Translation Series No. 726 C R Clin,104

Total Page:16

File Type:pdf, Size:1020Kb

Translation Series No. 726 �C R Clin,104 Nb- -ay) - «4 EIS Prv„ FISHPRIES RESEARCH BOARD OF CANADA /1/24 , 1 . Translation Series No. 726 c r CliN,104 .', The distribution.of Cottus laoonicus Okada (Cottidae) and of Tukugobius flumineus 1:Azuno (Gobiidae), with - special reference to peculiarities related to both the land-locking and their Speciation • from amphidromous ancestors By Nobuhiko,,f•izuno - • . From: Osaka Gakugei University (Pf-e- S>, pp. l29-161,,,,.19ô5, Translated by: Kenji Makin°, 7 7-7- - BUreau -for Translations Foreign-Languages- Division, - . Department of the Secretary of State Of Canada Fisheries Research Board of - Canada Biological -Station, - Nanaimoi- B. - .C. ----- • I ' . r fgt.; 44. sPEPARTMENT OF THE SECRETARY OF STATE r SECRÉTARIAT D'ÉTAT BUREAU FOR TRANSLATIONS BUREAU DES TRADUCTIONS FOiZE-IGN LANGUAGES ; DIVISION DE-S LANGUES DIVISION CANADA ÉT.'2AN&.-"!`2'ES TRANSLATED rRom TRADUCTION DE IN •ro - Japp nos ri sh SUI3JECT - SUJET Fish (lard-lock irg. and spooi.?,t:ion) AUTHOR - AUTEUR Yobuhiko Mizuno TITLE IN ENGLISH - TITRE ANGLAIS • I) The ..bl istri.buti on of Cottus Jp..nonicus 'Tuk-up,-obitims 1 71unineu s 7',.eference to thirdr /FrE- tr[1. -1,' ri-ties in both LI itand-Locking ar.d Seciatien erorn. YITLEIN roREIGN LANGUAGE - TITRE EN LANGUE ETRANGEklE d . ,. • ``. • „ ■ “.17 \% 7 11 ( C 1 (-2 .7.2l > - / ) a./ 17.1" . ... (0 • tt , 1.7 1 • • RErERENCE - ReFdRENCE (NAmE OF Book: OR PUBLICATION - NOM DU LIVRE OU PuBLIcATtoN) Osakaukbge71 University Per -l.ndfical . PUBLISHER - dDITEUR OsakaE;akuFèi University Press à CITY - VILLE DATE PAGES Osaka, Jan. n . 1963- 129-161 • Derartrent Of Fisb.c.rrIps , Iknc ino . 3[297 • - REQUEST RECEIVED FRoM OUP. NUER T)-1-0 1-)1, REQUIS PAR * No -CRIZ DOR • • Ken f, a no - DEPARTMENT TRANSLATOR • - MINISTRE TRADUCTEUR • - . - . - ')7 YOUR NUMBER DATE' CoMPLEV-:D - ( VOTRE DosSIER NO REMPLIE LE DATE RECEIVED • Jart2r3r,1966. REÇU LE - • . 80r-200-10- 47- ;1 (129) - The Distribution of Cottus Janonicus and TukuJ...-obious Flur_lineus with Specinl Reference to t:12eir Pnculinrities in both Land-Docking and Sneciation - from Arnhidromous Ancestors Nobuhiko MIZUNO Biological Laboratory • Osaka Gakugei University 10. Foreword The migration of fish, es vieil as that of birds, has been known as a peculiar phenomenon and has attracted the attention frP of scientist for a long time* Various classifications of these fish have been uu ,7gested (Myers, 1949). It is well known that some migratory fish cone to inhabit fresh-water regions permanently. This -phenomenon is Called land-locking. In my reportson the Tukugobious filleineus and the large-egg type Cottus japonicus of 1960 and 1961, I suggested that they were the fish which were land-locked and speciated fron the migratory Rhinogobius brunneus + (or i!elated-species) and the small-egg type CottUs japonicus (Lama°, 1960; Mizuno Tanba, 1961). In the following chapter, i would like to study the relationship. between the migration and land-locking of such fish mainly in our country and present the peculiar aspect of the land-locking. of the above-mentioned Tukugobious flumineus and the large-egg type Cottus . japonicus._ Further- more, I would like to investigate their way of spe(eiation in reference to their geographical distribution. RO similis Gill was formerly'used as the name of this species until ft was corrected by Tagaki (1962) and R. brunneus (Temminàk & Schlegel) . waà cdoptd. - ,- .• 2 I waeJ given a great deal of help by many people with the investigaticn and arrangement of the data. Professor D. Miyagi of Kyoto University and Professor H. Sugino of Osaka Gakugei University encouraged me and cornented on my study. Dr. Niwa of the Gifu prefecture and Dr. Kawanabe and i his group of Kyoto. University also gave me a great deal of 'assistance. Professor K. Dotsu of Nagasaki University, Profess- or I. Toyama of Tokyo University, and Professor K. Matsubara of Kyoto University gave me many specimens with helpful comment. Professor M. Tsuda of the Nara Womens University, Dr. H. Shiraish of the Fresh-water Products Laboratory, the Saito Requital Museum of Sendai-city, Dr. S. Kimura of Urama-city, Messrs. M. Urata 9 K. lirai of Osaka Gakugei University, and many others helped me a great deal with the collection of specimens. To all of the above-mentioned I would like to extend my deep-felt thanks. * Th,- Peculiarities of the Land-lockinz-of the'Lpree-eeg Tyne Cottus japonicus t,md Tul_rueobious flumineus - The classification which was published by Myers in 1949 (130) seerned to be Quite relevant to land-locking in reference to the typé of migration. He named the migration between .. sea-water and fresh-water Diadromous migration, and divided this category into, three sub-categories; namely, Anadromous migration, Catadromoils migration, and Amphidromous migration. The Anadromous migration and Catadromous migration-are seen, typically'in the salmon-trout family and the,eel family. The fore' goes from the sea to fresh-water regions in its •n ,.tu-re period, and the latter reversely from fresh-water .regions to the .sea. Both imigrations - have the same purpose of spawning. Amphidromous Migratory fish, however, travel :,back and forth between the sea 'and.fresh-jfiater in their infancy„This is not - a spawning migration. According to Myersp• the : Sicydium ofgoby. ' genus and its relatives are examples. He says that these gobies lny eLigsin rivers and the hatched infants soon go down to the sea, live'there during the first half of their infancy, return to rivers, grow up there, and lay eggs. , As for:the Japanese-grown Anadromaus migratory fish, there \!- 1 \ salmon and Salmopluvius•genera of the salmon-trout family; • are sJ <\ and Gastcrosteus aauleatus of the stickleback family. Besides, the 1 ariprsjy family migrates in the same manner, although it •••■ .\ does not belong to fish. These fish all go un rivers for spawning in their mature period and in re lation to land-locking it is interesting in what stage of their • growth they go down to the sea. They do not go down to the sea immediately after hatching. For example, the fish which. the salmon and Salno pluvius genus, and Tribolodon belong to • hakuensis have about 10 cm of body-length before going down, and the Gestarosteus aculeatus, whose full body-length is about 10 cm, start going down at about 3 cm. The lamprey family also stays in fresh-water until the completion of metamorphosis. As described above, they spend the first half of their infancy in fresh-water regions. It is not irrelevant to the above-mentioned fact that land- locking often occurs among such fish. For example, each of the Oncorhynchus masou and Oncorhynchus nerka of the' salmon genus; Salvelinus malma and Salvelinus leucomaenis of the Salmo pluvius genus; Tribolodon haluensis and Gasterostus aculeatus of the stickleback family produces land-locked • fish such as Salmo nocrostoma, 0.n.f. adonis; and Tribolodon hakuensis, Gastercstus aculeatus (the last two have not been named yet). Furthermore those, except 0.n0f. adonis, are all land-locked in rivers (fluvial land-locked). Those which live in fresh- water regions and that in rivers for the first.half of their infancy should not have nuch difficulty renaining,there to live for their lifetime. In fat, land-locking occurs among them and there are also many examples that such land-locked fish live with migratory ones, such as Salvelinus nalma and its land-locked fish (-U\i- x.c..7,,:.÷,te. in Saghalien, S. leucomaenis and Oncorhynchusmnsou andtheifc land-locked fich and Salmo mocrostoma in Hokkaido and Tohoku district, and G. aculeutus.and itsland-locked fish • (Kobayashi, 1957) in the Ishikari River. The term "land-lockine gives an_impression that migratory fish are passively locked-infreshwater regions, but as (131) 0no v(1933) . about Oncorhynchus masou and Ricker (1938) about Oncorhynchus nerka, the 'behaviour of lan d-locking seems to be explained mainly by the relationship between growth nrd naturity. It is not an abnormal phenomenon that Anadromous migratory fish are land-locked, since they do not have to change their early life histories, and in tact they never do. It also happens very easily that the descendants of land-lockec fish become migratory fish again. This phenomenon is proved in Oncorhynchus masou (Ono, 1933) 9 and in Oncorhynchus nerka (Ricker, 1938). It is known in Tohoku district that the migra- , tory female -Oncorhynchus masou inter-breeds with the land- locked tale and that rot of their male descendants remain in fresh-water regions, but that most of the females go . down to the sea (Tanaka, 1956). In short, in Anadromous migratory fish, migration and land-locking are, to a great extent, reversible. ;As: for Japanese-grown Catadromous migratory fish, there are Anguilla japonica, A. marmorata, and Trachidermus fasciatus and Cottus hazika of the Cottus japonicus family. There are, however, no land-locked fish reported. The Catadromous migra- tory fish live in the sea during the first half of their infancy, cone up the rivers, and go back to the sea again in their mature period to lay eggs there. The life history is completely reversed in this case and it seems to be difficult for them to become land-locked fish. Japanese-grown Amphidrous migratory fish are Plecoglossus artivelis, fish of the goby family such as Eleotris oxycephala, Rhinogobious brunneus, R. ziUrinus, Chaenogobius urotaenia, Ch. annularis, Tridentiger obscurus, iuciogobius guttatus, and Sicydilim- japonicum, and the small-egg type Cottus japonicus. They go doWn to . the seaa immediately after hatching, spend the first half of their infancy:there. and.then they goup . and spawn. In this:regard they are rivers where they grow . Similar to 1,iyers' (1949) examples of Sicydium and its relativ-. es. From the morphological point of view, their bodies are frail-looking and their fins are incomplete immediately after hatching, and in theÉe respects they are distinctively differ- ent from Anadromous migratory fish in the .
Recommended publications
  • Biogeography and Evolution of the Carassius Auratus-Complex in East
    Takada et al. BMC Evolutionary Biology 2010, 10:7 http://www.biomedcentral.com/1471-2148/10/7 RESEARCH ARTICLE Open Access Biogeography and evolution of the Carassius auratus-complex in East Asia Mikumi Takada1,2*, Katsunori Tachihara1, Takeshi Kon2, Gunji Yamamoto2, Kei’ichiro Iguchi3, Masaki Miya4, Mutsumi Nishida2 Abstract Background: Carassius auratus is a primary freshwater fish with bisexual diploid and unisexual gynogenetic triploid lineages. It is distributed widely in Eurasia and is especially common in East Asia. Although several genetic studies have been conducted on C. auratus, they have not provided clear phylogenetic and evolutionary descriptions of this fish, probably due to selection bias in sampling sites and the DNA regions analysed. As the first step in clarifying the evolutionary entity of the world’s Carassius fishes, we attempted to clarify the phylogeny of C. auratus populations distributed in East Asia. Results: We conducted a detailed analysis of a large dataset of mitochondrial gene sequences [CR, 323 bp, 672 sequences (528 sequenced + 144 downloaded); CR + ND4 + ND5 + cyt b, 4669 bp in total, 53 sequences] obtained from C. auratus in East Asia. Our phylogeographic analysis revealed two superlineages, one distributed mainly among the Japanese main islands and the other in various regions in and around the Eurasian continent, including the Ryukyus and Taiwan. The two superlineages include seven lineages with high regional specificity that are composed of endemic populations indigenous to each region. The divergence time of the seven lineages was estimated to be 0.2 million years ago (Mya) by a fossil-based method and 1.0-1.9 Mya by the molecular clock method.
    [Show full text]
  • 1 to the Leaders and People of G7 Member States: Proposals For
    To the Leaders and People of G7 Member States: Proposals for Pursuit of Genuine Prosperity through River Basin Thinking We the undersigned are members of citizens’ groups in the Tokai area, host to the Ise-Shima Summit. Despite our various standpoints, we have united to advocate for the “Ise Bay Initiative,” aiming to realize a sustainable and productive future based on river basin (bio-regional) thinking. Presenting the following experience and good practices, we propose to the leaders and the people of G7 member states to share the idea of Ise Bay Initiative and work together for a better future. “River basin thinking” means viewing the entire area of rivers flowing into the Ise Bay as one bio-region, and addressing issues within that region not on a reactive piecemeal basis but with the vision of integrated local development to enrichen the ecological value of the entire river basin area. Ise Bay basin communities have kept ideal relationship with nature and maintained their livelihood by utilizing the natural resources in co-existence with abundant forests, large and fertile plains, and rich and clear rivers like Kiso, Nagara, and Ibi rivers. However, as seen in the example of Yokkaichi Air Pollution which occurred after the post-war high economic growth period, air and water pollution that contaminated air and waters in the area severely affected human health and damaged fishery resources and as the result threatened people’s livelihoods. The pollution caused by Yokkaichi Petrochemical Complex built in northwest coast of Ise Bay deprived many people of their right to a healthy and safe living environment.
    [Show full text]
  • Title Rb-Sr Geochronology and Petrogenesis of the Late
    Rb-Sr Geochronology and Petrogenesis of the Late Mesozoic Title Igneous Rocks in the Inner Zone of the Southwestern part of Japan Author(s) Seki, Tatsuya Memoirs of the Faculty of Science, Kyoto University. Series of Citation geology and mineralogy (1978), 45(1): 71-110 Issue Date 1978-07-31 URL http://hdl.handle.net/2433/186625 Right Type Departmental Bulletin Paper Textversion publisher Kyoto University MEMolRs oF THE FAcuLTy oF SclENcE, KyOTO UNIvERSITy, SERIES oF GEoL. & MINERAL., Vol. XLV, No. 1, pp. 71-110, 1978 Rb-Sr Geochronology and Petrogenesis of the Late Mesozoic Igneous Rocks in the Inner Zone of the Southwestern Part of Japan By Tatsuya SEKi* (Received August 30, lq. 77) Abstract Rb-Sr isotopic measurements have been made on Cretaceous intermediate-acid igneous rocks from four districts, Yamaguchi, Hime.ii, Koto and Nohi, ofthe inner zone ofsouthwestJapan, and more than ten whole rock and internal isochrons have been obtained. Isochron ages of about 110 m.y. have been obtained from volcanic rocks of all of four districts. Another age of volcanic activity is about 70 m.y. The age ofgranitic rocks obtained is about 80-90 m.y. Initial Sr isotope ratios range from O.7051 to O.7103. The variation of these initial Sr ratios is more closely related with the crustal structure than with the age. Rb/Sr ratios (O.05-24) are higher than those of other calc-alkaline rocks of circum-Pacific regions. These data have been interpreted as that the parental magmas were generated from old lower crustal materials. Local geochronology, space-time relations of the igneous activity, the age of the "Roseki" deposits and the relation between age and paleomagnetism are discussed in detail.
    [Show full text]
  • Annex VIII Casestudy0502 Hid
    IEA Hydropower Implementing Agreement Annex VIII - Hydropower Good Practices: Environmental Mitigation Measures and Benefits Case Study 05-02: Water Quality – Hida River System, Japan Key Issues: 5- Water Quality 14- Development of Regional Industries Climatic Zone: Cf: Temperate Humid Climate Subjects: - Selective intake, techniques to operate a group of dams Effects: - Mitigation of turbid water persistence Project Name: Hydropower Dams in Hida River System Country: Gifu Prefecture, Japan (Asia) (N35˚56’ – N36˚4’, E137˚15’ – 29’) Implementing Party & Period - Project: Chubu Electric Power Co., Inc. 1969 (Completion of construction) - - Good Practices: Chubu Electric Power Co., Inc. 1983 (Commencement of operation) - Key Words: turbid water, selective intake, operation of reservoirs Abstract: In the Hida River basin, there are several power stations, and turbid water persistence became a problem shortly after the completion of the Asahi Dam in 1953. To solve this problem, selective intake facilities were constructed at the Asahi Dam and the Takane No.1 Dam. Using these facilities, coupled with power plant operation at 4 dams in the Hida River, the persistent turbidity has been gradually decreasing. 1. Outline of the Project The Hida River is the Kiso River System’s largest tributary with a total watercourse length of 134km and a total catchment area of 2,177m 2 that originates in Mt. Norikura and Mt. Ontake located in the southernmost part of the North Japan Alps and flows southward meeting many tributaries including the Akigami and Maze Rivers to finally join the Kiso river in Mino Kamo City (Fig.-1). Many power source development projects have been conducted in the Hida river basin since long ago, and currently the total number of power stations and the total of the permitted/approved maximum outputs are 23 and approximately 1.14 million kW, respectively (Table-1).
    [Show full text]
  • Title Destructive Effects of the Estuary Dam on the Nagara River's
    Destructive Effects of the Estuary Dam on the Nagara River's Title Environment, and the Program for its Regeneration Author(s) 粕谷, 志郎; 村瀬, 惣一; 青山, 己織 Citation [岐阜大学地域科学部研究報告] no.[20] p.[1]-[22] Issue Date 2007-02-28 Rights 岐阜大学地域科学部 (Faculty of Regional Studies, Gifu Version University) / リバーポリシーネットワーク(NPO) (River Policy Network(NPO)) URL http://hdl.handle.net/20.500.12099/15555 ※この資料の著作権は、各資料の著者・学協会・出版社等に帰属します。 BulletinoftheFaculyofRegionalStudies,GifuUniversityVol.20:1-22.(2007) DestructiveE恥ctsoftheEstuaryI)amontheNagaraRiver,s Environment,andtheProgram払ritsRegeneration ShiroKasuya,SohichiMuraseandMioriAoyama GifuUniversity,Defunctperson,RiverPolicyNetwork(NPO) (Received:November27,2006) Abstract TheplanOftheNagaraRiverestuarydamwasissuedin1960・Thepurposewasasupplyofthefresh watertoIseBayindustrialarea・Thoughitwastheplanforsupportlngtheeconomicgrowth・aWater demanddrasticallydidnotexpandafterwards,andtheoppositionmovementmainlyonthefisheryparty wasalsointensified・Afterthe一一Anpachifl00ddamage叩in1976,however,thefloodcontroIpurposeof thedamwasemphasized・Theriverbottommustbedredgedinordertorunthefloodsafely・Thesalt waterwillgoup,Whenitwillbesodone,andtheagrlCulturesaltdamagewillbecaused・Estuarydam, whichstopsthis,Callsitthenecessity・Theoppositionmovementonceceases,anditbeganconstruction in1988.It was almost simultaneous,and the new opposition movement mainly on environmental problembecamepopular・However,theoperationwasstartedin1995,Whilethefearoftheadverse effecttotheenvironmentdoesnotfadeaway. Afterwards,thesludgepilesupintheriverbed,benthosessuchastheclamsdisappearalmost,and
    [Show full text]
  • Japanese Electric Utilities' Efforts for Global Warming Issues
    9:00 on April 18, 2011 Concerning the Fukushima Daiichi NPP Accident Caused by the Great East Japan Earthquake Disaster The Federation of Electric Power Companies 電気事業連合会 The Federation of Electric Power Companies 1 We offer our sincerest condolences to all the people who were caught up in the Eastern Japan Earthquake Disaster on March 11. We are extremely aware of the serious concerns and difficulties caused by the accident at TEPCO’s Fukushima Daiichi Nuclear Power Plant and the consequent release of radioactive material, both for those living nearby and the wider public. We most deeply apologize for this situation. Working with the support of the Japanese Government and related agencies, TEPCO is making the utmost effort to prevent the situation from deteriorating, and the electricity industry as a whole is committing all its resources, including vehicles, equipment and manpower, toward resolving the situation. 電気事業連合会 The Federation of Electric Power Companies 2 Outline of the Tohoku-Pacific Ocean Earthquake Date of occurrence: 14:46 on Friday, March 11, 2011 Epicenter: Offshore Sanriku (38ºN, 142.9ºE), Depth of hypocenter: 24 km (tentative value), Magnitude: 9.0 (The largest in recorded history (130 years) in Japan. The U.S. Geological Survey Office placed the quake as the 4th largest in the world since 1900. ) Hypocenter and seismic intensity Seismic intensity Press release at 14:53 on March 11, 2011 7: Kurihara city, Miyagi prefecture Upper 6: Hitachi city, Ibaraki prefecture, Naraha- cho, Nuclear reprocessing Tomioka-cho, Okuma-machi, Futaba-cho, Fukushima facilities prefecture, Natori city, Miyagi prefecture, etc. Lower 6: Ofunato city, Ishinomaki city, Onagawa-cho, Miyagi prefecture, Tokai village, Ibaraki prefecture, etc.
    [Show full text]
  • Representations of Pleasure and Worship in Sankei Mandara Talia J
    Mapping Sacred Spaces: Representations of Pleasure and Worship in Sankei mandara Talia J. Andrei Submitted in partial fulfillment of the Requirements for the degree of Doctor of Philosophy in the Graduate School of Arts and Sciences Columbia University 2016 © 2016 Talia J.Andrei All rights reserved Abstract Mapping Sacred Spaces: Representations of Pleasure and Worship in Sankei Mandara Talia J. Andrei This dissertation examines the historical and artistic circumstances behind the emergence in late medieval Japan of a short-lived genre of painting referred to as sankei mandara (pilgrimage mandalas). The paintings are large-scale topographical depictions of sacred sites and served as promotional material for temples and shrines in need of financial support to encourage pilgrimage, offering travelers worldly and spiritual benefits while inspiring them to donate liberally. Itinerant monks and nuns used the mandara in recitation performances (etoki) to lead audiences on virtual pilgrimages, decoding the pictorial clues and touting the benefits of the site shown. Addressing themselves to the newly risen commoner class following the collapse of the aristocratic order, sankei mandara depict commoners in the role of patron and pilgrim, the first instance of them being portrayed this way, alongside warriors and aristocrats as they make their way to the sites, enjoying the local delights, and worship on the sacred grounds. Together with the novel subject material, a new artistic language was created— schematic, colorful and bold. We begin by locating sankei mandara’s artistic roots and influences and then proceed to investigate the individual mandara devoted to three sacred sites: Mt. Fuji, Kiyomizudera and Ise Shrine (a sacred mountain, temple and shrine, respectively).
    [Show full text]
  • The Brochure [1.5MB]
    Overview of the IWAYA Dam project Specifications The Iwaya dam, as a comprehensive development project, plays an important role on flood control in Kisogawa River system, as well as is used for irrigation, water supply for domestic and industrial use and hydropower (Chubu Electric Power Co.). In 1969, the project was inherited by Water Resources Development Public Corpora- tion from the Construction Ministry and the construction was performed by Chubu Electric Power Co. After the completion of construction in 1976, Japan Water Agency has been responsible for its management. SpecificationsSpecifications ofof ReservoirReservoir Location Kanayama Town and Gero Maze, Gero City, Gifu Prefecture Catchment Area (Direct:264.9㎢) (Indirect:770.0㎢) Total Capacity 173,500,000㎥ Effective Capacity 150,000,000 ㎥ Sedimentation Capacity 13,800,000 ㎥ Dead Storage Capacity 9,700,000 ㎥ Flood Control Capacity 50,000,000 ㎥ Water Utilization Capacity 61,900,000 ㎥ SSpecificationspecifications ooff DamDam Location Unogen and Onbara, Kanayama Town, Gero City, Gifu Prefecture River Maze river of Kiso River water system Type Tilt impervious core type rock-fill dam Elevation of Crest EL427.50m Height 127.5m Length 366.0m Width of Crest 10.0m Volume of embankment 5,780,000㎥ Spillway capacity 2,400㎥/s Dam Structure Embankment Standard Cross-section Surcharge water level Crest Plan Normal water level Lowest water level Rock zone I Filter Filter High water level of Rock zone I Masegawa No.2 Dam Dumped soil Rock zone II Rock zone II Rock Core Rock Intake tower Longitudinal Section
    [Show full text]
  • Inazawa City Tour Guide Booklet Inazawa Harmony of Five So
    Inazawa City Tour Guide Booklet Inazawa Harmony of Five So All you want to know about sightseeing in Inazawa is in this booklet with handy maps!! Map to Inazawa City HOKURIKU EXPWAY Oyabetonami JCT Kanazawa Takayama Nagano Main Line NAGANO EXPWY Hokuriku TOKAI-HOKURIKU EXPWY Main Line Chuo Main Line Okaya JCT CHUO EXPWY Tokyo Ichinomiya- TOKAI-KANJO EXPWY Nishi IC TOMEI EXPWY Ichinomiya IC MEISHIN EXPWY SHIN-TOMEI EXPWY Inazawa Komaki JCT Suita JCT Nagoya Shizuoka City Toyota JCT Yokkaichi JCT ISE-WANGAN Tokaido Main Line Kameyama JCT EXPWY SHIN-MEISHIN EXPWY Osaka Tokaido Shinkansen HIGASHI-MEIHAN EXPWY Chubu Centrair International Airport Fukuoka / Okinawa Sendai / Sapporo By train Tokyo Nagoya Inazawa Tokaido Shinkansen Tokaido Main Line 1 hr. and 40 min. by "NOZOMI" 10 min. by Local Shin-Osaka Konomiya Tokaido Shinkansen Meitetsu Nagoya Main Line 52 min. by "NOZOMI" 12 min. by Limited Express Kanazawa Gifu Inazawa Hokuriku Main Line / Tokaido Main Line Tokaido Main Line 2 hr. and 36 min. 15 min. by Local by Limited Express "SHIRASAGI" By car Ichinomiya Ichinomiya- Suita JCT JCT Nishi IC Inazawa City Komaki JCT Okaya JCT MEISHIN TOKAI-HOKURIKU 15 min. CHUO EXPWY EXPWY EXPWY 135 min. 120 min. 1 min. Kameyama Ichinomiya Suita JCT JCT Kanie IC IC SHIN-MEISHIN HIGASHI-MEIHAN 20 min. 20 min. MEISHIN EXPWY EXPWY EXPWY 10 min. 70 min. 35 min. Oyabetonami Shizuoka JCT Bisai IC IC TOKAI-HOKURIKU EXPWY 20 min. TOMEI EXPWY 150 min. 140 min. By air Sapporo Chubu Centrair International Airport 1 hr. and 55 min. Sendai Express Konomiya 1 hr.
    [Show full text]
  • Iwaki River System Iwaki River
    Iwaki River system Iwaki River History of Tsugaru Dam April 1988 Implementation plan survey begins Tsugaru Dam April 1991 Mascot Tsugaru Dam Research Office opens Pecker-kun Tsugaru Dam Construction Office opens August 2000 Concluded agreement on general compensation November 2008: Construction of main dam structure begins May 2010 Concrete casting begins August 2014 Concrete casting of main dam structure is completed February 2016: Trial flooding begins September 2016: Trial flooding is completed October 2016: Construction is completed April 2017: Transition made to management and operations Tsugaru Aomori prefecture Dam Akita prefecture Iwate prefecture The Tsugaru Dam is a concrete gravity dam constructed as a redevelopment of the Meya Dam completed in 1960. This is a “multipurpose dam” that has six different roles: flood control, river ecosystem conservation, agricultural water supply, municipal water supply, industrial water supply, and power generation. Concrete casting was performed using the cruising roller compacted dam (RCD) method_only the third such example in Japan (the first in Tohoku). Tsugaru Dam’s functions Mitigating flood disasters Maintaining proper waterflow functions Supplying municipal water Planned flood discharge at dam site: Providing consistent replenishment for Additional water supply to Hirosaki city: Adjusted from 3,100 m3/sec existing water supplies, and conserving 14,000 m3/day to 160 m3/sec the river’s ecosystem. Replenishing irrigation water Generating power Supplying industrial water Replenishes irrigation
    [Show full text]
  • 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
    [Show full text]
  • PICES-2012 Program and Abstracts
    PICES-2012 Program & Abstracts Image: “The Itsukushima Shrine from the sea”, November 25, 2010, watercolour, by Satoshi Arima, retiree of the National Research Institute of Fisheries and Environment of Inland Sea, Hiroshima, Japan. Permission to reproduce this artwork was kindly granted by Mr. Arima. Prepared and published by: North Pacific Marine Science Organization PICES Secretariat P.O. Box 6000 Sidney, BC PICES-2012 V8L 4B2 Canada Tel: 1-250-363-6366 Fax: 1-250-363-6827 Program and Abstracts E-mail: [email protected] Website: www.pices.int October 12-21, 2012 Hiroshima, Japan PICES-2012 Effects of natural and anthropogenic stressors in the North Pacific ecosystems: Scientific challenges and possible solutions North Pacific Marine Science Organization October 12-21, 2012 Hiroshima, Japan Table of Contents Notes for Guidance � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �vi International Conference Center Floor Plan � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � vii Meeting Timetable � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �viii Map of the International Conference Center Area � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � xii Keynote Lecture � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � 1 Schedules and Abstracts S1: Science Board Symposium Effects of natural and anthropogenic stressors in
    [Show full text]