Kazuo OKAYAMA , Yasuji TAKANO
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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 -
Keys to the Flesh Flies of Japan, with the Description of a New Genus And
〔Med. Entomol. Zool. Vol. 66 No. 4 p. 167‒200 2015〕 167 reference DOI: 10.7601/mez.66.167 Keys to the esh ies of Japan, with the description of a new genus and species from Honshu (Diptera: Sarcophagidae) Hiromu Kurahashi*, 1) and Susumu Kakinuma2) * Corresponding author: [email protected] 1) Department of Medical Entomology, National Institute of Infectious Diseases, Toyama 1‒23‒1, Shinjuku-ku, Tokyo 162‒8640 Japan 2) IDD Yamaguchi Lab., Aobadai 11‒22, Yamaguchi-shi, Yamaguchi 753‒0012 Japan (Received: 9 June 2015; Accepted: 2 October 2015) Abstract: A new genus and species of the Japanese Sarcophagidae, Papesarcophaga kisarazuensis gen. & sp. nov. is described and illustrated from Honshu, Japan. Practical keys to the Japanese 43 genera and 122 species are provided including this new species. A check list and data of specimens examined are also provided. Key words: Diptera, flesh flies, new species, new genus, Sarcophagidae, Japan INTRODUCTION The collection of Sarcophagidae made by the first author was studied during the course of the taxonomical studies on the calypterate muscoid flies from Japan since 1970 (Kurahashi, 1970). This was a revision of the subfamily Miltogramatinae dealing with seven genera and 14 species. Before this, Takano (1950) recorded seven genera and nine species of Japanese Sarcophagidae. Many investigation on the Japanese flesh flies made by Drs. K. Hori, R. Kano and S. Shinonaga beside the present authors. The results of these authors were published in the part of Sacophagidae, Fauna Japanica (Insecta: Diptera) and treated 23 genera and 65 species of the subfamilies of Sarcophaginae and Agriinae (=Paramacronychiinae), but the subfamily Miltogrammatinae was not included (Kano et al., 1967). -
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 ......................................................... -
FY2017 Results of the Radioactive Material Monitoring in the Water Environment
FY2017 Results of the Radioactive Material Monitoring in the Water Environment March 2019 Ministry of the Environment Contents Outline .......................................................................................................................................................... 5 1) Radioactive cesium ................................................................................................................... 6 (2) Radionuclides other than radioactive cesium .......................................................................... 6 Part 1: National Radioactive Material Monitoring Water Environments throughout Japan (FY2017) ....... 10 1 Objective and Details ........................................................................................................................... 10 1.1 Objective .................................................................................................................................. 10 1.2 Details ...................................................................................................................................... 10 (1) Monitoring locations ............................................................................................................... 10 1) Public water areas ................................................................................................................ 10 2) Groundwater ......................................................................................................................... 10 (2) Targets .................................................................................................................................... -
FY2018 Results of the Radioactive Material Monitoring in the Water Environment
FY2018 Results of the Radioactive Material Monitoring in the Water Environment March 2020 Ministry of the Environment Contents Outline .......................................................................................................................................................... 1 Part 1: National Radioactive Material Monitoring in the Water Environment throughout Japan (FY2018) . 6 1 Objective and Details ............................................................................................................................. 6 1.1 Objective .................................................................................................................................... 6 1.2 Details ........................................................................................................................................ 6 2 Survey Methods and Analysis Methods .............................................................................................. 19 2.1 Survey methods ....................................................................................................................... 19 2.2 Analysis methods ..................................................................................................................... 20 3 Results ................................................................................................................................................. 22 3.1 Detection of total β radioactivity and γ-ray emitting radionuclides .......................................... 22 (1) Public water -
Geomorphological Environment for Inundation Attacks: a Comparative Research
立命館地理学 第 30 号(2018)61-75 Geomorphological Environment for Inundation Attacks: A Comparative Research NUKATA Masahiro* The author compares different inundation I. Introduction attacks selected through geomorphological con- There were various tactics to assault castles siderations of them. The research started from and forts in Medieval Japan, including frontal, making landform classification maps of the fire, inundation, hole, starvation and surprise plains concerned based on the observation attacks. Usually multiple modes of attacks were using 1/10,000 areal photos. Archives, old pic- combined. For inundation attacks, the army torial maps and old geomorphological maps started with frontal attack, closing in on an were also surveyed. Geomorphology of inunda- enemy castle from all sides and then built an tion related remains were studied by observing embankment around the castle and introduced ruins and geological formations at the excava- water from the river to flood or isolate the tion sites as much as possible and by reviewing castle. the past excavation reports. There are four well-known inundation attacks in Japan: Bicchu Takamatsu Castle where II. Inundation attack of Bicchu Hideyoshi Toyotomi was involved, Owari Takamatsu Castle Takegahana Castle, Musashi Oshi Castle and Kii Ohda Castle (Figure 1). The author has a 1. Chugoku-no-eki (war) and inundation different idea from common view that Kii Ohda attack of Takamatsu Castle Castle was attacked with 5 km-long embank- The attack against Takamatsu Castle 2) took ment built around the castle located on the place in May and June 1582 during the last Holocene river terrace and therefore reviewed period of Chugoku-no-eki. -
Table of Japanese Cuisine
Table of Japanese Cuisine Wakayama Prefecture 1 Catalogue of Wakayama Prefecture’s Specialties の食卓 Table of Japanese Cuisine Grand mountains, the sea and the powerful Kuroshio Current, bright sunlight, and wisdom of people living in such a wonderful environment – Wakayama Prefecture is home to a wide variety of specialties developed through the rich nature, culture, and people. 2 Climate: Blessings from the Earth and the Sea 4 Premium Wakayama 10 Wakayama’s distinctive specialties are recommended with a focus The gourmet food of Kishu comes from its bountiful nature. on safety and reliability. Food Culture: Food History Traced to “Kinokuni” 6 Kishu Ume-Plum Burger 12 A pairing of Wakayama ume-plums and hamburgers, developed Japanese cuisine originated from the enterprising spirit of people in Kishu. with overseas sales in mind. Taste of the Hometown: Honor and Pride of the Hometown 8 Wakayama Punch 13 As a kingdom of fruit, Wakayama is proud to provide this While people in the past demonstrated their wisdom, people today pursue outstanding product filled with love for our hometowns. even deeper, which underpins Japanese cuisine. < Products Catalogue > Fruit 14 Vegetables 19 Livestock Products 22 Seafood 24 Processed foods 29 Wakayama Seasonal Product Calendar 36 Share of Wakayama’s Farm and Marine Production 38 Monde Selection 39 ※ Produce amounts and other information in this brochure are based on statistics in 2016. 3 Specialties from Wakayama lend flair to the Climate “Table of Japanese Cuisine.” W AKAYAMA In Wakayama, while the climate is moderate in some parts, the deep mountains The gourmet food of generate changes in temperature in other areas. -
Characteristics of Peach Summer – Harvest Peach Cultuivars Every Morning, the Farmers Start to Harvest Peach Fruits Before Sunrise
Hashimoto City Iwade Katsuragi City Town Kudoyama Town Wakayama City Kinokawa City Koya Town The Main Production Areas in Wakayama Prefecture Kimino Town Kainan City Arida City Aridagawa Town Yuasa Town Hirogawa Yura Town Town Hidakagawa Town Kitayama Village Hidaka Town Mihama Gobo Town City Minabe Town Inami Town Tanabe City Shingu City Kamitonda Town Shirahama Town Nachikatsuura Town Kozagawa Town Taiji Town Susami Town Kushimoto Town Wakayama Calendar of Operations for Peach Cultivation January February March April May June July August September October November December Harvesting Thinning Artificial Thinning Fruitlets/ Pruning Buds Pollination Regulation of Young Shoot Management in Summer Pruning Fertilization Bagging/ Mulching/ Removing Bags after Harvest Basal Fertilization For More Information on Foods of Wakayama Prefecture… To inquire about foods of Wakayama… Wakayama Specialties Online Catalog Wakayama Prefecture Peach http://www.pref.wakayama.lg.jp/prefg/071700/database/dbtop.html Agriculture, Forestry and Fisheries Department Wakayama Intermediate Product Catalog Food Promotion Division http://www.pref.wakayama.lg.jp/prefg/071700/proc/index.html http://www.pref.wakayama.lg.jp/prefg/071700/index.html <Wakayama Specialty Shop in Tokyo〉 Elaborate Handworks Wakayama Kishikan http://www.kishukan.com <Online Shopping〉 Furusato Wakayama Waiwai Ichiba (Yahoo shopping) Generate Excellent Flavor http://store.shopping.yahoo.co.jp/waiwai071700 4 T he Largest Peach Production Area in Western Japan – With a History of Over 300 Years Peach is one of the representative summer fruits. Covered in slightly reddish and velvety skin, it contains juicy, sweet and tender flesh. Wakayama is proud of its largest shipment volume of peach in Western Japan. Its major production area in Wakayama is the Naga region and the surrounding area, the middle basin of the Kinokawa River. -
Characteristic of Water Chemistry for Arima Type Deep Thermal Water in the Kinokawa River Catchment, Kii Peninsula, Japan
International Journal of GEOMATE, Oct., 2019 Vol.17, Issue 62, pp. 158 - 166 ISSN: 2186-2982 (P), 2186-2990 (O), Japan, DOI: https://doi.org/10.21660/2019.62.7156 Special Issue on Science, Engineering & Environment CHARACTERISTIC OF WATER CHEMISTRY FOR ARIMA TYPE DEEP THERMAL WATER IN THE KINOKAWA RIVER CATCHMENT, KII PENINSULA, JAPAN *Hiroyuki Ii1, Hiroki Kitagawa2, Takuma Kubohara2 and Isao Machida3 1Faculty of Systems Engineering, Wakayama University, Japan; 2 Graduate School of Systems Engineering, Wakayama University, Japan; 3 Geological Survey of Japan, Japan *Corresponding Author, Received: 10 March.2019, Revised: 01April. 2019, Accepted: 20 April. 2019 ABSTRACT: All soluble substances for coastal shallow well waters were higher than those for the inland well waters in the Kinokawa River catchment along the Median Tectonic Line in Wakayama Prefecture, Japan. Coastal areas were thought to have been contaminated by sewage wastewater due to a high population. Shallow groundwater is thought to have derived from precipitation because all shallow groundwater is on the Global Meteoric Water Line. There are many hot springs in the Kinokawa River catchment along the Median Tectonic Line in Wakayama. Most hot spring waters are thought to originate from mixing of shallow groundwater and Arima type deep thermal water because of their δ18O and δD values. High Li+ concentration water was found for Arima type deep thermal water. In particular, Li+ concentration of Nohan No.5 borehole, 1100m in depth, in the center of Kinokawa River catchment reached 100 mg/l and this value was the highest in Japan. However, both δ18O and δD values for hot spring waters did not always increase with Li+ and - 18 + - + HCO3 concentrations although both δ O and δD values increased with Na and Cl concentrations. -
Three Species of a Genus Tenuibaetis (Ephemeroptera: Baetidae) from Japan, with Description of a New Species
Limnology (2011) 12:213–223 DOI 10.1007/s10201-010-0342-0 RESEARCH PAPER Three species of a genus Tenuibaetis (Ephemeroptera: Baetidae) from Japan, with description of a new species Toshihito Fujitani • Norio Kobayashi • Toshiya Hirowatari • Kazumi Tanida Received: 31 March 2010 / Accepted: 5 December 2010 / Published online: 11 February 2011 Ó The Japanese Society of Limnology 2011 Abstract We associated nymphs of three Tenuibaetis Keywords Tenuibaetis Á Baetidae Á New species Á species with their imagoes by rearing. Herein we redescribe Japan Á Diagnostic characters T. flexifemora and T. pseudofrequentus, and also provide description of a new species T. parvipterus. Tenuibaetis pseudofrequentus is morphologically similar to T. flexife- Introduction mora in the imaginal stage, but we can distinguish these two species by the color patterns of their nymphs and their Kang and Yang (in Kang et al. 1994) erected a subgenus geographical distribution. Tenuibaetis parvipterus is dis- Tenuibaetis from Taiwan. This subgenus included three tinguishable from the other two species by the fore femur, species, and Baetis (Tenuibaetis) pseudofrequentus Mu¨ller- which is not bending distinctly, and abdominal sterna Liebenau 1985 was designated as type species (Kang et al. without distinct spots of male imago, reduced hind wing 1994). This subgenus is distinguishable from the other and abdominal sterna without distinct spots of female subgenera of Baetis (sensu lato) by the following charac- imago, and difference in color patterns of the abdomen of ters of nymphs: mandible with smooth medial margin, nymphs. Diagnostic characters of these species were pointed apex of labial palpus, villopore on femur and tabulated. paraproct with a patch of notched scales (Kang et al. -
Early Pleistocene Plant Biostratigraphy of the Shobudani Formation, Southwest Japan, with Reference to Extinction of Plants1)
第 四 紀 研 究 (The Quaternary Research) 29 (1) p. 1-15 Apr. 1990 Early Pleistocene Plant Biostratigraphy of the Shobudani Formation, Southwest Japan, with Reference to Extinction of Plants1) Arata MOMOHARA2), Kiyohide MIZUNO3), Sei-ichiro TSUJI4) and Shohei KOKAWA4) Plant macrofossil assemblages from the Shobudani Formation in the northern part of Hashimoto City, Wakayama Prefecture, are described. 221 taxa including 21 extinct plants are identified. Six assemblage zones, SB-I to SB-VI in ascending order, are established. The zones SB-II and SB-V are characterized by the occurrence of the members belonging to subarctic and cool-temperate elements indicative of a cool climate. The zones SB-I, SB-III, SB-IV and SB-VI are characterized by the occurrence of the members belonging to warm-temperate and/or subtropical elements associated with some cool-temperate elements, suggesting warm climatic conditions. The coexistence of the members attributed to both subtropical and cool-temperate elements in the zone SB-III suspects warm winters and cool summers. A scarcity of the members belonging to the cool-temperate elements associated with common subtropical and warm- temperate elements in the zone SB-VI indicates warmer summer conditions than in the zone SB-III. Based on the mode of the occurrence of fossil plants, the Shobudani Formation is thought to be early Pleistocene in age. The late early-Pleistocene extinction of Cyclocarya paliurus, Pterocarya aff. stenoptera, and Picea koribai is assumed to a lowering of the winter temperatures. In respect to the extinction of Metasequoia glyptostroboides from the area, a warming of the summer climate and a change in topography together with repeated changes in overall climatic deterioration are suspected. -
UNIVERSITY of CALIFORNIA RIVERSIDE Fujimoto Diaries 1941-1946: Japanese American Community in Riverside, California, and Toranos
UNIVERSITY OF CALIFORNIA RIVERSIDE Fujimoto Diaries 1941-1946: Japanese American Community in Riverside, California, and Toranosuke Fujimoto’s National Loyalties to Japan and the United States During the Wartime Internment A Dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in History by Akiko Nomura December 2010 Dissertation Committee Dr. Clifford E. Trafzer, Chairperson Dr. Lane Ryo Hirabayashi Dr. David Biggs Copyright by Akiko Nomura 2010 This Dissertation of Akiko Nomura is approved: Date__________________ ____________________________________ Committee Chairperson Date__________________ _____________________________________ Date__________________ _____________________________________ University of California, Riverside Acknowledgments During my years of study and research at the University of California, Riverside, I have accumulated many debts of gratitude. Since it is impossible to thank everyone individually, I would like to thank my mentors, colleagues, friends and family for their encouragement and support during this long process. Without their assistance, this dissertation would not have been possible. I also owe thanks to several organizations for their generous financial support. The Knox and Carlotta Mellon Fellowship, the Department of History, UCR, allowed me to travel to Arizona and conduct research at the University of Arizona. The findings from this research resulted in Chapter 5. The Dissertation Writing Fellowship, the Department of History, UCR, allowed me to focus on translation of the Fujimoto Diaries for a year. The Alpha Association of Phi Beta Kappa Alumni in Southern California enabled me to continue working on translation and of the Fujimoto Diaries. I would like to thank many individuals who have helped me complete the project. The Fujimoto family in the United States and in Wakayama shared the memories of their childhood with me in interviews and via emails messages.