Ethnic Minorities and Regional Development in Asia Reality and Challenges
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Tibetan Plateau (PDF, 279
Tibetan plateau W09 W09 Threatened species HE many high-altitude lakes and marshlands on the Tibetan Tplateau support one unique waterbird species, Black-necked CR EN VU Total Crane, which is widely distributed during the breeding season but —— 22 moves to the relatively low eastern and southern parts of the plateau for the winter. Baer’s Pochard and Pallas’s Fish-eagle also occur on ———— the southern and eastern fringes of the plateau. —— 11 ■ Key habitats High altitude lakes and marshland. Total —— 33 ■ Countries and territories China (Xinjiang, Tibet, Qinghai, Gansu, Sichuan, Yunnan, Guizhou); India (Jammu and Kashmir Key: = breeding in this wetland region. = passage migrant. [Ladakh], Sikkim, Arunachal Pradesh); Bhutan. = non-breeding visitor. Black-necked Crane is unique to the high altitude wetlands of the Tibetan plateau. PHOTO: OTTO PFISTER 177 Tibetan plateau OUTSTANDING IBAs FOR CONSERVATION ISSUES AND STRATEGIC THREATENED BIRDS (see Table 1) SOLUTIONS (summarised in Table 3) Nine IBAs have been selected, including three important Habitat loss and degradation breeding areas and six important non-breeding ■ WETLAND DRAINAGE W09 concentrations of Black-necked Crane. Some of the high-altitude wetlands used by Black-necked Cranes are being converted into wet grasslands, and then CURRENT STATUS OF HABITATS AND gradually into steppe and arid land. Habitat pressures are THREATENED SPECIES heaviest in the species’s wintering range, because it is at relatively low altitudes and more densely populated, with The human population density on the Tibetan plateau is many areas in Yunnan and Guizhou being affected by very low, and many areas are relatively undisturbed. drainage and damming. -
Development for Tibetans, but by Whom?
Consilience: The Journal of Sustainable Development Vol. 5, Iss. 1 (2011), Pp. 168-175 Development For Tibetans, But By Whom? Diana Jue Department of Urban Studies and Planning, International Development Group Massachusetts Institute of Technology, Cambridge, MA [email protected] Keywords: Tibet, China, development, design. 1. Introduction: Tibetans in China In addition to the Han majority, the People‟s Republic of China officially recognizes 55 ethnic minority groups within its borders. The degree to which minorities have been incorporated into the national mainstream community varies widely from group to group, with some demonstrating considerable resentment against the ethnic majority. Most notable are the Turkic Muslim Uyghurs, who made international headlines in July 2009 for the Urumqi riots; the Hui in Hunan province, where unrest broke out in 2004; and, of course, the Tibetans, whose high-profile protests were in to the spotlight in the months preceding the 2008 Olympic games in Beijing. The Tibet-China conflict is one of the most polarized disputes in which China is currently embroiled. At the core of this debate is Tibet‟s status as either an autonomous region of the People‟s Republic of China or an independent country. The Chinese leadership is staunchly against the “legitimate and meaningful autonomy” demanded by the Dalai Lama (BBC News, 2009); the Dalai Lama has also been labeled as a “separatist” by China‟s president Hu Jintao but maintains that he does not want to separate Tibet from China (Mazumdar 2010). Additionally, discontent among Tibetans is not limited to those residing in the Tibet Autonomous Region (TAR). -
Remote Sensing of Alpine Lake Water Environment Changes on the Tibetan Plateau and Surroundings: a Review ⇑ Chunqiao Song A, Bo Huang A,B, , Linghong Ke C, Keith S
ISPRS Journal of Photogrammetry and Remote Sensing 92 (2014) 26–37 Contents lists available at ScienceDirect ISPRS Journal of Photogrammetry and Remote Sensing journal homepage: www.elsevier.com/locate/isprsjprs Review Article Remote sensing of alpine lake water environment changes on the Tibetan Plateau and surroundings: A review ⇑ Chunqiao Song a, Bo Huang a,b, , Linghong Ke c, Keith S. Richards d a Department of Geography and Resource Management, The Chinese University of Hong Kong, Shatin, Hong Kong b Institute of Space and Earth Information Science, The Chinese University of Hong Kong, Shatin, Hong Kong c Department of Land Surveying and Geo-Informatics, The Hong Kong Polytechnic University, Kowloon, Hong Kong d Department of Geography, University of Cambridge, Cambridge CB2 3EN, United Kingdom article info abstract Article history: Alpine lakes on the Tibetan Plateau (TP) are key indicators of climate change and climate variability. The Received 16 September 2013 increasing availability of remote sensing techniques with appropriate spatiotemporal resolutions, broad Received in revised form 26 February 2014 coverage and low costs allows for effective monitoring lake changes on the TP and surroundings and Accepted 3 March 2014 understanding climate change impacts, particularly in remote and inaccessible areas where there are lack Available online 26 March 2014 of in situ observations. This paper firstly introduces characteristics of Tibetan lakes, and outlines available satellite observation platforms and different remote sensing water-body extraction algorithms. Then, this Keyword: paper reviews advances in applying remote sensing methods for various lake environment monitoring, Tibetan Plateau including lake surface extent and water level, glacial lake and potential outburst floods, lake ice phenol- Lake Remote sensing ogy, geological or geomorphologic evidences of lake basins, with a focus on the trends and magnitudes of Glacial lake lake area and water-level change and their spatially and temporally heterogeneous patterns. -
Origin and Character of Loesslike Silt in the Southern Qinghai-Xizang (Tibet) Plateau, China
Origin and Character of Loesslike Silt in the Southern Qinghai-Xizang (Tibet) Plateau, China U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1549 Cover. View south-southeast across Lhasa He (Lhasa River) flood plain from roof of Potala Pal ace, Lhasa, Xizang Autonomous Region, China. The Potala (see frontispiece), characteristic sym bol of Tibet, nses 308 m above the valley floor on a bedrock hill and provides an excellent view of Mt. Guokalariju, 5,603 m elevation, and adjacent mountains 15 km to the southeast These mountains of flysch-like Triassic clastic and volcanic rocks and some Mesozoic granite character ize the southernmost part of Northern Xizang Structural Region (Gangdese-Nyainqentanglha Tec tonic Zone), which lies just north of the Yarlung Zangbo east-west tectonic suture 50 km to the south (see figs. 2, 3). Mountains are part of the Gangdese Island Arc at south margin of Lhasa continental block. Light-tan areas on flanks of mountains adjacent to almost vegetation-free flood plain are modern and ancient climbing sand dunes that exhibit evidence of strong winds. From flood plain of Lhasa He, and from flood plain of much larger Yarlung Zangbo to the south (see figs. 2, 3, 13), large dust storms and sand storms originate today and are common in capitol city of Lhasa. Blowing silt from larger braided flood plains in Pleistocene time was source of much loesslike silt described in this report. Photograph PK 23,763 by Troy L. P6w6, June 4, 1980. ORIGIN AND CHARACTER OF LOESSLIKE SILT IN THE SOUTHERN QINGHAI-XIZANG (TIBET) PLATEAU, CHINA Frontispiece. -
2019 International Religious Freedom Report
CHINA (INCLUDES TIBET, XINJIANG, HONG KONG, AND MACAU) 2019 INTERNATIONAL RELIGIOUS FREEDOM REPORT Executive Summary Reports on Hong Kong, Macau, Tibet, and Xinjiang are appended at the end of this report. The constitution, which cites the leadership of the Chinese Communist Party and the guidance of Marxism-Leninism and Mao Zedong Thought, states that citizens have freedom of religious belief but limits protections for religious practice to “normal religious activities” and does not define “normal.” Despite Chairman Xi Jinping’s decree that all members of the Chinese Communist Party (CCP) must be “unyielding Marxist atheists,” the government continued to exercise control over religion and restrict the activities and personal freedom of religious adherents that it perceived as threatening state or CCP interests, according to religious groups, nongovernmental organizations (NGOs), and international media reports. The government recognizes five official religions – Buddhism, Taoism, Islam, Protestantism, and Catholicism. Only religious groups belonging to the five state- sanctioned “patriotic religious associations” representing these religions are permitted to register with the government and officially permitted to hold worship services. There continued to be reports of deaths in custody and that the government tortured, physically abused, arrested, detained, sentenced to prison, subjected to forced indoctrination in CCP ideology, or harassed adherents of both registered and unregistered religious groups for activities related to their religious beliefs and practices. There were several reports of individuals committing suicide in detention, or, according to sources, as a result of being threatened and surveilled. In December Pastor Wang Yi was tried in secret and sentenced to nine years in prison by a court in Chengdu, Sichuan Province, in connection to his peaceful advocacy for religious freedom. -
Religion in China BKGA 85 Religion Inchina and Bernhard Scheid Edited by Max Deeg Major Concepts and Minority Positions MAX DEEG, BERNHARD SCHEID (EDS.)
Religions of foreign origin have shaped Chinese cultural history much stronger than generally assumed and continue to have impact on Chinese society in varying regional degrees. The essays collected in the present volume put a special emphasis on these “foreign” and less familiar aspects of Chinese religion. Apart from an introductory article on Daoism (the BKGA 85 BKGA Religion in China prototypical autochthonous religion of China), the volume reflects China’s encounter with religions of the so-called Western Regions, starting from the adoption of Indian Buddhism to early settlements of religious minorities from the Near East (Islam, Christianity, and Judaism) and the early modern debates between Confucians and Christian missionaries. Contemporary Major Concepts and religious minorities, their specific social problems, and their regional diversities are discussed in the cases of Abrahamitic traditions in China. The volume therefore contributes to our understanding of most recent and Minority Positions potentially violent religio-political phenomena such as, for instance, Islamist movements in the People’s Republic of China. Religion in China Religion ∙ Max DEEG is Professor of Buddhist Studies at the University of Cardiff. His research interests include in particular Buddhist narratives and their roles for the construction of identity in premodern Buddhist communities. Bernhard SCHEID is a senior research fellow at the Austrian Academy of Sciences. His research focuses on the history of Japanese religions and the interaction of Buddhism with local religions, in particular with Japanese Shintō. Max Deeg, Bernhard Scheid (eds.) Deeg, Max Bernhard ISBN 978-3-7001-7759-3 Edited by Max Deeg and Bernhard Scheid Printed and bound in the EU SBph 862 MAX DEEG, BERNHARD SCHEID (EDS.) RELIGION IN CHINA: MAJOR CONCEPTS AND MINORITY POSITIONS ÖSTERREICHISCHE AKADEMIE DER WISSENSCHAFTEN PHILOSOPHISCH-HISTORISCHE KLASSE SITZUNGSBERICHTE, 862. -
Growth and Decline of Muslim Hui Enclaves in Beijing
EG1402.fm Page 104 Thursday, June 21, 2007 12:59 PM Growth and Decline of Muslim Hui Enclaves in Beijing Wenfei Wang, Shangyi Zhou, and C. Cindy Fan1 Abstract: The Hui people are a distinct ethnic group in China in terms of their diet and Islamic religion. In this paper, we examine the divergent residential and economic develop- ment of Niujie and Madian, two Hui enclaves in the city of Beijing. Our analysis is based on archival and historical materials, census data, and information collected from recent field work. We show that in addition to social perspectives, geographic factors—location relative to the northward urban expansion of Beijing, and the character of urban administrative geog- raphy in China—are important for understanding the evolution of ethnic enclaves. Journal of Economic Literature, Classification Numbers: O10, I31, J15. 3 figures, 2 tables, 60 refer- ences. INTRODUCTION esearch on ethnic enclaves has focused on their residential and economic functions and Ron the social explanations for their existence and persistence. Most studies do not address the role of geography or the evolution of ethnic enclaves, including their decline. In this paper, we examine Niujie and Madian, two Muslim Hui enclaves in Beijing, their his- tory, and recent divergent paths of development. While Niujie continues to thrive as a major residential area of the Hui people in Beijing and as a prominent supplier of Hui foods and services for the entire city, both the Islamic character and the proportion of Hui residents in Madian have declined. We argue that Madian’s location with respect to recent urban expan- sion in Beijing and the administrative geography of the area have contributed to the enclave’s decline. -
Himalaya - Southern-Tibet: the Typical Continent-Continent Collision Orogen
237 Himalaya - Southern-Tibet: the typical continent-continent collision orogen When an oceanic plate is subducted beneath a continental lithosphere, an Andean mountain range develops on the edge of the continent. If the subducting plate also contains some continental lithosphere, plate convergence eventually brings both continents into juxtaposition. While the oceanic lithosphere is relatively dense and sinks into the asthenosphere, the greater sialic content of the continental lithosphere ascribes positive buoyancy in the asthenosphere, which hinders the continental lithosphere to be subducted any great distance. Consequently, a continental lithosphere arriving at a trench will confront the overriding continent. Rapid relative convergence is halted and crustal shortening forms a collision mountain range. The plane marking the locus of collision is a suture, which usually preserves slivers of the oceanic lithosphere that formerly separated the continents, known as ophiolites. The collision between the Indian subcontinent and what is now Tibet began in the Eocene. It involved and still involves north-south convergence throughout southern Tibet and the Himalayas. This youthful mountain area is the type example for studies of continental collision processes. The Himalayas Location The Himalayas form a nearly 3000 km long, 250-350 km wide range between India to the south and the huge Tibetan plateau, with a mean elevation of 5000 m, to the north. The Himalayan mountain belt has a relatively simple, arcuate, and cylindrical geometry over most of its length and terminates at both ends in nearly transverse syntaxes, i.e. areas where orogenic structures turn sharply about a vertical axis. Both syntaxes are named after the main peaks that tower above them, the Namche Barwa (7756 m) to the east and the Nanga Parbat (8138 m) to the west, in Pakistan. -
Sichuan/Gansu/Qinghai/Tibet (14 Days) We Love Road Journeys
Tibetan Highlands: Sichuan/Gansu/Qinghai/Tibet (14 Days) We love road journeys. They are by far our favourite way of traveling. We think the world of western China and the countries that border on this region – think Vietnam, Lao, Thailand, Myanmar, for example. On the Road Experiences is all about sharing with like-minded travelers just how beautiful a road journey in these varied lands can be. Now turn the page to find out what we’ve come to love so much… p2 p3 Itinerary Map …where you will travel… p. 006 Yes, it is possible… p. 008 Journey of Discovery… p. 010 Day-by-day… p. 056 In closing... Any car you like, so long as it is an SUV… p. 077 Adventures and discoveries in local cuisines p. 078 What’s included/Best Months to Go... p. 080 Photo credits p. 083 p5 Itinerary Map Day1 Day8 Arrival in Chengdu – Dulan to Golmud – Apply for your temporary driving Across the Qaidam Basin to Golmud license and visit Chengdu’s beautiful Panda Reserve Day9 Golmud to Tuotuohe – Day2 Up, up, up - Onto the Plateau and Chengdu to Maerkang – into the highlands of Qinghai Through the valleys to the Gyarong Tibetan region Day10 Tuotuohe to Naqu – Day3 Cross the famous Tanggula Pass on Maerkang to Ruoergai – your way to Tibet itself Towards the very north of Sichuan on the way to Gansu Day11 Naqu to Damxung – Day4 Visit one of Tibet’s holiest lakes, Ruoergai to Xiahe – Lake Nam-tso Your first and only stop in Gansu province Day12 Damxung to Lhasa – Day5 Complete your journey with Xiahe to Qinghai’s capital, Xining – a beautiful drive to your final On your way to Qinghai destination Day6 Day13 Xining – In and around Lhasa – Spend a day in and around Xining for Visit Potala Palace and explore the a bit of rest and visit the spectacular old city of Lhasa Ta’er Monastery Day14 Day7 Depart from Lhasa – Xining to Dulan – Lift must go on...Farewell Lhasa On the way to Golmud.. -
Genetic Structure and Eco-Geographical Differentiation of Lancea Tibetica in the Qinghai-Tibetan Plateau
G C A T T A C G G C A T genes Article Genetic Structure and Eco-Geographical Differentiation of Lancea tibetica in the Qinghai-Tibetan Plateau Xiaofeng Chi 1,2 , Faqi Zhang 1,2,* , Qingbo Gao 1,2, Rui Xing 1,2 and Shilong Chen 1,2,* 1 Key Laboratory of Adaptation and Evolution of Plateau Biota, Northwest Institute of Plateau Biology, Chinese Academy of Sciences, Xining 810001, China; [email protected] (X.C.); [email protected] (Q.G.); [email protected] (R.X.) 2 Qinghai Provincial Key Laboratory of Crop Molecular Breeding, Xining 810001, China * Correspondence: [email protected] (F.Z.); [email protected] (S.C.) Received: 14 December 2018; Accepted: 24 January 2019; Published: 29 January 2019 Abstract: The uplift of the Qinghai-Tibetan Plateau (QTP) had a profound impact on the plant speciation rate and genetic diversity. High genetic diversity ensures that species can survive and adapt in the face of geographical and environmental changes. The Tanggula Mountains, located in the central of the QTP, have unique geographical significance. The aim of this study was to investigate the effect of the Tanggula Mountains as a geographical barrier on plant genetic diversity and structure by using Lancea tibetica. A total of 456 individuals from 31 populations were analyzed using eight pairs of microsatellite makers. The total number of alleles was 55 and the number per locus ranged from 3 to 11 with an average of 6.875. The polymorphism information content (PIC) values ranged from 0.2693 to 0.7761 with an average of 0.4378 indicating that the eight microsatellite makers were efficient for distinguishing genotypes. -
Drought Evolution Characteristics of the Qinghai-Tibet Plateau Over the Last 100 Years Based on SPEI
https://doi.org/10.5194/nhess-2021-73 Preprint. Discussion started: 31 March 2021 c Author(s) 2021. CC BY 4.0 License. Drought evolution characteristics of the Qinghai-Tibet Plateau over the last 100 years based on SPEI Shengzhen Wang1, Fenggui Liu1,2 , Qiang Zhou1 , Qiong Chen1, Baicheng Niu1 , Xingsheng Xia1 1 College of Geographical Sciences, Qinghai Normal University, Xining, 811600, China 5 2 Academy of Plateau Science and Sustainability, Xining, 811600, China Correspondence to: Fenggui Liu ([email protected]) Abstract: The standardized precipitation evapotranspiration index (SPEI) of the Qinghai-Tibetan Plateau was calculated using the CRU4.03 gridded dataset from 1901 to 2018 in this paper. Then, based on the SPEI data, drought on the Qinghai-Tibet Plateau was studied in terms of its spatial and temporal distributions and its changing characteristics over the last 100 years. 10 The results revealed that the precipitation in the southeastern part of the Qinghai-Tibet Plateau has been steadily rising over the last 100 years, in conjunction with only minor temperature shifts. In the northwestern part of the plateau, precipitation has decreased significantly, accompanied by a significant increase in temperature. The drought on the Qinghai-Tibetan Plateau showed a clear gradual increase in aridity from southeast to northwest over the last hundred years. The SPEI also showed distinct seasonal patterns, steadily increasing in spring and summer and decreasing significantly in autumn and winter. In 15 addition, each season had its own spatial characteristics. The northeastern part of the plateau, except the Qaidam Basin, showed a significant aridity trend in all seasons. -
Stroeven-Et-Al-2009-Landscape-Analysis-Huang-He-Headwaters.Pdf
Geomorphology 103 (2009) 212–226 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Landscape analysis of the Huang He headwaters, NE Tibetan Plateau — Patterns of glacial and fluvial erosion A.P. Stroeven a,⁎, C. Hättestrand a, J. Heyman a, J. Harbor b, Y.K. Li c, L.P. Zhou d, M.W. Caffee e, H. Alexanderson a, J. Kleman a, H.Z. Ma f, G.N. Liu d a Department of Physical Geography and Quaternary Geology, Stockholm University, Sweden b Department of Earth and Atmospheric Sciences, Purdue University, USA c Department of Geography, University of Missouri-Columbia, USA d Department of Geography, Peking University, Beijing, China e Purdue Rare Isotope Measurement Laboratory, Purdue University, West Lafayette, USA f Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China ARTICLE INFO ABSTRACT Article history: The large-scale geomorphology of the Huang He (Yellow River) headwaters, centered around the Bayan Har Accepted 1 December 2007 Shan (5267 m asl) in the northeastern part of the Tibetan Plateau, is dominated by an uplifted remnant of a Available online 10 May 2008 low-relief relict plateau with several mountain ranges. We have performed geomorphological mapping using SRTM topographic data and Landsat 7 ETM+ satellite imagery to evaluate landscape characteristics and Keywords: patterns, and to investigate the relative importance of different erosional processes in the dissection of this Tibet plateau remnant. The distribution of valley morphologies indicates that the eastern and southern margins of Glacial history River incision the plateau remnant have been extensively dissected by the Huang He and Chang Jiang (Yangtze) rivers and Huang He Ice Sheet associated tributaries, while the mountain ranges have valley morphologies with U-shaped cross-sections Relict surface that indicate large impacts from glacial erosion during Quaternary glaciations.