogeographical methodology . 76 V. Comparative Osteology and Discussion 1. Cranium.............................................................. 78 2. Mandibular arch ...................................................... 101 3. Hyoid arch .......................................................... 108 4. Branchial apparatus ...................................•..••......••.. 113 5. Suspensorium.......................................................... 120 6. Pectoral -
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. -
5Th Proceedings
th TThhee 55 IInntteerrnnaattiioonnaall SSyymmppoossiiuumm on Water Environment Systems on Water Environment Systems ------wwiitthh PPeerrssppeeccttiivvee ooff GGlloobbaall SSaaffeettyy th nd (( NNoovveemmbbeerr 3300 -- DDeecceemmbbeerr 22 ,, 22001177)) Department of Civil and Environmental Engineering Graduate School of Engineering Tohoku University Sponsors http://www.g-safety.tohoku.ac.jp/ Tohoku University, Main Administration Office Organization for Leading Graduate School Program of Tohoku University, Sendai, Miyagi 980-8578, Japan http://www.eng.tohoku.ac.jp/ Tohoku University, Graduate School of Engineering, Sendai, Miyagi 980-8579, Japan ORGANIZERS Dr. KAZAMA So (Professor, Tohoku University) Dr. LI Yu-You (Professor, Tohoku University) Dr. KOMORI Daisuke (Associate Professor, Tohoku University) SECRETARIES Assistant Professor, Toshimasa Hojo [email protected] Assistant Professor, Yoshiya Touge [email protected] DC Student, Jialing Ni [email protected] DC Student, Bo Jiang [email protected] M Student, Kaoruko Kimura [email protected] PARTICIPANTS Tohoku university Japan Name Identity Prem Rangsiwanichpong Student Noriko Uchida Student Chang Qing Student Miku Sakurai Student Danila Aleksandrovich Podobed Student Grace Puyang Emang Student Mbugua Jacqueline Muthoni Student Silva Vasquez Leonardo Alonso Student Kentaro Sugii Student Hironobu Hirayama Student Masafumi Kon Student Satoshi Anzai Student Koji Iwama Student Tao Zhang Student Jing Wu Student Jialing Ni Student -
ⅶ Session Reports
Ⅶ SESSION REPORTS Ⅶ-1 Japan Mr. Shin TSUBOKA Director General, National Institute for Land and Infrastructure Management Adaptation to Flood Change Due to Warming in Japan National Institute for Land and Infrastructure Management Director General : Shin Tsuboka Geographic Features and City Formation Most of the plains in Japan are alluvial plains and many cities are formed over these alluvial plains. Alluvial plain Alluvial plain Tokyo area Chukyo area (The Kanto Plain) (The Noubi plain) 1 2-1 Flood Vulnerability Tokyo and Edo river, Ara river and Sumida river Elevation Keihin- Tohoku Musashino line Line Ayase Shin Route 6 Sumida river saka Naka river Oba Edo Saka river riverJoban Ara river river river river Line Kita Adachi Katsushika Misato Matsudo Ward Arakawa Ward Ward City City Ward London and the Thames The Thames Information provided by MLIT The relation of grounds and rivers level in Tokyo and London 2 Flood damages Flood damage density of (100 billion Yen) ordinary assets Damage to ordinary assets (10 thousand yen/ha) Flooded area (10 thousand ha) Flood damage area Flood damage density of ordinary assets such as housing areas (The ratio of assets to an affected area) Ordinary asset damage 1978 1979 1980 1981 1982 1983 1984 1985 1986 1987 1988 1989 1990 1991 1992 1993 1994 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 Year Transition of Ordinary asset damages and flooded area 3 2-2 Precipitation change (1) Number of downpour occurrences with 50mm rainfall per hour or larger Total number of occurrences per year (Based -
Northern Jomon Culture Seen from the World 1/8
Northern Jomon culture seen from the world 1/8 Northern Jomon culture seen from the world Kazunori Takada (Director, Goshono Jomon Park ) J omon culture is a prehistoric culture that lasted for more than 10,000 years on the Japanese archipelago. The range of the culture is thought to have extended throughout almost all of the archipelago, from northern Hokkaido to southern Kagoshima, and then further, into Okinawa. However, the culture was not necessarily uniform, and distinctive regional characteristics have encouraged moves to understand Jomon as a regional cultural sphere. Among these regions, a unique cultural area was formed by the southern part of Hokkaido and the northern part of Tokhoku, the north-eastern part of Japan, which are separated by the Tsugaru Strait. Currently, efforts are underway to secure UNESCO World Heritage Site designation for the Jomon culture of this region, as “Jomon Archaeological Sites in Hokkaido and Northern Tohoku.” The Goshono Jomon Park continues to hold lectures to encourage learning about Jomon culture in the north, and many researchers into archaeology, history, and cultural anthropology have given interesting lectures. This article contains one of those lectures, on how Jomon is seen from outside the Japanese archipelago. I would like to remove the frame of the Japanese archipelago, and to think with everyone, from a broader perspective, about the strong regional ties and longevity of the culture of “Jomon Archaeological Sites in Hokkaido and Northern Tohoku.” Northern Jomon culture seen from the world 2/8 The beginning of pottery and changes in the natural environment F ifteen thousand years ago, rapid warming reduced the number of large animals, and pottery began to appear for the first time, from Primorsky Krai in East Asia (Russian Far East) to various part of China and the Japanese archipelago. -
FY2016 Results of the Radioactive Material Monitoring in the Water Environment
FY2016 Results of the Radioactive Material Monitoring in the Water Environment March 2018 Ministry of the Environment Contents Outline .......................................................................................................................................................... 1 Part 1: National Radioactive Material Monitoring in the Water Environment in the Whole of Japan (FY2016) ...................................................................................................................................................................... 5 1 Objective and Details ............................................................................................................................. 5 1.1 Objective .................................................................................................................................... 5 1.2 Details ........................................................................................................................................ 5 2 Survey Methods and Analysis Methods .............................................................................................. 18 2.1 Survey methods ....................................................................................................................... 18 2.2 Analysis methods ..................................................................................................................... 19 3 Results ................................................................................................................................................ -
Mt. Nanakura ■ a Seven-Mountain Range Where Native Akita Trek Altitude: 269.6 M ■ Cedar Trees Are Grown, Rare in Modern Times
▲ ■ Location: Noshiro City ■ Trek Length: 9.0 km 8 Mt. Nanakura ■ A seven-mountain range where native Akita Trek Altitude: 269.6 m ■ Cedar trees are grown, rare in modern times. Topographical Map (1/25,000): Height: 287.6 m Western part of Takanosu grade Physical 2 Skill B Strength level 2 1 Enjoying the scenic beauty of Shirakami Mountain from the Minokura Observation Spot 2 A deformed rock called Hokkenoiwa Boulder 1 Late April, I embarked from the former site of Tenjin Lodge, where some nationally- known celebrities, including a famous singer, Misora Hibari, had once stayed overnight. Proceeding clockwise, I encountered an array of spring flowers growing along the trail, including anemone pseudoaltaica H. hara, violets, Stee Matsukura Roadside and soft windflowers - I felt as if I had been dnhills Trek Starting Point Statin nearby ● 20m Futatsi swept into a picture book. 7 It seems that the abundance of remaining cedar ▲Matskura trees is due to the then feudal lord, the Satake 159.3 clan, prohibiting them from timbering them in order to preserve their position along the ▲⬅ Okra 60 Yoneshiro River. min Kotsunagi ▲ I touched the Shishiatama, a stone statue of a Yoneshir Sanbonsgikura 3 iver lion head that was once drawn by famous travel min Viewing 30 writer Sugae Masumi, who was hoping that it Shirakai ⬅ Nanakra Mountains Shibakra▲ Shrine Nanakura would help prevent a brain stroke. I then went to Nibuna Bridge to Hokkenoiwa Cave, which was similar to a big Tenin rek inokura ●▲ starting point bee hive. In the past, some Buddhist monks were chsan Observation Spot ● ● 18m to Aikawa, ?巻末の 一覧表では Shrine JunctinJunction WC P Kamikoani believed to carry out their religious training ゴール地点が松倉 登 山 口 、タ イ ム の San Shrine here. -
Dam/Barrage Year /Anne E River /Riviere City/Ville St/Et/ Pr/Dpt Type
Year Found Hight Vol Area Length Catc SpillCap/ River St/Et/ Type Leng Purp Type Sp Dam/barrage /Anne City/Ville /Fondatio /Haut /Vol Capacit. /Sur /Long /Bvers. E Owner/Proprie Engine/Bur.d'et Contractor/Entr /Riviere Pr/Dpt /Type /Long m /Buts /Typ Eva e n en m 103m3 103m2 km Km2 m3/s ICHIBANIKE 400 Ishite Matsuyama Ehime TE R 15 180 50 140 I 0 N Higashino Irrigation Assoc. Kagoshim Mitsumata Land SUMIYOSHIIKE 400 Beppu Gamo a TE R 20 60 14 230 I 0 N Improvement Assoc. KAERUMATAIKE 607 Yodo Nara Nara TE R 17 260 159 485 I 0 N Nara City SAYAMAIKE 616 Yamato Tondabayashi Osaka TE R 19 997 605 2800 I 18 0 N Osaka Prefecture (Obayashi-Gumi Co.) FUROTANIIKE 900 Kino Hashimoto Wakayam TE R 18 100 26 100 I 0 N Furotaniike Irrigation Wakayam Kumamichiike Irrigation KUMAMICHIIKE 900 Kino Hashimoto a TE R 18 32 5 9 I 0 N Assoc. MINENOIKE 900 Kino Hashimoto Wakayam TE R 16 45 7 15 I 0 N Minenoike Irrigation Assoc. Shido Land Improvement NAGAYUKIIKE 1000 Ohashi Takamatsu Kagawa TE R 20 171 87 483 I 0 N Assoc. Tatsuno Land DAIMONIKE 1128 Daimon Nara Nara TE X 20 78 105 98 10 I 0 N Improvement Assoc. SHINTARO 1260 Hido Ueno Mie TE 19 150 73 35 I Private Dam MARUYAMA(YAMAGU Yamaguch Maruyama Users'. CHI) 1346 Ara Ube i TE R 18 46 24 120 I 0 N Ube City Group OIKE 1360 Kino Hashimoto Wakayam TE R 18 80 30 200 I 0 N Oike Irrigation Assoc. -
National Radioactive Material Monitoring in the Water Environment in the Whole of Japan(2016) List of Results(Final Report)
National Radioactive Material Monitoring in the Water Environment in the Whole of Japan(2016) List of Results(Final Report) Results of Measurement in Public Water Areas(Water) ························· 1 Results of Measurement in Public Water Areas(Sediment) ······················ 7 Results of Measurement in Public Water Areas(Surrounding Environment) ······ 20 Results of Measurement of Groundwater(Water) ····························· 35 Results of Measurement in Public Water Areas(Water) 1 Results of Measurement in Public Water Areas(Water) Sampling location General items Water Water Sampling Secchi disk depth Electrical Detected γ-ray emitting radionuclides Total β radioactivity No. Prefecture Property Sampling Date Weather depth Transparency SS Turbidity Remarks Water area Location Municipality depth (Lake) conductivity (m) (cm) (mg/L) (FNU) Measured value Detection limits Measured value Detection limits (m) (m) (mS/m) Radionuclides (Bq/L) (Bq/L) (Bq/L) (Bq/L) Water purification plant intake at Ishikari River 1 Asahikawa City 2016/11/7 Sunny 2.0 0.1 >100 - 8.7 5 1 K-40 0.065 0.033 0.037 0.026 in Asahikawa City Ishikari River Intake at the Shirakawa water purification plant Be-7 0.017 0.0080 2 Sapporo City 2016/10/11 Cloudy 1.7 0.1 >100 - 16.3 3 3 0.075 0.026 in Sapporo City K-40 0.062 0.023 Nakashibetsu Bridge Be-7 0.027 0.0083 3 Teshio River (Intake at the Higashiyama water purification Shibetsu City 2016/10/12 Cloudy 0.8 0.1 88 - 8.4 4 6 0.067 0.024 plant in Shibetsu City) K-40 0.041 0.028 4 Tokoro River Tadashi Bridge Kitami City -
Concentrations of 21 Collected from and 3 M Etalsin
Geochem icalJournal,Vol.14,pp.203to 226,1980 203 C oncentrations of 21 m etals in the suspended solids collected from the principal 166 rivers and 3 lakes in Japan HISAYU KI T E RA OK A an d JUN K OBAYASHI Institute for A gricultural and Biological Sciences, O kayam a U niversity, K urashiki 710, Japan (R eceived July 21, 1980, A ccepted October 20, 1980) In the analysis ofnatural water,it w ould beinteresting to determine sm allbut significant quantities of trace m etals which are concentrated in suspended solids, since som e of these m etals, derived from geologic formations, mines and industries not only influence the environment for men and anim als,but will also help us in tracing m etallic resources. Taking advantage of the nation-wide chemicalinvestigations conducted by JUN K OBAYASHI, FUJI M ORII and cow orkers on various constituents dissolved in the principal Japanese rivers and lak es, the present authorscould analyze major an d minor metallic elementsin the suspended solids by theemission spectrographic m ethod. The following are the results obtained: (1) M arkedly high er concentrations of minor elements such as Pb, Zn, Cu, Ni, M n and Co were found in the suspended solids th an in unpoluted soils or in the continentalcrustreported by TAYLOR (1964). (2) TheconcentrationsofM n,Cu,Ni,Pb and Sn were foundto bem arkedly highinthe North eastern provinces. Thism ustbedueto the higherconcentrationsofthesem etalsdistributedin geologicform ations in this section as well as to the influence of m any copper and other mines. (3) The distribution of Be happened to divide Japan into tw o halves.