DOCSLIB.ORG

Kumamoto Earthquake Gc Briefing

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Kumamoto Earthquake Gc Briefing GC BRIEFING An Update from GC Analytics® May 2016 KUMAMOTO EARTHQUAKE In April of 2016, at mid-month, the world was once again reminded of the potential power of seismic activity by a series of earthquakes that hit Kumamoto prefecture on the southernmost island of Japan, as well as by the large shake that occurred half way around the world in Ecuador. In this briefing we summarize the basic facts regarding the 2016 Kumamoto Earthquake, including a description of the event itself and the basic seismic background of the area. We also outline the major earthquake coverages provided by Japanese insurers, report on possible loss amounts and list some of the major affected facilities. 1 F-4 | DEPTH OF THE RYUKYU TRENCH AND DEPTH OF HISTORICAL EARTHQUAKES T-1 | EARTHQUAKE EVENTS IN JAPAN STANDARD F-5 | INDUSTRIAL PARKS AND CORPORATIONS IN KUMATOMO PREFECTURE F-1 | EVENTS OF MOMENT MAGNITUDE 6.0 AND LARGER UTC+09 Moment Depth in Epicenter F-3 | EARTHQUAKE INTENSITY BY LOCATION USING MODIFIED MERCALLI INTENSITY UTC+09 Moment Depth in Epicenter Intensity 7.5 Date Time Magnitudekilometers Latitude Longitude Date Time MagnitudekilometersLatitudeLongitude April 14, 2016 21:26:36 (UTC+09) Magnitude 6.2 April 16, 2016 01:25:06 (UTC+09) Magnitude 7.0 32.849oN 130.635oE Depth 10 kilometers 32.782oN 130.726oE Depth 10 kilometers Intensity 8.0 Apr-14 21:26 6.2 10.0 32.849 130.635 Apr-16 01:445.3 10.0 32.695 130.735 D Intensity 7.0 Apr-14 21:424.8 10.0 32.578 130.636 Apr-16 01:455.7 10.0 32.881 130.846 Intensity 8.5 Apr-14 22:075.4 10.0 32.788 130.835 Apr-16 02:044.6 11.7 32.757 130.742 Apr-14 22:224.8 10.0 32.683 130.646 Apr-16 02:494.5 12.2 33.203 131.321 M Apr-14 22:384.8 10.0 32.685 130.711 Apr-16 03:035.4 4.9 32.926 131.043 L Apr-14 22:434.5 10.0 32.704 130.696 Apr-16 03:164.6 18.6 33.086 130.836 J K B Apr-14 23:284.5 10.0 32.785 130.745 Apr-16 03:204.5 19.4 33.101 130.997 I Apr-14 23:294.6 10.0 32.752 130.726 Apr-16 03:264.5 10.0 32.870 130.918 A Aisin Kyushu Co. F Apr-14 23:434.9 10.0 32.783 130.758 Apr-16 03:555.5 13.8 32.980 131.136 B Renesas Semiconductor Package & Testing Apr-15 00:03 6.0 6.0 32.693 130.732 Apr-16 04:184.4 10.6 32.937 130.950 G C Aisin Kyushu Casting Co. D AT Kyushu Co. Apr-15 00:065.3 10.0 32.707 130.701 Apr-16 04:514.7 3.4 32.698 130.734 E NEC Semiconductors Kyushu Yamaguchi Co. H F Kumamoto Technology and Research Park Apr-15 00:344.7 10.0 32.698 130.759 Apr-16 05:344.5 10.0 32.569 130.509 E G Iseki Co. Apr-15 00:504.5 10.0 32.742 130.727 Apr-16 06:314.3 11.0 32.867 131.137 C H NEC Semiconductors Kyushu Yamaguchi Co. Apr-15 01:534.6 11.8 32.696 130.767 Apr-16 06:404.5 10.0 32.945 130.917 A I Fuji Film Kyushu Co. N J Semicon Techno Park Apr-15 02:144.5 10.0 32.713 130.671 Apr-16 07:115.1 10.0 33.256 131.370 K Honda Motor Co. Apr-15 05:104.7 10.0 32.754 130.694 Apr-16 07:234.6 10.0 32.754 130.744 L Kumamoto Core M Miraiaru Co. Source: USGS Apr-15 07:294.6 10.0 32.843 130.791 Apr-16 07:424.1 10.0 32.788 130.645 N Sanwa Kagaku Kenkyusho Apr-15 07:464.5 10.0 32.804 130.729 Apr-16 08:204.5 10.0 32.645 130.667 Source: USGS Apr-16 01:25 7.0 10.0 32.782 130.726 Apr-16 09:164.3 10.0 32.559 130.583 Source: Guy Carpenter Apr-16 09:485.2 9.1 32.848 130.777 T-3 | NUMBER OF DWELLINGS AND THE PERCENTAGE INSURED WITH THE JER Source: Guy Carpenter Apr-16 10:384.3 10.0 32.486 130.465 T-2 | MODIFIED MERCALLI INTENSITY SCALE AND THE POPULATION BY OBSERVED INTENSITY Apr-16 11:024.9 10.0 32.729 130.670 Number of Number of Number of Homes Takeup Number of Homes Takeup Prefecture Zone Prefecture Zone Apr-16 14:034.6 10.7 33.003 131.118 Homes Insured with Rate Homes Insured with Rate Instrumental Intensity I II-III IV V VI VII VIII IX X+ EVENT DESCRIPTION Apr-16 14:274.6 1.3 32.660 130.639 the JER the JER Hokkaido 12,727,000 619,000 22.7%Hyogo 82,460,000 616,000 25.0% On April 14, 2016 at 9:26 p.m., local time, a moment magnitude 6.2 earthquake occurred approximately 12 kilometers Apr-16 16:025.3 16.2 32.747 130.668 Perceived Shaking Not felt Weak LightModerateStrongVery Strong Severe ViolentExtreme Akita2425,000 82,00019.3% Kyoto81,176,000 325,000 27.6% (7.5 miles) west-northwest of Kumamoto city, which is situated in Kyushu, the southernmost main island of Japan. Two Apr-16 17:404.6 3.3 32.766 130.555 Peak Accelerage (%g) <.17 .17-1.41.4-3.9 3.9-9.29.2-1818-34 34-65 65-124>124 Aomori 2 585,000114,000 19.5%Nara8577,000 158,000 27.4% hours and 37 minutes later, a moment magnitude 6.0 earthquake occurred approximately 10 kilometers (6.2 miles) south Apr-16 21:054.6 12.7 32.728 130.750 Niigata2 874,000179,000 20.5%Osaka 84,117,000 1,258,000 30.6% of Kumamoto city. Peak Velocity (cm/s) <0.10.1-1.1 1.1-3.43.4-8.1 8.1-16 16-3131-60 60-116>116 F-2 | EARTHQUAKE SHOCKS FROM APRIL 14TH THROUGH APRIL 17TH, UTC Apr-17 00:144.7 10.0 32.933 130.941 Yamagata 2 407,000 79,00019.4% Shiga8548,000 142,000 25.9% Resistant On April 16 at 1:25 a.m., local time, 28 hours after the first foreshock, an event of moment magnitude 7.0 occurred Apr-17 03:304.3 16.0 33.016 131.050 None None None Very light LightModerateMod./HeavyHeavy Very Heavy Fukushima3 760,000209,000 27.5%Wakayama8 437,000 105,000 24.0% Structures approximately one kilometer (0.62 miles) west-southwest of Kumamoto city1. The events were shallow earthquakes with Apr-17 04:464.6 10.0 32.725 130.680 Potential Iwate3515,000108,000 21.0%Hiroshima 91,273,000 364,000 28.6% Damage Vulnerable None None None LightModerateMod./HeavyHeavy Very HeavyVery Heavy reported depth of 10 kilometers (6.2 miles), according to the U.S. Geological Survey (USGS). The shallow depth of these Apr-17 19:234.7 5.1 32.733 130.564 Structures Miyagi 3 950,000493,000 51.9%Okayama 9817,000 172,000 21.1% events indicated that they occurred on crustal faults, the USGS said. Population Exposed in Gunma4 808,000159,000 19.7%Shimane 9284,000 42,000 14.8% Apr-18 08:354.6 10.0 32.867 130.695 -8,510,000 1,757,000592,000 892,000 00 Damage Prone Areas Ibaraki41,187,000 328,000 27.6%Tottori 9232,000 51,000 22.0% There were a series of foreshocks and aftershocks, shown in maps below, for the four day period that began with the first Apr-18 20:425.3 10.7 33.013 131.092 Source: Guy Carpenter Saitama43,085,000 948,000 30.7%Yamaguchi 9656,000 149,000 22.7% event of April 14. Apr-19 06:204.3 10.0 33.014 131.003 Tochigi4 793,000206,000 26.0%Ehime 10 645,000 148,000 22.9% Apr-19 17:525.1 3.2 32.512 130.567 Chiba52,704,000 897,000 33.2%Kagawa10427,000 126,000 29.5% April 14, 2016 April 15, 2016 April 16, 2016 April 17, 2016 Apr-19 20:474.8 10.0 32.600 130.542 Kanagawa 54,114,000 1,418,000 34.5%Kochi 10 353,000 87,000 24.6% (UTC) (UTC) (UTC) (UTC) Apr-20 03:384.1 5.0 32.480 130.656 Tokyo56,699,000 2,446,000 36.5%Tokushima 10 329,000 89,000 27.1% Apr-21 05:164.5 8.0 33.250 131.433 Aichi63,096,000 1,261,000 40.7%Fukuoka 11 2,296,000 751,000 32.7% Gifu 6 792,000266,000 33.6%Kagoshima 11 802,000 194,000 24.2% Source: Guy Carpenter Source: USGS 1 The source of the moment magnitudes are the USGS. Mie6768,000213,000 27.7% Kumamoto 11 757,000 219,000 28.9% 2 Nagano 6 846,000156,000 18.4%Miyazaki11515,000 123,000 23.9% Shizuoka 61,518,000 453,000 29.8%Nagasaki11626,000 86,000 13.7% Yamanashi6 350,000103,000 29.4%Oita11525,000 118,000 22.5% Fukui7284,000 70,00024.6% Saga 11 321,000 59,000 18.4% Ishikawa 7 466,000111,000 23.8%Okinawa 12 600,000 86,000 14.3% Toyama 7 405,000 81,00020.0% Total 55,931,00016,467,000 29.4% Source: http://www.nihonjishin.co.jp/disclosure/2015/a_05.pdf F-4 | DEPTH OF THE RYUKYU TRENCH AND DEPTH OF HISTORICAL EARTHQUAKES T-1 | EARTHQUAKE EVENTS IN JAPAN STANDARD F-5 | INDUSTRIAL PARKS AND CORPORATIONS IN KUMATOMO PREFECTURE F-1 | EVENTS OF MOMENT MAGNITUDE 6.0 AND LARGER UTC+09 Moment Depth in Epicenter F-3 | EARTHQUAKE INTENSITY BY LOCATION USING MODIFIED MERCALLI INTENSITY UTC+09 Moment Depth in Epicenter Intensity 7.5 Date Time Magnitudekilometers Latitude Longitude Date Time MagnitudekilometersLatitudeLongitude April 14, 2016 21:26:36 (UTC+09) Magnitude 6.2 April 16, 2016 01:25:06 (UTC+09) Magnitude 7.0 32.849oN 130.635oE Depth 10 kilometers 32.782oN 130.726oE Depth 10 kilometers Intensity 8.0 Apr-14 21:26 6.2 10.0 32.849 130.635 Apr-16 01:445.3 10.0 32.695 130.735 D Intensity 7.0 Apr-14 21:424.8 10.0 32.578 130.636 Apr-16 01:455.7 10.0 32.881 130.846 Intensity 8.5 Apr-14 22:075.4 10.0 32.788 130.835 Apr-16 02:044.6 11.7 32.757 130.742 Apr-14 22:224.8 10.0 32.683 130.646 Apr-16 02:494.5 12.2 33.203 131.321 M Apr-14 22:384.8 10.0 32.685 130.711 Apr-16 03:035.4 4.9 32.926 131.043 L Apr-14 22:434.5 10.0 32.704 130.696 Apr-16 03:164.6 18.6 33.086 130.836 J K B Apr-14 23:284.5 10.0 32.785 130.745 Apr-16 03:204.5 19.4 33.101 130.997 I Apr-14 23:294.6 10.0 32.752 130.726 Apr-16 03:264.5 10.0 32.870 130.918 A Aisin Kyushu Co.
Load more

Recommended publications
  • Groundwater Oxygen Isotope Anomaly Before the M6.6 Tottori Earthquake
    www.nature.com/scientificreports OPEN Groundwater oxygen isotope anomaly before the M6.6 Tottori earthquake in Southwest Japan Received: 13 December 2017 Satoki Onda1, Yuji Sano 1, Naoto Takahata 1, Takanori Kagoshima1, Toshihiro Miyajima1, Accepted: 8 March 2018 Tomo Shibata2, Daniele L. Pinti 3, Tefang Lan4, Nak Kyu Kim5, Minoru Kusakabe5 & Published: xx xx xxxx Yoshiro Nishio6 Geochemical monitoring of groundwater in seismically-active regions has been carried out since 1970s. Precursors were well documented, but often criticized for anecdotal or fragmentary signals, and for lacking a clear physico-chemical explanation for these anomalies. Here we report – as potential seismic precursor – oxygen isotopic ratio anomalies of +0.24‰ relative to the local background measured in groundwater, a few months before the Tottori earthquake (M 6.6) in Southwest Japan. Samples were deep groundwater located 5 km west of the epicenter, packed in bottles and distributed as drinking water between September 2015 and July 2017, a time frame which covers the pre- and post-event. Small but substantial increase of 0.07‰ was observed soon after the earthquake. Laboratory crushing experiments of aquifer rock aimed to simulating rock deformation under strain and tensile stresses were carried out. Measured helium degassing from the rock and 18O-shift suggest that the co-seismic oxygen anomalies are directly related to volumetric strain changes. The fndings provide a plausible physico- chemical basis to explain geochemical anomalies in water and may be useful in future earthquake prediction research. Hydro-geochemical precursors of major earthquakes have attracted the attention of researchers worldwide, because they are not entirely unexpected1,2.
    [Show full text]
  • Disaster, Recovery, & Renewal: Lessons from Japan
    DISASTER, RECOVERY, & RENEWAL: LESSONS FROM JAPAN Students will be led by Dr. Michael Strausz and Dr. Wendy Williams. Explore Japan to learn first-hand about this resilient country and how it has rebuilt and renewed itself after numerous devastating natural and human-made disasters. Japan has faced a number of major disasters in the last 75 years, including earthquakes, tsunamis, the firebombing and nuclear bombing of its cities, and a nuclear meltdown. How has Japan recovered and renewed itself after these disasters, and, more broadly, what does “renewal” mean in the Japanese context? We will consider these questions as we visit sites in Japan including Kumamoto, Hiroshima, WHEN: Kyoto, Tokyo, and the Asian Rural Institute in Tochigi Prefecture. At the Asian Rural Institute, we will learn about Su M Tu W Th F Sa leadership in the global community from the institute’s 15 16 17 18 director, 2019 TCU Global Innovator, Tomoko Arakawa. In Tokyo, we will partner with a group of students from Meiji MAY 19 20 21 22 23 24 25 University to explore this vibrant city and learn about issues of recovery and renewal in Japan. Please join us on what 26 27 28 29 30 31 1 promises to be an amazing educational opportunity! TOKYO (5/15 -5/16 & 5/24-5/29) Tokyo is the capital of Japan. With 39 million residents, it is the most populous metropolitan area in the world. This bustling, high-energy city is beautiful, friendly, clean, and safe. KYOTO (5/20-5/21) Kyoto is the cultural and spiritual capital of Japan with many captivating temples and shrines.
    [Show full text]
  • Ffe
    JP9950127 ®n m&?. mti HBA\ /j^¥ m** f «ffe#«i^p^fe«j:y f^± (top-soii) frbzarm (sub-son) '\<Dm$tm*wfeLtz0 i37 ,37 ®mmm(nmij\c£^ffi'Pi-& cs(DfrMim%¥mmmm7^mT\ ££>c cs<z)fe , i3, !^«££1ffiIELfc&JK0*£«fc^«'> tS Cs<Dn<Dffi8¥tmffil*4l~-42Spk%-3tz0 ffi^f.^CTi'N© 137Cs©*»4^iMf^±fc*)1.6~1.7%/^-C&o^o £fc* 1996^K t3, &\fZ Cs<Dft±£*<DTm<D%ttm&*mfeLfcm%\*¥ftX-6:4t1i-it:0 Residence half-time of 137Cs in the top-soils of Japanese paddy and upland fields Misako KOMAMURA, Akito TSUMURA*. Kiyoshi K0DA1RA** National Institute of Agro-Environmental Sciences, *ex-National Institute of Agro-Environmental Sciences, **Prof. Em. Ashikaga Institute of Technology A series of top-soil samples of 14 paddy fields and 10 upland fields in Japan, were annually collected during more than 30 years, to be examined in the contents of ,37Cs. The data, which were obtained by the use of a gamma spectrometric system, received some statistical treatments to distinguish the annual decline of 137Cs contents from deviations. Then the authors calculated "residence half-time of137Cs" within top-soil, and "eluviation rate of 137Cs" from top to the sub-layer of the soil. The following nationwide results were obtained irrespective of paddy or upland fields: (1) The "apparent residence half-time" was estimated as 16—-17 years. This one consists of both effects of eluviation and nuclear disintegration. (2) The "true residence half-time" was reported as 41~~42 years. This one depends on the eluviation speed of 137Cs exclusively, because the influence of nuclear disinte• gration has been compensated.
    [Show full text]
  • China Russia
    1 1 1 1 Acheng 3 Lesozavodsk 3 4 4 0 Didao Jixi 5 0 5 Shuangcheng Shangzhi Link? ou ? ? ? ? Hengshan ? 5 SEA OF 5 4 4 Yushu Wuchang OKHOTSK Dehui Mudanjiang Shulan Dalnegorsk Nongan Hailin Jiutai Jishu CHINA Kavalerovo Jilin Jiaohe Changchun RUSSIA Dunhua Uglekamensk HOKKAIDOO Panshi Huadian Tumen Partizansk Sapporo Hunchun Vladivostok Liaoyuan Chaoyang Longjing Yanji Nahodka Meihekou Helong Hunjiang Najin Badaojiang Tong Hua Hyesan Kanggye Aomori Kimchaek AOMORI ? ? 0 AKITA 0 4 DEMOCRATIC PEOPLE'S 4 REPUBLIC OF KOREA Akita Morioka IWATE SEA O F Pyongyang GULF OF KOREA JAPAN Nampo YAMAJGATAA PAN Yamagata MIYAGI Sendai Haeju Niigata Euijeongbu Chuncheon Bucheon Seoul NIIGATA Weonju Incheon Anyang ISIKAWA ChechonREPUBLIC OF HUKUSIMA Suweon KOREA TOTIGI Cheonan Chungju Toyama Cheongju Kanazawa GUNMA IBARAKI TOYAMA PACIFIC OCEAN Nagano Mito Andong Maebashi Daejeon Fukui NAGANO Kunsan Daegu Pohang HUKUI SAITAMA Taegu YAMANASI TOOKYOO YELLOW Ulsan Tottori GIFU Tokyo Matsue Gifu Kofu Chiba SEA TOTTORI Kawasaki KANAGAWA Kwangju Masan KYOOTO Yokohama Pusan SIMANE Nagoya KANAGAWA TIBA ? HYOOGO Kyoto SIGA SIZUOKA ? 5 Suncheon Chinhae 5 3 Otsu AITI 3 OKAYAMA Kobe Nara Shizuoka Yeosu HIROSIMA Okayama Tsu KAGAWA HYOOGO Hiroshima OOSAKA Osaka MIE YAMAGUTI OOSAKA Yamaguchi Takamatsu WAKAYAMA NARA JAPAN Tokushima Wakayama TOKUSIMA Matsuyama National Capital Fukuoka HUKUOKA WAKAYAMA Jeju EHIME Provincial Capital Cheju Oita Kochi SAGA KOOTI City, town EAST CHINA Saga OOITA Major Airport SEA NAGASAKI Kumamoto Roads Nagasaki KUMAMOTO Railroad Lake MIYAZAKI River, lake JAPAN KAGOSIMA Miyazaki International Boundary Provincial Boundary Kagoshima 0 12.5 25 50 75 100 Kilometers Miles 0 10 20 40 60 80 ? ? ? ? 0 5 0 5 3 3 4 4 1 1 1 1 The boundaries and names show n and t he designations us ed on this map do not imply of ficial endors ement or acceptance by the United N at ions.
    [Show full text]
  • CORPORATE DIRECTORY (As of June 28, 2000)
    CORPORATE DIRECTORY (as of June 28, 2000) JAPAN TOKYO ELECTRON KYUSHU LIMITED TOKYO ELECTRON FE LIMITED Saga Plant 30-7 Sumiyoshi-cho 2-chome TOKYO ELECTRON LIMITED 1375-41 Nishi-Shinmachi Fuchu City, Tokyo 183-8705 World Headquarters Tosu City, Saga 841-0074 Tel: 042-333-8411 TBS Broadcast Center Tel: 0942-81-1800 District Offices 3-6 Akasaka 5-chome, Minato-ku, Tokyo 107-8481 Kumamoto Plant Osaka, Kumamoto, Iwate, Tsuruoka, Sendai, Tel: 03-5561-7000 2655 Tsukure, Kikuyo-machi Aizuwakamatsu, Takasaki, Mito, Nirasaki, Toyama, Fax: 03-5561-7400 Kikuchi-gun, Kumamoto 869-1197 Kuwana, Fukuyama, Higashi-Hiroshima, Saijo, Oita, URL: http://www.tel.co.jp/tel-e/ Tel: 096-292-3111 Nagasaki, Kikuyo, Kagoshima Regional Offices Ozu Plant Fuchu Technology Center, Osaka Branch Office, 272-4 Takaono, Ozu-machi TOKYO ELECTRON DEVICE LIMITED Kyushu Branch Office, Tohoku Regional Office, Kikuchi-gun, Kumamoto 869-1232 1 Higashikata-cho, Tsuzuki-ku Yamanashi Regional Office, Central Research Tel: 096-292-1600 Yokohama City, Kanagawa 224-0045 Laboratory/Process Technology Center Koshi Plant Tel: 045-474-7000 Sales Offices 1-1 Fukuhara, Koshi-machi Sales Offices Sendai, Nagoya Kikuchi-gun, Kumamoto 861-1116 Utsunomiya, Mito, Kumagaya, Kanda, Tachikawa, Tel: 096-349-5500 Yamanashi, Matsumoto, Nagoya, Osaka, Fukuoka TOKYO ELECTRON TOHOKU LIMITED Tohoku Plant TOKYO ELECTRON MIYAGI LIMITED TOKYO ELECTRON LEASING CO., LTD. 52 Matsunagane, Iwayado 1-1 Nekohazama, Nemawari, Matsushima-machi 30-7 Sumiyoshi-cho 2-chome Esashi City, Iwate 023-1101 Miyagi-gun, Miyagi
    [Show full text]
  • Teradyne K.K. Teradyne Inc
    Success StoriesーOther Manufacturing Teradyne K.K. Teradyne Inc. was founded in 1960 in the student quarter of Boston, Massachusetts to provide Automated Test Equipment (ATE) for electronic parts to the world. The company now boasts the largest sales in the global ATE market for semiconductors (based on its own research). Its only non-US research and development site of ATE for semiconductor is in Kumamoto Prefecture. Even after the 2016 Kumamoto earthquakes, the company was determined to continue business there, where there are many experienced and competent engineers and, with talented professionals, rebuilt the local factory. We talked to Hiroshi Takashima, Representative Director & President of Teradyne K.K. and Yuzo Motomura, Manager of the Kumamoto site. Mobile phones and smartphones are essential development and manufacturing. There has tools in our daily lives today. According to Mr. already been an increase in inquiries from Takashima, “Sixty to seventy percent of the Japanese companies showing interest in their semiconductors used for those products hit the cobots, as the issue of manpower shortage market after being tested with Teradyne testers.” continues to grow more severe in Japan. With about 4,700 employees in 32 locations worldwide and sales of about 235 billion yen Development and manufacturing in (2,137 million dollar) in 2017, the company is Kumamoto, a Japanese semiconductor leading the semiconductor ATE market. industry center where clients who boast According to the company, about 80% of the the world’s top market share operate global market (as per sales forecasts) is led by Teradyne K.K. started business in Japan as two companies: Teradyne (50%) and the early as 1973 and celebrates the 45th Japanese company Advantest (33%).
    [Show full text]
  • Resilient Water Supply and Sanitation Services
    RESILIENT WATER SUPPLY AND SANITATION SERVICES AND SANITATION SUPPLY WATER RESILIENT THE CASE OF JAPAN RESILIENT WATER SUPPLY AND SANITATION SERVICES THE CASE OF JAPAN ©2018 The World Bank International Bank for Reconstruction and Development The World Bank Group 1818 H Street NW, Washington, DC 20433 USA February 2018 DISCLAIMER This work is a product of the staff of The World Bank with external contributions. The findings, interpretations, and conclusions expressed in this work do not necessarily reflect the views of The World Bank, its Board of Executive Directors, or the governments they represent. The World Bank does not guarantee the accuracy of the data included in this work. The boundaries, colors, denominations, and other information shown on any map in this work do not imply any judgment on the part of The World Bank concerning the legal status of any territory or the endorsement or acceptance of such boundaries. Nothing herein shall constitute or be considered to be a limitation upon or waiver of the privileges and immunities of The World Bank, all of which are specifically reserved. The report reflects information available up to November 30, 2017. RIGHTS AND PERMISSIONS The material in this work is subject to copyright. Because The World Bank encourages dissemination of its knowledge, this work may be reproduced, in whole or in part, for noncommercial purposes as long as full attribution to this work is given. Any queries on rights and licenses, including subsidiary rights, should be addressed to World Bank Publications, The World Bank Group, 1818 H Street NW, Washington, DC 20433, USA; e-mail: [email protected].
    [Show full text]
  • From Fukuoka Airport to Kumamoto If You Arrive at Fukuoka Airport, There Are 2 Ways to Access to Kumamoto. 1. Highway Bus Line B
    From Fukuoka Airport to Kumamoto If you arrive at Fukuoka Airport, there are 2 ways to access to Kumamoto. 1. Highway bus line between Fukuoka Airport ⇔ Kumamoto Hinokuni-go – Fukuoka Airport Take an expressway bus to Kumamoto and get off at Torichosuji or Bus terminal. It takes about 2 hours. Kumamoto Fukuoka Airport: 2,280 JPY/Person *One-way ticket 2280 JPY *Round-trip ticket 4100 JPY Reference: https://kyushubusbooking.com/highway-bus/hinokuni-go/ 2. Take Shinkansen (bulletin train) from Hakata Station to Kumamoto. There is a subway between Fukuoka Airport and Hakata St. (https://www.fukuoka-airport.jp/english/subway.html#out ) Hakata Station ⇔ Kumamoto Station *One-way ticket 5,330 JPY *Round-trip 7,460 JPY Reference: https://www.jrkyushu.co.jp/english/ From ASO KUMAMOTO AIRPORT to Kumamoto city If you arrive at Kumamoto Airport, take a limousine bus to downtown and get off at Torichosuji or Bus terminal. It takes about 40 minutes. *One-way ticket 700 JPY Reference: https://kyushubusbooking.com/airport-limousine/ Access to Kumamoto University https://ewww.kumamoto-u.ac.jp/en/about/access/access_map/ Please check our university web site for the map. How to access from downtown to South Campus, Kumamoto University This is the Bus number Bus stop: Kumamoto Daigaku Mae（熊本大学前） If you take a bus from downtown to Kumamoto University, 1. Check and find the bus number with E1-3~4, E2-0~3, and E3-1 ~ 5. Only the buses with these numbers will take you to South Campus, Kumamoto University. 2. Get on the bus from the rear door and take a numbered ticket.
    [Show full text]
  • Impact of Additional Chromosomal Abnormalities in Patients with Acute Promyelocytic Leukemia - 10 Years' Results of the Japan Adult Leukemia Study Group APL97 Study"
    Manuscript no. HAEMATOL /2010/030205 entitled “Impact of additional chromosomal abnormalities in patients with acute promyelocytic leukemia - 10 years' results of the Japan Adult Leukemia Study Group APL97 study" Authors: Takaaki Ono, Akihiro Takeshita, Masako Iwanaga, Norio Asou, Tomoki Naoe, Ryuzo Ohno Information about the contributions of each person named as having participated in the study 1) Guarantor(s), i.e., person(s) who is (are) responsible for the integrity of the work as a whole: • Takaaki Ono, Department of Internal Medicine III, Hamamatsu University School of Medicine, Hamamatsu, Japan. Email: [email protected] • Akihiro Takeshita, Department of Internal Medicine III, Hamamatsu University School of Medicine, Hamamatsu, Japan. Email: [email protected] • Masako Iwanaga, Department of Molecular Medicine, Atomic Bomb Disease Institute, Nagasaki University Graduate School of Biomedical Sciences, Nagasaki, Japan. Email: [email protected] • Norio Asou, Department of Hematology, Kumamoto University School of Medicine, Kumamoto, Japan. Email: [email protected] • Tomoki Naoe, Department of Hematology/Oncology, Nagoya University Graduate School of Medicine, Nagoya, Japan. Email: [email protected] • Ryuzo Ohno, Aichi Cancer Center, Nagoya, Japan. Email: [email protected] According to the International Committee of Medical Journal Editors (ICMJE) (http://www.icmje.org/ethical_1author.html): “Authorship credit should be based on: 1) substantial contributions to conception and design, acquisition of data, or analysis and interpretation of data; 2) drafting the article or revising it critically for important intellectual content; and 3) final approval of the version to be published. Authors should meet conditions 1, 2, and 3 …………………….
    [Show full text]
  • Justice and Humanity JCG - Keeping the Oceans Safe and Enjoyable for Future Generations! 120°E 130°E 140°E 150°E 160°E 170°E
    Justice and Humanity JCG - Keeping the oceans safe and enjoyable for future generations! 120°E 130°E 140°E 150°E 160°E 170°E Territorial sea 165° East Approx. 430,000 km2 (Including inland waters) 5 0 °N Territorial sea + EEZ Approx. 4,470,000 km2 (Japan’s Land area x 12) Etorofu Island Land area Japan Sea 2 Approx. 380,000 km 4 0 °N Takeshima Pacific Ocean Exclusive Economic Zone (EEZ) 2 East China Sea Approx. 4,050,000 km 3 0 °N Senkaku Islands Ogasawara Islands Io To Island Yonagunijima Island Minami-Tori Shima Island 2 0 °N Oki-no-Tori Shima Island 17° North Extended continental shelves* Japan's search responsibility area Approx. 180,000 km2 under the U.S.-Japan SAR Agreement * Areas of the sea as defined in Article 2 (2) of the Exclusive Economic Zone and Continental Shelf Act. For illustration purposes, this map also shows geographical intermediate lines in waters in which borders with neighboring countries have yet to be demarcated. Despite ranking only 61st in the world in terms of land area (380,000 km2), Japan’s territorial waters and exclusive economic zone combined are 12 times larger (4,470,000 km2) than its land area. In December 1986, the Agreement between the Government of the United States of America and the Government of Japan on Maritime Search and Rescue (U.S.-Japan SAR Agreement) was concluded, under which Japan is responsible for coordinating search and rescue activities in the vast expanse of ocean that extends northward from 17° North and westward from 165° East.
    [Show full text]
  • Distributions of a Halophilous and a Riparian Species of Harvestmen Along Sendai River, Tottori City, with the First Records of Harvestmen in Tottori Sand Dunes
    Acta Arachnologica, 69 (2): 95–103, December 20, 2020 Distributions of a halophilous and a riparian species of harvestmen along Sendai River, Tottori City, with the first records of harvestmen in Tottori Sand Dunes Nobuo Tsurusaki1, 2*, Minako Kawaguchi2,3, Yamato Funakura2,4, Toru Matsumoto2,5 & Yuito Obae6 1 Laboratory of Animal Taxonomy, Faculty of Agriculture, Tottori University, Tottori 680-8551, Japan 2Department of Regional Environment, Faculty of Regional Sciences, Tottori University, Tottori 680-8551, Japan and 6Faculty of Environmental Studies, Tottori University of Environmental Studies, Wakabadai-kita 1-1-1, 689-1111, Japan E-mail: [email protected], *Corresponding author Abstract ― Distributions of a maritime harvestman, Psathyropus tenuipes and a riparian harvestman Paraum- bogrella pumilio were investigated along the Sendai River, Tottori City, Honshu, Japan. Psathyropus tenuipes was found from the mouth of the river to the site 4 km upstream where slight salinity (0.1 PPT) was detected in the river. On the other hand, no specimens were found from the upstream sites where no salinity was detect- ed. This indicates that the species needs at least a slight salinity for its occurrence. Paraumbogrella pumilio was found at five sites from the dry riverbed near the Shobu floodgate to a site on the right bank of Sendai River just upstream of Yachiyo Bridge. Occurrence of this species seems to be related to presence of open ground covered with lower grasses on the banks. Recently, the both species were also found from the right bank of the river mouth of Sendai River that is also a part of Tottori Sand Dunes.
    [Show full text]
  • By Municipality) (As of March 31, 2020)
    The fiber optic broadband service coverage rate in Japan as of March 2020 (by municipality) (As of March 31, 2020) Municipal Coverage rate of fiber optic Prefecture Municipality broadband service code for households (%) 11011 Hokkaido Chuo Ward, Sapporo City 100.00 11029 Hokkaido Kita Ward, Sapporo City 100.00 11037 Hokkaido Higashi Ward, Sapporo City 100.00 11045 Hokkaido Shiraishi Ward, Sapporo City 100.00 11053 Hokkaido Toyohira Ward, Sapporo City 100.00 11061 Hokkaido Minami Ward, Sapporo City 99.94 11070 Hokkaido Nishi Ward, Sapporo City 100.00 11088 Hokkaido Atsubetsu Ward, Sapporo City 100.00 11096 Hokkaido Teine Ward, Sapporo City 100.00 11100 Hokkaido Kiyota Ward, Sapporo City 100.00 12025 Hokkaido Hakodate City 99.62 12033 Hokkaido Otaru City 100.00 12041 Hokkaido Asahikawa City 99.96 12050 Hokkaido Muroran City 100.00 12068 Hokkaido Kushiro City 99.31 12076 Hokkaido Obihiro City 99.47 12084 Hokkaido Kitami City 98.84 12092 Hokkaido Yubari City 90.24 12106 Hokkaido Iwamizawa City 93.24 12114 Hokkaido Abashiri City 97.29 12122 Hokkaido Rumoi City 97.57 12131 Hokkaido Tomakomai City 100.00 12149 Hokkaido Wakkanai City 99.99 12157 Hokkaido Bibai City 97.86 12165 Hokkaido Ashibetsu City 91.41 12173 Hokkaido Ebetsu City 100.00 12181 Hokkaido Akabira City 97.97 12190 Hokkaido Monbetsu City 94.60 12203 Hokkaido Shibetsu City 90.22 12211 Hokkaido Nayoro City 95.76 12220 Hokkaido Mikasa City 97.08 12238 Hokkaido Nemuro City 100.00 12246 Hokkaido Chitose City 99.32 12254 Hokkaido Takikawa City 100.00 12262 Hokkaido Sunagawa City 99.13
    [Show full text]