Assessment of Japanese and Chinese Flood Control Policies
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The Chinese Civil War (1927–37 and 1946–49)
13 CIVIL WAR CASE STUDY 2: THE CHINESE CIVIL WAR (1927–37 AND 1946–49) As you read this chapter you need to focus on the following essay questions: • Analyze the causes of the Chinese Civil War. • To what extent was the communist victory in China due to the use of guerrilla warfare? • In what ways was the Chinese Civil War a revolutionary war? For the first half of the 20th century, China faced political chaos. Following a revolution in 1911, which overthrew the Manchu dynasty, the new Republic failed to take hold and China continued to be exploited by foreign powers, lacking any strong central government. The Chinese Civil War was an attempt by two ideologically opposed forces – the nationalists and the communists – to see who would ultimately be able to restore order and regain central control over China. The struggle between these two forces, which officially started in 1927, was interrupted by the outbreak of the Sino-Japanese war in 1937, but started again in 1946 once the war with Japan was over. The results of this war were to have a major effect not just on China itself, but also on the international stage. Mao Zedong, the communist Timeline of events – 1911–27 victor of the Chinese Civil War. 1911 Double Tenth Revolution and establishment of the Chinese Republic 1912 Dr Sun Yixian becomes Provisional President of the Republic. Guomindang (GMD) formed and wins majority in parliament. Sun resigns and Yuan Shikai declared provisional president 1915 Japan’s Twenty-One Demands. Yuan attempts to become Emperor 1916 Yuan dies/warlord era begins 1917 Sun attempts to set up republic in Guangzhou. -
World's Major Rivers
WWWWWWoorrlldd’’ss mmaajjoorr rriivveerrss AAnn IInnttrroodduuccttiioonn ttoo iinntteerrnnaattiioonnaall wwwwwwaatteerr llaawwwwww wwwwwwiitthh ccaassee ssttuuddiieess THIS PAGE INTENTIONALLY LEFT BLANK WWWWWWoorrlldd’’ss mmaajjoorr rriivveerrss An introduction to international water law with case studies Colorado River Commission of Nevada 555 E. Washington Avenue, Suite 3100 Las Vegas, Nevada 89101 Phone: (702) 486-2670 Website: http://crc.nv.gov November 2008 Jacob (Jay) D. Bingham, Chairman Ace I. Robinson, Vice Chairman Andrea Anderson, Commissioner Marybel Batjer, Commissioner Chip Maxfield, Commissioner George F. Ogilvie III, Commissioner Lois Tarkanian, Commissioner George M. Caan, Executive Director Primary Author: Daniel Seligman, Attorney at Law Columbia Research Corp. P.O. Box 99249 Seattle, Washington 98139 (206) 285-1185 Project Editors: McClain Peterson, Project Manager Manager, Natural Resource Division Colorado River Commission of Nevada Sara Price Special Counsel-Consultant Colorado River Commission of Nevada Esther Valle Natural Resource Analyst Colorado River Commission of Nevada Nicole Everett Natural Resource Analyst Colorado River Commission of Nevada THIS PAGE INTENTIONALLY LEFT BLANK World’s Major Rivers ACKNOWLEDGMENTS Daniel Seligman at the Columbia Research Corp. wishes to thank Jacqueline Pruner, attorney at law in Seattle, for her contribution to the section on water law in Canada and her valuable editing assistance throughout the entire document. The staff at the Murray-Darling Basin Commission and Goulburn-Murray Water in Australia provided important information about the Murray-Darling River system, patiently answered the author’s questions, and reviewed the draft text on water trading. Staff at the International Joint Commission in Washington, D.C., and the Prairie Provinces Water Board in Regina, Canada, also offered helpful comments on an earlier draft. -
Respective Influence of Vertical Mountain Differentiation on Debris Flow Occurrence in the Upper Min River, China
www.nature.com/scientificreports OPEN Respective infuence of vertical mountain diferentiation on debris fow occurrence in the Upper Min River, China Mingtao Ding*, Tao Huang , Hao Zheng & Guohui Yang The generation, formation, and development of debris fow are closely related to the vertical climate, vegetation, soil, lithology and topography of the mountain area. Taking in the upper reaches of Min River (the Upper Min River) as the study area, combined with GIS and RS technology, the Geo-detector (GEO) method was used to quantitatively analyze the respective infuence of 9 factors on debris fow occurrence. We identify from a list of 5 variables that explain 53.92%% of the total variance. Maximum daily rainfall and slope are recognized as the primary driver (39.56%) of the spatiotemporal variability of debris fow activity. Interaction detector indicates that the interaction between the vertical diferentiation factors of the mountainous areas in the study area is nonlinear enhancement. Risk detector shows that the debris fow accumulation area and propagation area in the Upper Min River are mainly distributed in the arid valleys of subtropical and warm temperate zones. The study results of this paper will enrich the scientifc basis of prevention and reduction of debris fow hazards. Debris fows are a common type of geological disaster in mountainous areas1,2, which ofen causes huge casual- ties and property losses3,4. To scientifcally deal with debris fow disasters, a lot of research has been carried out from the aspects of debris fow physics5–9, risk assessment10–12, social vulnerability/resilience13–15, etc. Jointly infuenced by unfavorable conditions and factors for social and economic development, the Upper Min River is a geographically uplifed but economically depressed region in Southwest Sichuan. -
Sustainable Tourism in Vibrant Chengdu
CHINA DAILY MONDAY, OCTOBER 15, 2012 chengduspecial 7 Left to right: Night view of the Tianfu Bridge in Chengdu, the provincial capital. Gateway to the Qingcheng Mountains, birthplace of Taoism. Renowned Sichuan hotpot is one of the city’s signature dishes. UN: Sustainable tourism in vibrant Chengdu particularly spiciness from liberal use of gar- Home of the giant lic and chili peppers as well as the unique flavor of the Sichuan pepper. panda, ancient One dish recommended by almost all is Sichuan hotpot. As the metal pot starts to simmer, typi- wonders and cal ingredients including thinly sliced meat, leafy vegetables, mushrooms, and seafood renowned cuisine, are added. The result is usually eaten with a dipping sauce. Visitors to Chengdu can enjoy the dish Li Fusheng reports. at countless hotpot restaurants operating throughout the city. he UN World Tourism Organiza- in the world. Another signature dish of Sichuan cuisine tion unveiled an agency to observe The Dujiangyan system, which has stood is mapo tofu — soft bean curd served up with tourism development on Oct 12 in for nearly 2,300 years, silently diverts water a fiery meat sauce. Chengdu, the capital city of South- to irrigate nearly 70,000 hectares of farmland In addition, Zongfu Road, Chunxi Road Twest China’s Sichuan province, as part of its that produce almost a third of the province’s and Jinli Street are places to taste delicious Global Observatory on Sustainable Tourism grain. It survived the disastrous Wenchuan local snacks in Chengdu. The 5-square-kilometer Jinsha site in the city’s western suburbs has been hailed as one of program. -
Dams on the Mekong
Dams on the Mekong A literature review of the politics of water governance influencing the Mekong River Karl-Inge Olufsen Spring 2020 Master thesis in Human geography at the Department of Sociology and Human Geography, Faculty of Social Sciences UNIVERSITY OF OSLO Words: 28,896 08.07.2020 II Dams on the Mekong A literature review of the politics of water governance influencing the Mekong River III © Karl-Inge Olufsen 2020 Dams on the Mekong: A literature review of the politics of water governance influencing the Mekong River Karl-Inge Olufsen http://www.duo.uio.no/ IV Summary This thesis offers a literature review on the evolving human-nature relationship and effect of power struggles through political initiatives in the context of Chinese water governance domestically and on the Mekong River. The literature review covers theoretical debates on scale and socionature, combining them into one framework to understand the construction of the Chinese waterscape and how it influences international governance of the Mekong River. Purposive criterion sampling and complimentary triangulation helped me do rigorous research despite relying on secondary sources. Historical literature review and integrative literature review helped to build an analytical narrative where socionature and scale explained Chinese water governance domestically and on the Mekong River. Through combining the scale and socionature frameworks I was able to build a picture of the hybridization process creating the Chinese waterscape. Through the historical review, I showed how water has played an important part for creating political legitimacy and influencing, and being influenced, by state-led scalar projects. Because of this importance, throughout history the Chinese state has favored large state-led scalar projects for the governance of water. -
Irrigation of World Agricultural Lands: Evolution Through the Millennia
water Review Irrigation of World Agricultural Lands: Evolution through the Millennia Andreas N. Angelakιs 1 , Daniele Zaccaria 2,*, Jens Krasilnikoff 3, Miquel Salgot 4, Mohamed Bazza 5, Paolo Roccaro 6, Blanca Jimenez 7, Arun Kumar 8 , Wang Yinghua 9, Alper Baba 10, Jessica Anne Harrison 11, Andrea Garduno-Jimenez 12 and Elias Fereres 13 1 HAO-Demeter, Agricultural Research Institution of Crete, 71300 Iraklion and Union of Hellenic Water Supply and Sewerage Operators, 41222 Larissa, Greece; [email protected] 2 Department of Land, Air, and Water Resources, University of California, California, CA 95064, USA 3 School of Culture and Society, Department of History and Classical Studies, Aarhus University, 8000 Aarhus, Denmark; [email protected] 4 Soil Science Unit, Facultat de Farmàcia, Universitat de Barcelona, 08007 Barcelona, Spain; [email protected] 5 Formerly at Land and Water Division, Food and Agriculture Organization of the United Nations-FAO, 00153 Rome, Italy; [email protected] 6 Department of Civil and Environmental Engineering, University of Catania, 2 I-95131 Catania, Italy; [email protected] 7 The Comisión Nacional del Agua in Mexico City, Del. Coyoacán, México 04340, Mexico; [email protected] 8 Department of Civil Engineering, Indian Institute of Technology, Delhi 110016, India; [email protected] 9 Department of Water Conservancy History, China Institute of Water Resources and Hydropower Research, Beijing 100048, China; [email protected] 10 Izmir Institute of Technology, Engineering Faculty, Department of Civil -
Minshan Draft Factsheet 13Oct06.Indd
Gift to the Earth 103, 25 October 2006 Gift to the Earth China: Sichuan and Gansu Provinces join efforts to preserve the giant panda and its habitat in the Minshan Landscape SUMMARY The 2004 Panda Survey concluded that 1,600 giant pandas survive in the wild. The pandas are scattered in 20 isolated populations in six major landscapes in southwestern China in the upper Yangtze River basin. Almost half these pandas are found in the Minshan landscape, shared by Sichuan and Gansu provinces. In a major development, the provincial governments of Sichuan and Gansu have each committed to establish new protected areas (PAs), linking corridors and co-managed areas to ensure all the pandas in Minshan are both protected and reconnected to ensure their long term health and survival. This represents the designation of almost 1,6 million hectares of panda habitat. Both provincial governments have also committed to establish PAs for other wildlife totaling an additional 900,000 hectares by 2010. WWF considers the giant panda as a ‘flagship’ species – a charismatic animal representative of the biologically rich temperate forest it WWF, the global conservation organization, recognizes these inhabits which also mobilizes support for conservation of the commitments by the two provincial governments as a Gift to larger landscape and its inhabitants. By conserving the giant panda the Earth – symbolizing a globally significant conservation and its habitat, many other species will also be conserved – including achievement and inspiring environmental leadership. -
A Yangtze Three Gorges Adventure ,,,,, .', ,'
CL-15 N OT FOR PUBI' WITHOUT WRITER'S CONSENTIcATION] INSTITUTE OF CURRENT WORLD AFFAIRS LIFE & HU,,MAN RESPONS!,B!L!,TY: A YANGTZE THREE GORGES ADVENTURE ,,,,, .', ,',,, Part III "Damn Dam!" Shanghai, China Summer 1994 Mr. Peter Bird Martin Executive Director Institute of Current World Affairs 4 West Wheelock Street Hanover, NH 03755 U.S.A. Dear Peter, "How could it be possible that the Chinese government has still decided to build the dam at all with the great impact on the environment, cultural relics and migration?" Tony asked me when we stood on. the deck enjoying the beautiful scenery of the Xiling Gorge in the early morning of our last day ofthe cruise. "Is it a silly question?" Tony wanted to have my opinion. "No, not at all," I told Tony. "This is also the question that has puzzled me for several years." When I was a graduate student at Princeton, I intended to write a term paper on the feasibility of the Three Gorges Dam. But later I found it was extremely difficult to get information concerning the dam project because any data related to Cheng Li is a an ICWA fellow studying the political economy of the coast of China. Since 1925 the Institute of Current World Affairs (the Crane-Rogers Foundation) has provided long-term fellowships to enable outstanding young adults to live outside the United Sates and write about international areas and issues. Endowed by the late Charles R. Crane, the Institute is also supported by conu'ibutions from like-minded individuals and foundations. CL-15 2 A scene of the Xiling Gorge. -
Emergence, Concept, and Understanding of Pan-River-Basin
HOSTED BY Available online at www.sciencedirect.com International Soil and Water Conservation Research 3 (2015) 253–260 www.elsevier.com/locate/iswcr Emergence, concept, and understanding of Pan-River-Basin (PRB) Ning Liu The Ministry of Water Resources, Beijing 10083, China Received 10 December 2014; received in revised form 20 September 2015; accepted 11 October 2015 Available online 4 November 2015 Abstract In this study, the concept of Pan-River-Basin (PRB) for water resource management is proposed with a discussion on the emergence, concept, and application of PRB. The formation and application of PRB is also discussed, including perspectives on the river contribution rates, harmonious levels of watershed systems, and water resource availability in PRB system. Understanding PRB is helpful for reconsidering river development and categorizing river studies by the influences from human projects. The sustainable development of water resources and the harmonization between humans and rivers also requires PRB. & 2015 International Research and Training Center on Erosion and Sedimentation and China Water and Power Press. Production and Hosting by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/). Keywords: Aquatic Base System; Harmonization of humans and rivers; Pan-River-Basin; River contribution rate; Water transfer 1. Emergence of Pan-River-Basin A river basin (or watershed) is the area of land where surface water, including rain, melting snow, or ice, converges to a single point at a lower elevation, usually the exit of the basin. From the exit, the water joins another water body, such as a river, lake, reservoir, estuary, wetland, or the ocean. -
On China's Rivers
102 A The “Last Report” On China’s Rivers Executive Summary By Bo Li, Songqiao Yao, Yin Yu and Qiaoyu Guo English Translation released in March 2014 This report is issued jointly by the following initiating and supporting organizations: Initiating organizations: Friends of Nature Institute of Public & Environmental Affairs Green Watershed SHAN SHUI Chengdu Urban Rivers Association Supported by: Nature University Xiamen Green Cross Association Huaihe River Eco-Environmental Science Research Center Green Zhejiang Saunders’ Gull Conservation Society of Panjin City Green Panjin Eco Canton EnviroFriends Institute of Environmental Science and Technology Dalian Environmental Protection Volunteers Association Green Stone Environmental Action Network Greenovation Hub Wild China Film English translation support from: China Environment Forum, Woodrow Wilson Center 1 1 First Bend of the Yangtze River FOREWORD In January 2013, the third year of China’s Twelfth • Reduce coal consumption as a percentage of prima- Five-Year Plan, the State Council released its 12th ry energy to below 65% by 2017; and, Five-Year Plan for Energy Development1, which • Construct 160 GW of hydropower capacity and to included targets that aim to shift China’s energy mix raise nationwide hydropower capacity to 290 GW. to one that pollutes less yet still fuels the country’s growing energy needs. Specifically, by 2015 the Plan If the Plan’s hydropower targets are to be met, by proposes to: 2015, nationwide conventional hydropower installed capacity will reach 48% of the technically exploitable • Increase the proportion of non-fossil fuels in overall hydropower potential, and 72% of the economically primary energy use to 11.4 percent; recoverable potential. -
Earthquake Hazards and Large Dams in Western China
Earthquake Hazards and Large Dams in Western China A Probe International Study By JOHN JACKSON April 2012 PROBE INTERNATIONAL EDITOR: PATRICIA ADAMS John Jackson is a pseudonym for a geologist with detailed knowledge of western China who wishes to remain anonymous to protect his sources. TABLE OF CONTENTS EXECUTIVE SUMMARY Page 1 INTRODUCTION Page 2 ANALYSIS Page 3 DISCUSSION Page 4 CONCLUSION Page 10 ENDNOTES Page 11 RESOURCES Page 14 APPENDIX A Page 16 − TABLE 1: Summary of ziyuan_b dam database for Page 16 selected rivers in western China − TABLE 2: Summary of U.S. Geological Survey Page 17 (USGS) earthquake database, 1973 – 2011 − TABLE 3: Percentage of total dams in each seismic Page 18 hazard zone for selected rivers in western China − TABLE 4: Percentage of total megawatt (MW) Page 19 capacity in each seismic hazard zone for each river − TABLE 5: Estimated number of dams completed and under construction before 2004, as of 2011, and the Page 20 percentage increase − TABLE 6: Incidences of RIS resulting in damage to dams and other structures, 1937 – 1981 Page 21 APPENDIX B Page 22 − FIGURE 1: Seismic hazard map showing dams Page 22 and major earthquake epicenters in western China Page 23 − FIGURE 2: Map of major dams in China (map "ziyuan_b") Page 24 − FIGURE 3: Geological Map of Nujiang, Lancang, and Jinsha River area Page 25 − FIGURE 4: Present-day crustal motion within the Tibetan Plateau inferred from GPS measurements Page 26 − FIGURE 5: Proximity of large dams to seismic hazard zones and shallow (< 10 km) earthquakes in western China 0 Executive Summary By constructing more than 130 large dams in a region of known high seismicity, China is embarking on a major experiment with potentially disastrous consequences for its economy and its citizens. -
The Water Balance of China and Its Large River Basins
Hydrology for the Water Management of Large Riva- Basins (Proceedings of the Vienna Symposium, August 1991). IAHS Publ. no. 201, 1991. THE WATER BALANCE OF CHINA AND ITS LARGE RIVER BASINS LIU GUOWEI AND GUI YUENG Nanjing Institute of Hydrology and Water Resources China ABSTRACT The Yangtze River, Yellow River and other five large river basins are the largest ones in China, with a total area amount ing to about 4 333 687 km2 and covering both humid and arid/semi- arid regions. Based on the computation of atmospheric vapour transport, precipitation, évapotranspiration and runoff, water bal ance models for the whole country and its seven large river basins have already been developed. Through analyses with the models, some characteristics of hydrologie cycles in the river basins, includ ing the origins and routes of atmospheric moisture flux, the water circulation coefficients, etc., have been determined. The results provide a hydrologie basis for water resources assessment and management in China. INTRODUCTION China is located in the East Asian monsoon region, where the hydrologie cycle presents a monsoon climate regime. Every year in May, with the monsoon onset, the rainy season begins in the region south of 25 °N in China. During June to July, the rain band advances to the south of 35°N, and in the whole country the rainy season has developed by August. From November to March of the next year, it is a dry season, and there is a transient season from April to September. The whole country can be divided into three hydrologic-climatic zones: humid, semi-arid and arid zone.