White-Spotted Charr, Salvelinus Leucomaenis Imbrius and S. L. Pluvius, on the Basis of RAPD Analysis
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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 -
5 International Conference on Flood
Abstract Proceedings 5th International Conference on Flood Management (ICFM5) - Floods: from Risk to Opportunity - 27 to 29 September 2011 Tokyo-Japan Organized by: ICFM5 Secretariat at International Centre for Water Hazard Risk Management (ICHARM) under the auspices of UNESCO Public Works Research Institute (PWRI) 5th International Conference on Flood Management (ICFM5) 27-29 September 2011, Tokyo-Japan Ad-hoc Committee Slobodan Simonovic (ad-hoc commitee chair), ICLR, Canada Jos van Alphen, Rijkswaterstaat, Netherlands Paul Bourget, IWR-USACE, USA Ali Chavoshian, PWRI/ICHARM, Japan Xiaotao Cheng, IWHR, China Erich Plate, Karlsruhe University, Germany Kuniyoshi Takeuchi, ICHARM, Japan ICFM5 Local Organizing Committee Kuniyoshi Takeuchi (ICFM5 co-chair), PWRI/ICHARM Koji Ikeuchi (ICFM5 co-chair), MLIT Kazuhiro Nishikawa, NILIM Norio Okada, DPRI, Kyoto University Yuji Okazaki, JICA Kotaro Takemura, JWF Kiyofumi Yoshino, IDI Kenzo Hiroki, PWRI/ICHARM Minoru Kamoto, PWRI/ICHARM Ali Chavoshian (ICFM5 Secretary), PWRI/ICHARM ICFM5 International Scientific & Organizing Committee Giuseppe Arduino, UNESCO- Jakarta Office Mustafa Altinakar, IAHR, University of Mississippi Arthur Askew, IAHS Mukand Babel, AIT, Thailand Liang-Chun Chen, NCDR, Taiwan Ian Cluckie, IAHS-ICRS/Swansea University, UK Johannes Cullmann, IHP /HWRP, Germany Siegfried Demuth, UNESCO-IHP Koichi Fujita, NILIM, Japan Shoji Fukuoka, Chuo University, Japan Srikantha Herath, UNU Pierre Hubert, IAHS Toshio Koike, GEOSS/ University of Tokyo, Japan Shangfu Kuang, IWHR/IRTCES, China Zbigniew Kundzewicz, RCAFE, Poland Soontak Lee, UNESCO-IHP/ Yeungnam Uni., Korea Kungang Li, MWR, China Arthur Mynett, IAHR Katumi Musiake, Hosei University, Japan Hajime Nakagawa, JSCE/Kyoto University, Japan Taikan Oki, University of Tokyo, Japan Katsumi Seki, MLIT, Japan Michiharu Shiiba, JSHWR/Kyoto Unuversity, Japan Soroosh Sorooshian, CHRS, U.C. -
Place Names and the Rediscovery of Former
PLACE NAMES AND THE REDISCOVERY OF FORMER LANDSCAPES IN IZUMO CITY AND HIKAWA TOWN, JAPAN By MIDORI YAMAMOTO B.A., Ritsumeikan University, 1981 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS in THE FACULTY OF GRADUATE STUDIES (Department of Geography) We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA September 1 992 © Midori Yamamoto __-- In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the head of my department or by his or her representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Department of Geography The University of British Columbia Vancouver, Canada Date 7-3 I DE.6 (2/88) ABSTRACT Place names in Japan are closely connected to the land where they were named. Differences between Japan and the West regarding the concept of “what is named” are introduced, and universal characteristics of place names are reviewed. Some of the unique and complex characteristics of Japanese place names are also examined. In Japan, especially since early in the Meiji Period (1 808-1 912), many traditional place names have been lost, mainly due to attempts to reduce and simplify names through local government reform. In this thesis, an analysis is made of place names collected from land registration maps issued in 1889 in Izurno City and Hikawa Town, Shimane Prefecture, Japan. -
Japan-Birding "Birding Spots"
Top-page Inquiry Trip reports Check list News Links Birdwatching Spots Hokkaido Regeon Tohoku Regeon Kou-Shin-Etsu Regeon Northern-Kanto Regeon Southern-Kanto Regeon Tokyo Regeon Izu Islands Ogasawara Islands Izu-Hakone- Fuji Regeon Tokai Regeon Hokuriku Regeon Kansai Regeon Chugoku Regeon Shikoku Regeon Kyushu Regeon Okinawa Regeon Cruise - Over 400 popular birding sites in all over Japan are listed in this page. - The environment, the time required for birding (the traveling time to the site is not included), the birds expected and the visit proper season of each site are briefly described. - You can also check the location of the site in Googl Map. Please click Google-Map in the descriptions. On the Google Map, search the site with the number (i.e,: D6-1 for Watarase Retarding Basin). - The details of the sites can be checked on the linked websites (including Japanese sites). A) Hokkaido Regeon Google-Map West-Northern Part of Hokkaido A1-1 Sarobetsu Plain (Sarobetsu Gen-ya) - Magnificent wetland extending at the mouth of Sarobetsu River, a part of the northernmost national park in Japan - 1-2 days - summer birdss - Best season: May to Sep. A1-2 Kabutonuma Park (Kabutonuma-Koen) - Forest and lake, a part of the northernmost national park in Japan. - 0.5 day - summer birds - Best season: May to Sep. A2-1 Teuri Island (Teuri-Tou) - National Natural Treasure in Japan, the breeding ground for around a million sea-birds; Common Murre, Spectacled Guillemot, Rhinoceros Auklet and Black-tailed Gull . - 1-2 days (*depending on the ship schedule) - the breeding sea-birds or the migrating birds in springa and autumn - Best season: Apr. -
Exhibitor Company Profiles
Poster Program All posters will be displayed for the duration of the conference, with discussion and questions taking place according to the schedule below: Poster Session 1 - Themes A: Environment & B: Biodiversity Monday 3 September, 17:15-18:15 & Tuesday 4 September, 13:10-14:00 Poster Session 2 - Themes C: People & D: Integration Wednesday 5 September, 12:40-13:00 & Thursday 6 September, 13:10-14:00 [P.A.001] Regularities of the bottom sediments suspension in the frequency domain R.D. Kosyan*, B.V. Divinskii, Shirshov Institute of Oceanology, Russia [P.A.002] Contribution of wind wave components to the climatic alongshore sediment flux (on the example of the Anapa bay-bar, Black Sea) B.V. Divinskii*, R.D. Kosyan, Shirshov Institute of Oceanology, Russia [P.A.003] The seasonal morphological evolution pattern of the mouth bar in Modaomen estuary of the Pearl River G.L. Huang*1,2, C. Tan1,2, B.S. Huang1,2, J. Qiu1,2, J.L. Huang1,2, 1Guangdong Research Institute of Water Resources and Hydropower, China, 2Guangdong Key Laboratory of Hydrodynamic Research, China [P.A.004] Spatio-temporal variability of phytoplankton biomass in relation to salinity in the southeast area of Setiu lagoon during high and low river flow conditions Z. Zainol*, M.F. Akhir, A. Johari, R. Latif, Universiti Malaysia Terengganu, Malaysia [P.A.005] Prevalence of microplastics in east coast of Peninsular Malaysia’s coastal marine environment S.A. Zainal*, M.F. Akhir, Universiti Malaysia Terengganu, Malaysia [P.A.006] Monthly variations in the intracellular nutrient pools of phytoplankton in Jaran Bay, Korea S.H. -
Izumo (No Kuni) Fudoki
Japanese Journal of Religious Studies 37/2: 185–222 © 2010 Nanzan Institute for Religion and Culture Anders Carlqvist The Land-Pulling Myth and Some Aspects of Historic Reality Izumo fudoki describes Izumo Province, situated in today’s Shimane Prefec- ture and facing the Japan Sea. It is the oldest surviving Japanese text compiled by aristocrats from a region, hence giving us unique information about a Japa- nese province during the Nara period. However, Izumo fudoki has been little consulted by Western scholars. The land-pulling myth is the first myth to be related in Izumo fudoki; it narrates how one of the local deities looks across the Japan Sea and decides to pull land from four of the places that he can see, including from the Korean Peninsula. This land he cuts off, pulls across the sea, and attaches to Izumo, hence making the province larger. This article dis- cusses two ways of interpreting the myth. One possible interpretation is that the four places from which land is being pulled correspond to an area that was in different ways connected to Izumo during the late Yayoi period. The other, perhaps more worthwhile, explanation of the myth is to see how it sup- ported the local aristocracy in Izumo Province as it tried to maintain partial autonomy vis-à-vis the central government. keywords: Izumo fudoki—Izumo Province—Izumo no Omi—myths—deities— burial mounds—kofun—Yayoi period—Nara period Anders Carlqvist teaches at Morioka Junior College in Iwate Prefectural University. 185 he eighth-century text Izumo (no kuni) fudoki 出雲国風土記 (733) narrates several intriguing myths, most of them not mentioned in the official records,Kojiki 古事記 (712) and Nihon shoki 日本書紀 (720), com- Tpiled by the central government.1 The myths not only differ from the ones of the central tradition; some of them even outright oppose the hegemony of the court. -
Composition of Subspecies, Head Spot Types and Genetic Types of Charr Distributed in the Hino River, Japan
View metadata, citation and生物圏科学 similar papers at core.ac.uk brought to you by CORE Biosphere Sci. provided by Hiroshima University Institutional Repository 51:1-8 (2012) Composition of subspecies, head spot types and genetic types of charr distributed in the Hino River, Japan Koichiro KAWAI, Hidetoshi SAITO and Hiromichi IMABAYASHI Graduate School of Biosphere Science, Hiroshima University, Kagamiyama 1-4-4, Higashi-hiroshima, Hiroshima 739-8528, Japan Abstract Composition of 2 subspecies of white-spotted charr, Salvelinus leucomaenis imbrius (“Gogi”) and S. l. pluvius (“Nikko-iwana”), head spot types and genetic types were investigated for the Hino River, Tottori Prefecture, Japan. A total of 38 charr samples was collected from the 19 branches. All the branches were categorized into 8 groups based on the mountain mass from which the branch originates. Nikko-iwana was distributed in the Daisen, Futago and Hanami mountain masses in the eastern part of the basin and was not distributed in the other 5 mountain masses in the western part. In contrast, Gogi was distributed in the western Onibayashi, Dogo, Mikuni, Senzu and Takairi mountain masses and was not distributed in the 3 eastern mountain masses. For head spot types, C, E, F , G and H were distributed in the 3 eastern masses whereas A, B and D were not recorded from these masses. On the other hand, all the types were distributed in the 5 western masses. For genetic types, 6 and 9 haplotypes were Nikko-iwana- and Gogi-specific, respectively. Only a haplotype comprised both subspecies. In the dendrogram, 5 haplotypes constructed an exclusive clade of Nikko-iwana whereas 6 haplotypes constructed an exclusive clade of Gogi. -
霞ヶ浦ake Kasumigaura
3 The present conditions and eutrophication measures in lakes in Japan There are many designated lakes as well as other lakes in this country, but the closed nature (retention time), water depth, water temperature and catchment area load vary. Therefore, the eutrophication characteristics in lakes also vary as do opinions on the measures for tackling the problem. In this chapter, based on these points mentioned above, the present conditions of eutrophication in lakes in this country are described. For each lake, (1) the characteristics of catchment areas, (2) the water quality in lakes, the characteristics of biota, (3) the problems of the present situation and prospects for measures are described. 3-1 Lake Kasumigaura 3-1-1 Characteristics of the catchment area/lake Lake Kasumigaura is an inland sea-lake belonging to the Tonegawa River system that flows through the Kanto Plain, and the lake is situated on the left bank of the lower reaches of the Tonegawa River, a low-lying area in the southeast part of Ibaraki prefecture. The water area is about 220 km2, so it has the second largest area after Lake Biwa in this country. Moreover, the pondage is about 850 million m3, which is larger than the total pondage of the multipurpose dam that was constructed in the upper reaches of the Tonegawa River. About six thousand years ago, Lake Kasumigaura was part of the inlet connected to the present upper reaches of the Tonegawa River, Lake Inba and Lake Tega. Over the centuries, the mouth of the river became blocked by earth and sand that was carried from the upper reaches, and it is said that the lake more or less assumed its present shape about 1,500-2,000 years ago, becoming a freshwater lake around 1638 during the Edo period. -
Arao-Higata 鳥栖 I.C 日田 I.C 湯布院 I.C 佐賀大和 I.C 久留米 I.C 別府 I.C the Guide Book to Arao-Higata, Ramsar Site
門司 I.C 九 州 Ramsar Site 自 動 車 道 Fukuoka Airport Hakata St. 太宰府 I.C Arao-higata 鳥栖 I.C 日田 I.C 湯布院 I.C 佐賀大和 I.C 久留米 I.C 別府 I.C The Guide Book to Arao-higata, Ramsar Site 佐世保 I.C 武雄 I.C 八女 I.C 新大牟田駅 Saga Airport Nankan I.C 津久見 I.C Arao St. Kikusui I.C 新玉名駅 諫早 I.C KUMAMOTO 長崎 I.C 有明フェリー 熊本 I.C Kumamoto St. Aso-Kumamoto Airport 島原 新八代駅 Arao City, 鹿 八代 I.C 児 Kumamoto Pref. 島 本 線 芦北 I.C えびの I.C 九 州 新 宮崎 I.C 幹 都城 I.C 線 鹿児島中央駅 鹿児島 I.C Protect and nurture our rich treasure sea and the life of Arao-higata for the future 頴娃 I.C It’s a great expanse of tidal flat in the Sea of Ariake Tasty clams and laver are harvested from this tidal flat Migratory birds, shellfish, lugworms, a diversity of life Living side by side with the fertile tidal flat are the people who nurture the life in the tidal flat, who enjoy mud shrimp fishing during summer The Ramsar site, Arao-higata is our asset recognized by the World indeed Published by Kyushu Regional Environmental Offce, Ministry of the Environment, Japan. Outline of Arao-higata Arao-higata—a tidal fat that represents the Sea of Ariake The Sea of Ariake located in Kumamoto Prefecture, Japan, accounts for around 40% of the total tidal fat area of Japan. The ex- tensive tidal fats in the Sea of Ariake were formed by large volumes of sediment carried by Japan’s largest tidal fow and a vertical tid- al range of 6 meters. -
Regional Overview
NOWPAP POMRAC Northwest Pacific Action Plan Pollution Monitoring Regional Activity Centre 7 Radio St., Vladivostok 690041, Russian Federation Tel.: 7-4232-313071, Fax: 7-4232-312833 Website: http://www.pomrac.dvo.ru http://pomrac.nowpap.org REGIONAL OVERVIEW on River and Direct Inputs of Contaminants into the Marine and Coastal Environment in NOWPAP Region POMRAC, Vladivostok, Russian Federation 2006 POMRAC Technical Report No. 4 Foreword The Global Programme of Action (GPA) for the Protection of the Marine Environment from Land- based Activities was adopted in 1995 and since then significant results have been achieved. Because about 80% of pollutants entering the marine environment originate from land-based activities, the GPA implementation is supported by more than 100 Governments, the European Commission and many international and non-governmental organizations. The comprehensive, multi-sectoral approach of the GPA reflects the desire of Governments to strengthen the collaboration and coordination of all agencies with mandates relevant to the impact of land-based activities on the marine environment, through their participation in a global programme. The Second Intergovernmental Review Meeting (16-20 October 2006, Beijing, People’s Republic of China) will consider the status of GPA implementation and future actions. Several pollutant categories are covered by the GPA including sewage, persistent organic pollutants, heavy metals, oils (hydrocarbons) and nutrients. This Overview on River and Direct Inputs of Contaminants to the Marine and Coastal Environment of the Northwest Pacific has been prepared by the Pollution Monitoring Regional Activity Center (POMRAC) of NOWPAP. The Overview can be considered as a NOWPAP contribution to the GPA implementation in the Northwest Pacific region. -
Modeling Suspended Sediment Sources and Transport in the Ishikari River Basin, Japan, Using SPARROW
Hydrol. Earth Syst. Sci., 19, 1293–1306, 2015 www.hydrol-earth-syst-sci.net/19/1293/2015/ doi:10.5194/hess-19-1293-2015 © Author(s) 2015. CC Attribution 3.0 License. Modeling suspended sediment sources and transport in the Ishikari River basin, Japan, using SPARROW W. L. Duan1,2, B. He1, K. Takara2, P. P. Luo3,4, D. Nover5, and M. C. Hu2 1Key Laboratory of Watershed Geographic Sciences, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, 210008, China 2Disaster Prevention Research Institute, Kyoto University, Kyoto, Japan 3Institute of Hydraulic Structure Engineering and Water Environment, College of Civil Engineering and Architecture, Zhejiang University, Hangzhou, Zhejiang, China 4Institute for the Advanced Study of Sustainability, United Nations University, Shibuya, Tokyo, Japan 5AAAS Science and Technology Policy Fellow, US Environmental Protection Agency, Global Change Research Group, Washington, D.C., 20010, USA Correspondence to: W. L. Duan ([email protected]), B. He ([email protected]), and P. P. Luo ([email protected]) Received: 13 September 2014 – Published in Hydrol. Earth Syst. Sci. Discuss.: 6 October 2014 Revised: – – Accepted: 15 February 2015 – Published: 6 March 2015 Abstract. It is important to understand the mechanisms that that 35 % comes from agricultural lands, 23 % from forested control the fate and transport of suspended sediment (SS) lands, 23 % from developing lands, and 19 % from stream in rivers, because high suspended sediment loads have sig- channels. The results of this study improve our understand- nificant impacts on riverine hydroecology. In this study, ing of sediment production and transportation in the Ishikari the SPARROW (SPAtially Referenced Regression on Wa- River basin in general, which will benefit both the scien- tershed Attributes) watershed model was applied to esti- tific and management communities in safeguarding water re- mate the sources and transport of SS in surface waters sources. -
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.