Proposed Loan-People's Republic of China: Emergency Assistance For
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World Bank Document
CONFORMED COPY Public Disclosure Authorized LOAN NUMBER 7616-CN Loan Agreement Public Disclosure Authorized (Wenchuan Earthquake Recovery Project) between PEOPLE’S REPUBLIC OF CHINA Public Disclosure Authorized and INTERNATIONAL BANK FOR RECONSTRUCTION AND DEVELOPMENT Dated March 20, 2009 Public Disclosure Authorized LOAN AGREEMENT AGREEMENT dated March 20, 2009, between PEOPLE’S REPUBLIC OF CHINA (“Borrower”) and INTERNATIONAL BANK FOR RECONSTRUCTION AND DEVELOPMENT (“Bank”). The Borrower and the Bank hereby agree as follows: ARTICLE I – GENERAL CONDITIONS; DEFINITIONS 1.01. The General Conditions (as defined in the Appendix to this Agreement) constitute an integral part of this Agreement. 1.02. Unless the context requires otherwise, the capitalized terms used in the Loan Agreement have the meanings ascribed to them in the General Conditions or in the Appendix to this Agreement. ARTICLE II – LOAN 2.01. The Bank agrees to lend to the Borrower, on the terms and conditions set forth or referred to in this Agreement, an amount equal to seven hundred ten million Dollars ($710,000,000), as such amount may be converted from time to time through a Currency Conversion in accordance with the provisions of Section 2.07 of this Agreement (“Loan”), to assist in financing the project described in Schedule 1 to this Agreement (“Project”). 2.02. The Borrower may withdraw the proceeds of the Loan in accordance with Section IV of Schedule 2 to this Agreement. 2.03. The Front-end Fee payable by the Borrower shall be equal to one quarter of one percent (0.25%) of the Loan amount. The Borrower shall pay the Front-end Fee not later than sixty (60) days after the Effective Date. -
M6.9 Southern Qinghai, China Earthquake of 13 April 2010 Network
U.S. DEPARTMENT OF THE INTERIOR EARTHQUAKE SUMMARY MAP XXX U.S. GEOLOGICAL SURVEY Prepared in cooperation with the Global Seismographic M6.9 Southern Qinghai, China Earthquake of 13 April 2010 Network Epicentral Region L. B Tectonic Setting alka 90° 92° 94° 96° 98° 100° 102° 104° 106° 70° sh 80° 90° 100° 110° 120° M O N G O L I A GOLMUD Shymkent Changchun Jilin Xinjiang Minhe Dzhambul Almaty 36° QABQA 2001 Urumqi LANZHOU Tashkent Bishkek 36° NamanganK ATE Fushun Y R T i a PL Gulistan G Y n S h a n MUR Kanggye Southern Qinghai Ningxia Z S T A 40° Andizhan A N Shenyang Osh Hamhung K U N L U N Fergana 40° F A U L T Anshan Sinuiju 13 April 2010 23:49:37 UTC Pingliang T Linxia A J Kashi T H Jingning I K I Huhot P'yongyang O R ZIKETAN Neiguanying S T N E A A N Baotou Beijing O R Dalian K 1937 Lintao 33.271° N., 96.629° E. Kulob Tangshan Maying Lung- EUR Kaesong Kagang Depth 10 km AS EXPLANATION shan- IA P H LA l t Tianjin U T Mw = 6.9 (USGS) TE a u Inch`on S O A chen h F R E Ta g Shijiazhuang K O Longxi y n Yinchuan Taiyuan Mag ≥ 7.0 Hezuo K A l t E Felt across the mountaiQnionuasn area in western China, over 400 u AT e PL killed, tens of thousands displaced. n H SIA Gangu RA j Eg U W 0 - 69 km u s n O i n a L TIANSHUI n t a Xining u L H u n Y E Gansu Rawalpindi M o K u n H A l u n F S E 70 - 299 Min Xian Tianshui Islamabad a u l t Lanzhou DAWU I Luoyang Zhengzhou 34° Li Xian M Xi'an 300 - 600 Qinghai Amritsar A C H I N A Tewo 34° Faisalabad TIBETAN PLATEAU Nanjing Volcanoes Lahore g Shanghai Hui-Xian Simla L Hefei in 30° Chandigarh a J A g -
SMIP13 Seminar Proceedings OBSERVATIONS from the APRIL 20, 2013 LUSHAN COUNTY, YA'an CITY, SICHUAN PROVINCE, CHINA EARTHQUAKE
SMIP13 Seminar Proceedings OBSERVATIONS FROM THE APRIL 20, 2013 LUSHAN COUNTY, YA’AN CITY, SICHUAN PROVINCE, CHINA EARTHQUAKE Marshall Lew AMEC Environment & Infrastructure, Inc. Los Angeles, California Abstract The April 20, 2013 Lushan earthquake followed the 2008 Great Wenchuan earthquake by almost five years. Although the rupture also started in the Longmenshan fault zone, the Lushan earthquake is not an aftershock. Although similar damage and disruptions to infrastructure and society occurred, it was of a smaller scale and not unexpected due to the short time for the lessons from Wenchuan to be applied. There were some examples of lessons learned and the strong motion dataset obtained in this event will prove valuable in assessing how effective the actions taken have been. The visual observations were made on May 27 and 28, 2013 in Lushan. Introduction On April 20, 2013, at 8:02 am (Beijing Time), an earthquake occurred in Lushan County of Ya’an City in Sichuan Province in southwestern China. The epicenter was located at 30o 17’ 02” N and 102o 57’ 22” E, about 120 km from the major city of Chengdu; see Figure 1. Ya’an City is a prefecture level city in the western part of Sichuan Province and has a population of about 1.5 million people and is the location of one of China’s main centers for the protection of the endangered giant panda. Sichuan Province is known as the “Province of Abundance.” The province is a leading agricultural region of China and the province is also very rich in mineral resources, including large natural gas reserves. -
Mammalia: Chiroptera: Rhinolophidae
Morphometric Variation in the Pusillus Group of the Genus Rhinolophus (Mammalia: Chiroptera: Rhinolophidae) in East Asia Author(s) :Yi Wu, Masaharu Motokawa, Masashi Harada, Vu Dinh Thong, Liang-Kong Lin and Yu- Chun Li Source: Zoological Science, 29(6):396-402. 2012. Published By: Zoological Society of Japan DOI: http://dx.doi.org/10.2108/zsj.29.396 URL: http://www.bioone.org/doi/full/10.2108/zsj.29.396 BioOne (www.bioone.org) is a nonprofit, online aggregation of core research in the biological, ecological, and environmental sciences. BioOne provides a sustainable online platform for over 170 journals and books published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Web site, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/page/terms_of_use. Usage of BioOne content is strictly limited to personal, educational, and non-commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. ZOOLOGICAL SCIENCE 29: 396–402 (2012) ¤ 2012 Zoological Society of Japan Morphometric Variation in the pusillus Group of the Genus Rhinolophus (Mammalia: Chiroptera: Rhinolophidae) in East Asia Yi Wu1, -
World Bank Document
INTEGRATED SAFEGUARDS DATA SHEET CONCEPT STAGE Report No.: AC3902 Public Disclosure Authorized Date ISDS Prepared/Updated: 10/30/2008 I. BASIC INFORMATION A. Basic Project Data Country: China Project ID: P114107 Project Name: Wenchuan Earthquake Recovery Task Team Leader: Mara K. Warwick Estimated Appraisal Date: November 13, Estimated Board Date: December 16, 2008 2008 Managing Unit: EASCS Lending Instrument: Emergency Recovery Public Disclosure Authorized Loan Sector: General water, sanitation and flood protection sector (44%);Roads and highways (39%);Health (13%);General education sector (4%) Theme: Natural disaster management (P);Pollution management and environmental health (S);Access to urban services and housing (S) IBRD Amount (US$m.): 710.00 IDA Amount (US$m.): 0.00 GEF Amount (US$m.): 0.00 PCF Amount (US$m.): 0.00 Other financing amounts by source: Borrower 30.00 30.00 Public Disclosure Authorized B. Project Objectives [from section 2 of PCN] To restore essential infrastructure, health, and education services to at least pre-earthquake levels and reduce vulnerability to seismic and flood hazards in project areas. C. Project Description [from section 3 of PCN] The proposed emergency recovery loan (ERL) will span Sichuan and Gansu provinces and will be processed using a programmatic approach, which will include the following key areas: (a) identification, selection, and appraisal of individual investment projects, including technical standards; (b) safeguards; (c) procurement; (d) financial management; and (e) monitoring and evaluation. During preparation, frameworks will be developed to guide the selection, appraisal and implementation of the individual investments during project implementation. Public Disclosure Authorized The components of the ERL cover three main sectors: infrastructure, health and education. -
3 Year on Sichuan Earthquake Response
3 Year On Sichuan Earthquake Response Executive Summary: Introduction On 20th April 2013, a 7.0-magnitude earthquake struck Lushan County of Ya’an City in Sichuan province at 8:02 am local time (GMT +8). In the epicenter, most houses were either damaged or collapsed; public services were suspended, while water and electricity supply were cut. The disaster was declared as a CAT III, National Office Response. Immediate emergency response was carried out after the quake in Lushan, Baoxing and Tianquan. World Vision moved into rehabilitation phase since 2014, and extended its coverage to Hongya and Jiajiang Counties. In third year of response, World Vision continued our recovery work in Baoxing and Jiajiang Counties. Disaster Impact Quick Facts Death 196 Collapsed house Rural: 20,000 Injury >13,000 rooms Urban: 9,500 Affected population >2,000,000 Direct economic RMB 4.40 billion Displaced population 233,191 loss in Ya’an Relief Reponses and Rehabilitation In the emergency response phase, WV China met the immediate needs of quake-affected communities by responding to the following sectors of needs: Non-Food-Items (NFIs), Water, Sanitation and Hygiene (WASH), Protection, and Education. In rehabilitation phase, WV China has addressed the following sectors of need: Shelter, Education, Infrastructure, Disaster Risk Reduction (DRR) and Livelihood. In total, WV China has reached over 230,000 beneficiary times. Beneficiary Sector Activities times NFI Family Kits, quilts, beds & mattresses >17,500 WASH Hygiene Kits, drinking water facility, irrigation -
Challenges and Countermeasures of Tourism
International Conference on Social Science and Technology Education (ICSSTE 2015) Challenges and Countermeasures of Regional Tourism Cooperation Development Strategy of Sichuan-Shanxi-Gansu Golden Triangle Area,Western China Qin Jianxiong1 Zhang Minmin1 1 College of tourism and historic culture, Southwest University For Natianalities, Chengdu, 610041 Abstract visitors can explore in this line up and down five SSGGTA triangle of three provinces , dependent thousand years of culture, enjoy the mystery of Qinba [1] landscape, folk customs are similar, for the first time landscape . These tourism resources in Chongqing, since the 2002 held in Bazhong of SSGGTA triangle area Chengdu, Xi'an, Lanzhou, Wuhan five source among SSGGTA triangle tourism cooperation zone is composed tourism cooperation will be signed in SSGGTA triangle of Sichuan Bazhong, Guangyuan, Dazhou and Shanxi tourism, build "Golden Triangle" cooperation agreement, Hanzhoung, Ankang three provinces and five to 2005 has successively held 3 annual meeting. The goal municipalities, carry out cooperation in the past 3 years, of cooperation is through the sincere cooperation of the three provinces and five municipalities in the propaganda, three provinces, the formation of regional tourism build mutual interaction, line group, strategic planning collaboration regular contact system, the characteristics of consensus interaction and so on has made significant tourism products, the formation of regional joint progress, regional cooperation has been fully affirmed the promotion,a barrier free Tourism Zone, to realize the two provincial government and support. Sichuan North Sichuan area has been the focus of tourism development sustainable development of Shanxi tourism in Golden in the province, tourism development, Shanxi will also Triangle. -
Sichuan Q I N G H a I G a N S U Christian Percentage of County/City Ruo'ergai
Sichuan Q i n g h a i G a n s u Christian Percentage of County/City Ruo'ergai Shiqu Jiuzhaigou S h a a n x i Hongyuan Aba Songpan Chaotian Qingchuan Nanjiang Seda Pingwu Lizhou Rangtang Wangcang Dege Heishui Zhaohua Tongjiang Ma'erkang Ganzi Beichuan Jiangyou Cangxi Wanyuan Mao Jiange Bazhou Enyang Zitong Pingchang Luhuo Jinchuan Li Anzhou Youxian Langzhong Xuanhan Mianzhu Yilong Shifang Fucheng Tongchuan Baiyu Luojiang Nanbu Pengzhou Yangting Xiaojin Jingyang Santai Yingshan Dachuan Danba Dujiangyan Xichong Xinlong Wenchuan Guanghan Peng'an Kaijiang Daofu Shehong Shunqing Qu Pi Xindu Zhongjiang Gaoping Chongzhou Jialing DayiWenjiang Jintang Pengxi Guang'an Dazhu Lushan Daying Yuechi Qianfeng Shuangliu Chuanshan Baoxing Qionglai Huaying T i b e t Batang Xinjin Jianyang Anju Wusheng Pujiang Kangding Pengshan Lezhi Linshui Mingshan Yanjiang Tianquan DanlengDongpo H u b e i Litang Yajiang Yucheng Renshou Anyue Yingjing Qingshen Zizhong Luding Jiajiang Jingyan Hongya Shizhong Weiyuan Dongxing Hanyuan Emeishan Rong Shizhong WutongqiaoGongjing Da'an Longchang C h o n g q i n g Xiangcheng Shimian Jinkouhe Shawan Ziliujing Yantan Ebian Qianwei Lu Jiulong Muchuan Fushun Daocheng Ganluo Longmatan Derong Xuzhou NanxiJiangyang Mabian Pingshan Cuiping Hejiang Percent Christian Naxi Mianning Yuexi Jiang'an Meigu Changning (County/City) Muli Leibo Gao Gong Xide Xingwen 0.8% - 3% Zhaojue Junlian Xuyong Gulin Chengdu area enlarged 3.1% - 4% Xichang Jinyang Qingbaijiang Yanyuan Butuo Pi Puge Xindu 4.1% - 5% Dechang Wenjiang Y u n n a n Jinniu Chenghua Qingyang 5.1% - 6% Yanbian Ningnan Miyi G u i z h o u Wuhou Longquanyi 6.1% - 8.8% Renhe Jinjiang Xi Dong Huidong Shuangliu Renhe Huili Disputed boundary with India Data from Asia Harvest, www.asiaharvest.org. -
Since the Reform and Opening Up1 1
Int. Statistical Inst.: Proc. 58th World Statistical Congress, 2011, Dublin (Session CPS020) p.6378 Research of Acceleration Urbanization Impacts on Resources and Environment in Sichuan Province Caimo,Teng National Bureau of Statistics of China, Survey Organizations of Sichuan No.31, the East Route, Qingjiang Road Chengdu, China, 610072 E-mail: [email protected] Since the reform and opening up, the rapid development of economic society and the rise ceaselessly of urbanization in Sichuan play an important role for material civilization and spiritual civilization, but also bring influence for resources and environment, this paper give an in-depth analysis about this. Ⅰ. The Main Characteristics of the Urbanization Development in Sichuan The reflection of urbanization in essence is from the industry cluster to population cluster., we tend to divided the process of urbanization into four stages, 1949-1978 is the first stage, 1978 – 1990 is the second stage, 1990 -2000 is the third stage, After the year of 2000 is the fourth stage. In view the particularities of the first phase, this paper researches mainly after three stages. 1. The level of the urbanization enhances unceasingly. With the reform and opening-up and the rapid development of social economy, the urbanization in Sichuan has significant achievements. The average annual growth of the level of urbanization is 0.8 percent in the twelve years of the second stage. The average annual growth in the third stage and the four stages is individually 0.5 and 1.3 percentage. The average annual growth of urbanization in the fourth stage is faster respectively 0.5 and 0.8 percent than the previous two stages which reflects obviously the rapid rise of the urbanization after the fourth stage in Sichuan. -
The Survey on the Distribution of MC Fei and Xiao Initial Groups in Chinese Dialects
IALP 2020, Kuala Lumpur, Dec 4-6, 2020 The Survey on the Distribution of MC Fei and Xiao Initial Groups in Chinese Dialects Yan Li Xiaochuan Song School of Foreign Languages, School of Foreign Languages, Shaanxi Normal University, Shaanxi Normal University Xi’an, China /Henan Agricultural University e-mail: [email protected] Xi’an/Zhengzhou, China e-mail:[email protected] Abstract — MC Fei 非 and Xiao 晓 initial group discussed in this paper includes Fei 非, Fu groups are always mixed together in the southern 敷 and Feng 奉 initials, but does not include Wei part of China. It can be divided into four sections 微, while MC Xiao 晓 initial group includes according to the distribution: the northern area, the Xiao 晓 and Xia 匣 initials. The third and fourth southwestern area, the southern area, the class of Xiao 晓 initial group have almost southeastern area. The mixing is very simple in the palatalized as [ɕ] which doesn’t mix with Fei northern area, while in Sichuan it is the most initial group. This paper mainly discusses the first extensive and complex. The southern area only and the second class of Xiao and Xia initials. The includes Hunan and Guangxi where ethnic mixing of Fei and Xiao initials is a relatively minorities gather, and the mixing is very recent phonetic change, which has no direct complicated. Ancient languages are preserved in the inheritance with the phonological system of southeastern area where there are still bilabial Qieyun. The mixing mainly occurs in the southern sounds and initial consonant [h], but the mixing is part of the mainland of China. -
The Spatial and Temporal Distribution Characteristics of Rainstorm Disaster in Sichuan Province Over the Past Decade
Journal of Geoscience and Environment Protection, 2017, 5, 1-9 http://www.scirp.org/journal/gep ISSN Online: 2327-4344 ISSN Print: 2327-4336 The Spatial and Temporal Distribution Characteristics of Rainstorm Disaster in Sichuan Province over the Past Decade Jie Gao1,2, Jianhua Pan1, Mingtian Wang1, Shanyun Guo1 1Sichuan Provincial Meteorological Observatory, Chengdu, China 2Heavy Rain and Drought-Flood Disasters in Plateau and Basin Key Laboratory of Sichuan Province, Chengdu, China How to cite this paper: Gao, J., Pan, J.H., Abstract Wang, M.T. and Guo, S.Y. (2017) The Spatial and Temporal Distribution Charac- The spatial and temporal distribution characteristics of rainstorm disaster in teristics of Rainstorm Disaster in Sichuan Sichuan Province were investigated by statistical analysis method based on Province over the Past Decade. Journal of 2002-2015 rainstorm disaster data of Sichuan Province. As shown by the re- Geoscience and Environment Protection, 5, 1-9. sults, the rainstorm disaster in Sichuan Province was distributed mainly in https://doi.org/10.4236/gep.2017.58001 four regions including Liangshan Prefecture and Sichuan Basin during 2002-2015, and the rainstorm disaster distribution had a good corresponding Received: March 29, 2017 Accepted: July 16, 2017 relationship with the rainstorm center regions; in terms of annual variation Published: July 19, 2017 trend, the variation of rainstorm disaster frequency showed a significant qua- si-2-3-year oscillation period; in terms of monthly distribution, June, July and Copyright © 2017 by authors and August saw the heaviest rainstorms; the high death toll from rainstorms was Scientific Research Publishing Inc. This work is licensed under the Creative attributed to not only routine rainfall, occurrence time and terrain feature, but Commons Attribution International also the populace’s awareness of disaster prevention and the disaster preven- License (CC BY 4.0). -
Source Rupture Process of Lushan MS7.0 Earthquake, Sichuan, China and Its Tectonic Implications
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Springer - Publisher Connector Article SPECIAL TOPIC October 2013 Vol.58 No.28-29: 34443450 Coseismic Deformation and Rupture Processes of the 2013 Lushan Earthquake doi: 10.1007/s11434-013-6017-6 Source rupture process of Lushan MS7.0 earthquake, Sichuan, China and its tectonic implications ZHAO CuiPing1*, ZHOU LianQing1 & CHEN ZhangLi2 1 Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China; 2 China Earthquake Administration, Beijing 100036, China Received June 9, 2013; accepted July 8, 2013; published online August 22, 2013 The source rupture process of the MS7.0 Lushan earthquake was here evaluated using 40 long-period P waveforms with even azimuth coverage of stations. Results reveal that the rupture process of the Lushan MS7.0 event to be simpler than that of the Wenchuan earthquake and also showed significant differences between the two rupture processes. The whole rupture process 19 lasted 36 s and most of the moment was released within the first 13 s. The total released moment is 1.9×10 N m with MW=6.8. Rupture propagated upwards and bilaterally to both sides from the initial point, resulting in a large slip region of 40 km×30 km, with the maximum slip of 1.8 m, located above the initial point. No surface displacement was estimated around the epicenter, but displacement was observed about 20 km NE and SW directions of the epicenter. Both showed slips of less than 40 cm. The rup- ture suddenly stopped at 20 km NE of the initial point.