China Shaping Tibet for Strategic Leverage
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Damage Mapping of April 2015 Nepal Earthquake Using Small
J-Rapid Final Workshop 21 June, 2016, Kathmandu Inventory mapping of landslides induced by the Gorkha earthquake 2015 and a proposal for hazard mapping of future landslides for making a plan of better reconstruction "Impact on infrastructure by Gorkha earthquake 2015 induced landslides" Masahiro CHIGIRA Masahiro CHIGIRA Professor, Disaster Prevention Research Institute, Professor, Disaster Prevention Research Institute, Kyoto University Kyoto University Vishnu DANGOL Vishnu DANGOL Professor, Department of Geology, Professor, Department of Geology, Tribhuvan University Tribhuvan University Objective 1. to make an inventory mapping on landslides, cracks, and landslide dams induced by the Nepal earthquake and to investigate their formative mechanisms 2. to detect displaced areas of slope surfaces, of which future susceptibility to landslides would be evaluated on the basis of geology, geomorphology, and groundwater conditions. 3. propose a methodology of hazard mapping for earthquake-induced landslides in Nepal. Members (Japan side) 1. Masahiro CHIGIRA (Kyoto Univ.) PI Applied Geology 2. Daisuke HIGAKI (Hirosaki Univ.) Landslide control 3. Hiroshi YAGI (Yamagata Univ.) Landslide susceptibility mapping 4. Akihiko WAKAI (Gunma Univ.) Geotechnical analysis of landslide 5. Hiroshi, P. SATO (Nihon Univ.) Remote sensing 6. Go, SATO (Teikyo Heisei Univ.) Geomorphology 7. Ching-Ying, TSOU (Hirosaki Univ.) GIS analysis 8. Akiyo YATAGAI (Res. Inst. Humanity and Nature) Meteorology Members (Nepali side) 1. Vishnu DANGOL (Tribhuvan Univ.) PI Applied Geology 2. Smajwal BAJRACHARYA (ICIMOD) Remote sensing 3. Shanmukhesh Chandra AMATYA (DWIDP) Hydrogeology 4. Tuk Lal ADHIKARI (ITECO-Nepal) Geotechnical Field survey • Trishuli River catchment from Trishuli to Syabrubesi (29 October to 1 November, 2015) • Sun Kosi and Bhote Kosi River catchments from Bansaghu to Kodari. -
Situation Analysis Nepal Earthquake
Situation Analysis OSOCC Nepal Earthquake Assessment Cell 05.05.2015 SITUATION OVERVIEW The earthquake from 25 April (7.8 magnitude) was followed by a series of aftershocks up to a magnitude of 6.7, mostly to the east of the original epicentre causing further localised damage. As of 4 May, 7,365 people have been killed and more than 14,300 injured. 39 of Nepal’s 75 districts have been affected. Access to remote areas remains a challenge. Initial reports were that up to 90 per cent of the houses in Gorkha and Sindhupalchok districts have been destroyed. UNDAC has established humanitarian hubs in Gorkha and Sindhupalchok. Most affected districts (4 May 2015) Based on estimates of damaged buildings. Analysis using data from: Multi-National Military and Coordination Centre, Ministry of Home Affairs, National Population Census (2011) Priorities for humanitarian intervention (based on consolidated secondary data): Shelter: tarpaulins, tents, blankets, repair tools and other NFIs Food delivery WASH: water supply, sanitation Health: facilities, medicine Access to remote areas Ensuring equitable distribution of relief items Rubble removal CRISIS IMPACT According to the government, the worst affected districts are Bhaktapur, Dhading, Dolakha, Gorkha, Kathmandu, Lalitpur, Lamjung, Rasuwa, Ramechhap, Nuwakot, Sindhupalchok, Makawanpur, and Sindhuli (LCT 02/05/2015). Currently available information indicates that Sindhupalchok, Gorkha and Dhading are the priority districts for assistance. Although Rasuwa has a relatively small population, it is difficult to access and current information indiactesover 80% of the population are affected. While the relief effort is now reaching beyond Kathmandu, access to remote areas remains a key challenge (LCT 02/05/2015). -
Spatial Heterogeneous of Ecological Vulnerability in Arid and Semi-Arid Area: a Case of the Ningxia Hui Autonomous Region, China
sustainability Article Spatial Heterogeneous of Ecological Vulnerability in Arid and Semi-Arid Area: A Case of the Ningxia Hui Autonomous Region, China Rong Li 1, Rui Han 1, Qianru Yu 1, Shuang Qi 2 and Luo Guo 1,* 1 College of the Life and Environmental Science, Minzu University of China, Beijing 100081, China; [email protected] (R.L.); [email protected] (R.H.); [email protected] (Q.Y.) 2 Department of Geography, National University of Singapore; Singapore 117570, Singapore; [email protected] * Correspondence: [email protected] Received: 25 April 2020; Accepted: 26 May 2020; Published: 28 May 2020 Abstract: Ecological vulnerability, as an important evaluation method reflecting regional ecological status and the degree of stability, is the key content in global change and sustainable development. Most studies mainly focus on changes of ecological vulnerability concerning the temporal trend, but rarely take arid and semi-arid areas into consideration to explore the spatial heterogeneity of the ecological vulnerability index (EVI) there. In this study, we selected the Ningxia Hui Autonomous Region on the Loess Plateau of China, a typical arid and semi-arid area, as a case to investigate the spatial heterogeneity of the EVI every five years, from 1990 to 2015. Based on remote sensing data, meteorological data, and economic statistical data, this study first evaluated the temporal-spatial change of ecological vulnerability in the study area by Geo-information Tupu. Further, we explored the spatial heterogeneity of the ecological vulnerability using Getis-Ord Gi*. Results show that: (1) the regions with high ecological vulnerability are mainly concentrated in the north of the study area, which has high levels of economic growth, while the regions with low ecological vulnerability are mainly distributed in the relatively poor regions in the south of the study area. -
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ASIAN DEVELOPMENT BANK TAR:PRC 31175 TECHNICAL ASSISTANCE (Financed by the Cooperation Fund in Support of the Formulation and Implementation of National Poverty Reduction Strategies) TO THE PEOPLE'S REPUBLIC OF CHINA FOR PARTICIPATORY POVERTY REDUCTION PLANNING FOR SMALL MINORITIES August 2003 CURRENCY EQUIVALENTS (as of 31 July 2003) Currency Unit – yuan (CNY) Y1.00 = $0.1208 $1.00 = Y8.2773 ABBREVIATIONS ADB – Asian Development Bank FCPMC – Foreign Capital Project Management Center LGOP – State Council Leading Group on Poverty Alleviation and Development NGO – nongovernment organization PRC – People's Republic of China RETA – regional technical assistance SEAC – State Ethnic Affairs Commission TA – technical assistance UNDP – United Nations Development Programme NOTES (i) The fiscal year (FY) of the Government ends on 31 December (ii) In this report, "$" refers to US dollars. This report was prepared by D. S. Sobel, senior country programs specialist, PRC Resident Mission. I. INTRODUCTION 1. During the 2002 Asian Development Bank (ADB) Country Programming Mission to the People's Republic of China (PRC), the Government reconfirmed its request for technical assistance (TA) for Participatory Poverty Reduction Planning for Small Minorities as a follow-up to TA 3610- PRC: Preparing a Methodology for Development Planning in Poverty Blocks under the New Poverty Strategy. After successful preparation of the methodology and its adoption by the State Council Leading Group on Poverty Alleviation and Development (LGOP) to identify poor villages within the “key working counties” (which are eligible for national poverty reduction funds), the Government would like to apply the methodology to the PRC's poorest minority areas to prepare poverty reduction plans with villager, local government, and nongovernment organization (NGO) participation. -
17-Point Agreement of 1951 by Song Liming
FACTS ABOUT THE 17-POINT “Agreement’’ Between Tibet and China Dharamsala, 22 May 22 DIIR PUBLICATIONS The signed articles in this publication do not necessarily reflect the views of the Central Tibetan Administration. This report is compiled and published by the Department of Information and International Relations, Central Tibetan Administration, Gangchen Kyishong, Dharamsala 176 215, H. P., INDIA Email: [email protected] Website: www.tibet.net and ww.tibet.com CONTENTS Part One—Historical Facts 17-point “Agreement”: The full story as revealed by the Tibetans and Chinese who were involved Part Two—Scholars’ Viewpoint Reflections on the 17-point Agreement of 1951 by Song Liming The “17-point Agreement”: Context and Consequences by Claude Arpi The Relevance of the 17-point Agreement Today by Michael van Walt van Praag Tibetan Tragedy Began with a Farce by Cao Changqing Appendix The Text of the 17-point Agreement along with the reproduction of the original Tibetan document as released by the Chinese government His Holiness the Dalai Lama’s Press Statements on the “Agreement” FORWARD 23 May 2001 marks the 50th anniversary of the signing of the 17-point Agreement between Tibet and China. This controversial document, forced upon an unwilling but helpless Tibetan government, compelled Tibet to co-exist with a resurgent communist China. The People’s Republic of China will once again flaunt this dubious legal instrument, the only one China signed with a “minority” people, to continue to legitimise its claim on the vast, resource-rich Tibetan tableland. China will use the anniversary to showcase its achievements in Tibet to justify its continued occupation of the Tibetan Plateau. -
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StudyontheInteractionoftheSinicizationofChristianityand theReconstructionofCrossGborderEthnicMinoritiesƳCulturesinYunnan〔1〕 ZhiyingGAOandDongleiWANG (YunnanUniversityandYunnanUniversityofFinanceandEconomics,Kunming,YunnanProvince,P.R.China) Abstract :TheSinicizationofChristianity,whichisthedevelopingstrategyandpracticeto makeChristianityadaptto Chineseculture.ItcorrespondstotheChristianizationofChineseethnic minoritypeoplewhobelievedinChristianity. Fromtheperspectiveofculturalinteraction,borrowingandblending,thestudyexploresthe motivation,processand characteristicsoftheinteractivedevelopmentbetweenthelocalizationandcontextualizationofChristianityin Yunnan ethnicminorities ‘areasandtheChristianizationofethnic minorities’culturesbyhistoricalcombingandsynchronic comparison.Mostly between Christianity and ethnic minoritiesƳ traditional cultures had experienced from the estrangement,andcoexistedwitheachotherandblendingprocess,andfinishedtheChristianfrom “in”tothetransitionof “again”,soastorealizetheSinicizationalcharacteristicsoftheregional,national,butalsomaketheborderethniccultural reconstruct. KeyWords :Yunnanethnicminorities;Sinicization;Christianization;Interactivedevelopment Author :GaoZhiying,Professor,PhD,CenterforStudiesofChineseSouthwestƳsBorderlandEthnicMinoritiesofYunnan University.Tel:13888072229Email:2296054891@qq.com WangDonglei,ViceProfessor,PhD,SchoolofInternational LanguagesandCulturesofYunnanUniversityofFinanceandEconomics.Tel:15887015580Email:1609766878@qq.com Ⅰ.TheOriginoftheTopic JustasZhuoXinpingsaid,ItisnecessaryforforeignreligionssuchasBuddhism,Christianity -
Estimations of Undisturbed Ground Temperatures Using Numerical and Analytical Modeling
ESTIMATIONS OF UNDISTURBED GROUND TEMPERATURES USING NUMERICAL AND ANALYTICAL MODELING By LU XING Bachelor of Arts/Science in Mechanical Engineering Huazhong University of Science & Technology Wuhan, China 2008 Master of Arts/Science in Mechanical Engineering Oklahoma State University Stillwater, OK, US 2010 Submitted to the Faculty of the Graduate College of the Oklahoma State University in partial fulfillment of the requirements for the Degree of DOCTOR OF PHILOSOPHY December, 2014 ESTIMATIONS OF UNDISTURBED GROUND TEMPERATURES USING NUMERICAL AND ANALYTICAL MODELING Dissertation Approved: Dr. Jeffrey D. Spitler Dissertation Adviser Dr. Daniel E. Fisher Dr. Afshin J. Ghajar Dr. Richard A. Beier ii ACKNOWLEDGEMENTS I would like to thank my advisor, Dr. Jeffrey D. Spitler, who patiently guided me through the hard times and encouraged me to continue in every stage of this study until it was completed. I greatly appreciate all his efforts in making me a more qualified PhD, an independent researcher, a stronger and better person. Also, I would like to devote my sincere thanks to my parents, Hongda Xing and Chune Mei, who have been with me all the time. Their endless support, unconditional love and patience are the biggest reason for all the successes in my life. To all my good friends, colleagues in the US and in China, who talked to me and were with me during the difficult times. I would like to give many thanks to my committee members, Dr. Daniel E. Fisher, Dr. Afshin J. Ghajar and Dr. Richard A. Beier for their suggestions which helped me to improve my research and dissertation. -
Regionalization of Cryosphere Water Resource Service
Desalination and Water Treatment 168 (2019) 394–404 www.deswater.com November doi: 10.5004/dwt.2019.24214 Regionalization of cryosphere water resource service Haoxi Lina,b,c, Jinchuan Huangb,c,*, Chuanglin Fangb,c, Jie Liub,c, Xiaoxiao Qib, Yunqian Chend aGuangzhou Institute of Geography, Guangdong Open Laboratory of Geospatial Information Technology and Application, Guangzhou 510070, China bInstitute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China, email: [email protected] (J.C. Huang) cCollege of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China dBeijing National Day School, Beijing 100039, China Received 22 October 2018; Accepted 21 January 2019 abstract The cryosphere water resource service (CWRS) is the most significant cryosphere service (CS) to directly affect human societies. Regionalization of CWRS is an important prototype for the comprehensive regionalization of CSs. It is also a crucial cutting-edge exploration of interdisciplinary work across cryospheric science, physical geography and human geography. We constructed a quan- titative indexing system for the regionalization of CWRS along the dimensions of base–supply– demand informed by the characteristics of cryosphere resources and human use of CSs. Different levels of regionalization are subdivided using cluster analysis, the importance index of CWRS, and a location entropy model. A region in Northwest China with significant CWRS use was the study area. From the joint effects of nature and human activity, there emerge principles of regional differentia- tion that govern the regionalization of CWRS. The study area was first divided into three high level service regions according to the availability of stored cryosphere water in snow cover, frozen ground and glaciers, indicating the regulatory function of cryosphere components. -
Diversion of the Paleo‐Yellow River Channel in the Qingtongxia Area of Ningxia, China: Evidence from Terraces and Fluvial Landforms
Received: 28 June 2019 Revised: 3 September 2019 Accepted: 13 October 2019 DOI: 10.1002/gj.3684 SPECIAL ISSUE ARTICLE Diversion of the paleo‐Yellow River channel in the Qingtongxia area of Ningxia, China: Evidence from terraces and fluvial landforms Hong Chen1,2 | Guo‐dong Bao1 | Wei Shi1,2 | Jian‐min Hu1,2 1 Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, China The Qingtongxia Grand Canyon (QGC) of the Yellow River is a region of intense tec- 2 Key Laboratory of Paleomagnetism and tonic deformation that is located in the southern Yinchuan Basin, at the junction of Tectonic Reconstruction of Ministry of Natural Resources, Beijing, China the western margin of the Ordos Plateau and the northeast arcuate structural belt of the Qinghai–Tibetan Plateau. The Yellow River makes a 90° turn as it traverses Correspondence Hong Chen, Institute of Geomechanics, the Qingtongxia area, incising the hard Ordovician sandstones of Niushou Mountain, Chinese Academy of Geological Sciences, while leaving the relatively soft Quaternary sediments on the northern side of the No.11 Minzudaxue South Road, Haidian District. Beijing 100081, China. channel undisturbed. Despite this apparent inconsistency with the expected pattern Email: [email protected] of river erosion, there has been no significant research to date on the formation of Funding information the QGC. Here, we utilize remote sensing, surficial geomorphology, and shallow cor- Geological Survey Project of the Geological ing to confirm the evolution of the Yellow River channel and formation of the QGC. Survey of China, Grant/Award Numbers: – ‐ DD20160060 and DD20190018; Special Using Landsat Thermic Mapper and ASTER imagery, we identified a N S oriented Funds for Basic Scientific Research Operation zone of high water‐content in the northern part of the QGC that is characterized at Fees of the Chinese Academy of Geosciences, Grant/Award Number: YYWF201616 the surface by marsh and wetlands. -
DEPARTMENT of the INTERIOR U.S. GEOLOGICAL SURVEY Notes
DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Notes on Sedimentary Basins in China Report of the American Sedimentary Basins Delegation to the People's Republic of China A. W. Bally 1 , I-Ming Chou2, R. Clayton3, H. P. Eugster4, S. Kidwell5, L. D. Meckel6, R. T. Ryder7, A. B. Watts8, A. A. Wilson9 1. Rice University, Houston 2. U. S. Geological Survey, Reston 3. California Institute of Technology, Pasadena 4. Johns Hopkins University, Baltimore 5. University of Chicago 6. L. D. Meckel Company, Houston 7. U. S. Geological Survey, Reston 8. Lament Doherty Geological Observatory, Columbia University, New York 9. National Academy of Sciences, Washington Open-File Report 86-327 This report is preliminary and has not been reviewed for conformity with U. S. Geological Survey editiorial standards. 1986 NOTICE The views expressed in this report are those of the members of the Sedimentary Basins Delegation and are in no way the official views of the Committee on Scholarly Communication with the People's Republic of China or its sponsoring organizations the American Council of Learned Societies, the National Academy of Sciences, and the Social Science Research Council. The visit consisting of a bilateral workshop and field trip was part of the exchange program between the two countries and was supported by the National Academy of Sciences in the United States and the China Association for Science and Technology in China, with the Chinese Petroleum Society bearing special responsibilities as host. U.S. funding was provided by the National Science Foundation. The Committee on Scholarly Communication with the People's Republic of China was founded in 1966 by the American Council of Learned Societies, the National Academy of Sciences, and the Social Science Research Council. -
NUNAWADING MILITARY HISTORY GROUP MINI NEWSLETTER No. 21 SINO INDIAN WAR of 1967
NUNAWADING MILITARY HISTORY GROUP MINI NEWSLETTER No. 21 SINO INDIAN WAR OF 1967 The Nathu La and Cho La clashes were a series of military clashes between India and China alongside the border of the Himalayan Kingdom of Sikkim, then an Indian protectorate. The Nathu La clashes started on 11 September 1967, when the People's Liberation Army (PLA) launched an attack on Indian posts at Nathu La, and lasted till 15 September 1967. In October 1967, another military duel took place at Cho La and ended on the same day. According to independent sources, India achieved "decisive tactical advantage" and managed to hold its own against Chinese forces. PLA fortifications at Nathu La were said to be destroyed, where the Indian troops drove back the attacking Chinese forces. The competition to control the disputed borderland in Chumbi valley is seen as a major cause for heightening the tensions in these incidents. Observers have commented that these clashes indicated the decline of 'claim strength' in China's decision to initiate the use of force against India, and stated that India was greatly pleased with the combat performance of its forces in the Nathu La clashes, seeing it as a sign of striking improvement since its defeat in the 1962 Sino-Indian War. Background Following the 1962 Sino-Indian War, tensions continued to run high along the Himalayan border shared by India and China. Influenced by its previous defeat, the Indian Army raised a number of new units, nearly doubling their deployed forces along the disputed region. As a part of this military expansion, seven mountain divisions were raised to defend India's northern borders against any Chinese attack. -
The Design of the Ali CMB Polarization Telescope Receiver
The design of the Ali CMB Polarization Telescope receiver M. Salatinoa,b, J.E. Austermannc, K.L. Thompsona,b, P.A.R. Aded, X. Baia,b, J.A. Beallc, D.T. Beckerc, Y. Caie, Z. Changf, D. Cheng, P. Chenh, J. Connorsc,i, J. Delabrouillej,k,e, B. Doberc, S.M. Duffc, G. Gaof, S. Ghoshe, R.C. Givhana,b, G.C. Hiltonc, B. Hul, J. Hubmayrc, E.D. Karpela,b, C.-L. Kuoa,b, H. Lif, M. Lie, S.-Y. Lif, X. Lif, Y. Lif, M. Linkc, H. Liuf,m, L. Liug, Y. Liuf, F. Luf, X. Luf, T. Lukasc, J.A.B. Matesc, J. Mathewsonn, P. Mauskopfn, J. Meinken, J.A. Montana-Lopeza,b, J. Mooren, J. Shif, A.K. Sinclairn, R. Stephensonn, W. Sunh, Y.-H. Tsengh, C. Tuckerd, J.N. Ullomc, L.R. Valec, J. van Lanenc, M.R. Vissersc, S. Walkerc,i, B. Wange, G. Wangf, J. Wango, E. Weeksn, D. Wuf, Y.-H. Wua,b, J. Xial, H. Xuf, J. Yaoo, Y. Yaog, K.W. Yoona,b, B. Yueg, H. Zhaif, A. Zhangf, Laiyu Zhangf, Le Zhango,p, P. Zhango, T. Zhangf, Xinmin Zhangf, Yifei Zhangf, Yongjie Zhangf, G.-B. Zhaog, and W. Zhaoe aStanford University, Stanford, CA 94305, USA bKavli Institute for Particle Astrophysics and Cosmology, Stanford, CA 94305, USA cNational Institute of Standards and Technology, Boulder, CO 80305, USA dCardiff University, Cardiff CF24 3AA, United Kingdom eUniversity of Science and Technology of China, Hefei 230026 fInstitute of High Energy Physics, Chinese Academy of Sciences, Beijing 100049 gNational Astronomical Observatories, Chinese Academy of Sciences, Beijing 100012 hNational Taiwan University, Taipei 10617 iUniversity of Colorado Boulder, Boulder, CO 80309, USA jIN2P3, CNRS, Laboratoire APC, Universit´ede Paris, 75013 Paris, France kIRFU, CEA, Universit´eParis-Saclay, 91191 Gif-sur-Yvette, France lBeijing Normal University, Beijing 100875 mAnhui University, Hefei 230039 nArizona State University, Tempe, AZ 85004, USA oShanghai Jiao Tong University, Shanghai 200240 pSun Yat-Sen University, Zhuhai 519082 ABSTRACT Ali CMB Polarization Telescope (AliCPT-1) is the first CMB degree-scale polarimeter to be deployed on the Tibetan plateau at 5,250 m above sea level.