Earthquake Hazards and Large Dams in Western China
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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. -
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. -
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. -
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. -
Coal, Water, and Grasslands in the Three Norths
Coal, Water, and Grasslands in the Three Norths August 2019 The Deutsche Gesellschaft für Internationale Zusammenarbeit (GIZ) GmbH a non-profit, federally owned enterprise, implementing international cooperation projects and measures in the field of sustainable development on behalf of the German Government, as well as other national and international clients. The German Energy Transition Expertise for China Project, which is funded and commissioned by the German Federal Ministry for Economic Affairs and Energy (BMWi), supports the sustainable development of the Chinese energy sector by transferring knowledge and experiences of German energy transition (Energiewende) experts to its partner organisation in China: the China National Renewable Energy Centre (CNREC), a Chinese think tank for advising the National Energy Administration (NEA) on renewable energy policies and the general process of energy transition. CNREC is a part of Energy Research Institute (ERI) of National Development and Reform Commission (NDRC). Contact: Anders Hove Deutsche Gesellschaft für Internationale Zusammenarbeit (GIZ) GmbH China Tayuan Diplomatic Office Building 1-15-1 No. 14, Liangmahe Nanlu, Chaoyang District Beijing 100600 PRC [email protected] www.giz.de/china Table of Contents Executive summary 1 1. The Three Norths region features high water-stress, high coal use, and abundant grasslands 3 1.1 The Three Norths is China’s main base for coal production, coal power and coal chemicals 3 1.2 The Three Norths faces high water stress 6 1.3 Water consumption of the coal industry and irrigation of grassland relatively low 7 1.4 Grassland area and productivity showed several trends during 1980-2015 9 2. -
Assessment of Japanese and Chinese Flood Control Policies
京都大学防災研究所年報 第 53 号 B 平成 22 年 6 月 Annuals of Disas. Prev. Res. Inst., Kyoto Univ., No. 53 B, 2010 Assessment of Japanese and Chinese Flood Control Policies Pingping LUO*, Yousuke YAMASHIKI, Kaoru TAKARA, Daniel NOVER**, and Bin HE * Graduate School of Engineering ,Kyoto University, Japan ** University of California, Davis, USA Synopsis The flood is one of the world’s most dangerous natural disasters that cause immense damage and accounts for a large number of deaths and damage world-wide. Good flood control policies play an extremely important role in preventing frequent floods. It is well known that China has more than 5000 years history and flood control policies and measure have been conducted since the time of Yu the great and his father’s reign. Japan’s culture is similar to China’s but took different approaches to flood control. Under the high speed development of civil engineering technology after 1660, flood control was achieved primarily through the construction of dams, dykes and other structures. However, these structures never fully stopped floods from occurring. In this research, we present an overview of flood control policies, assess the benefit of the different policies, and contribute to a better understanding of flood control. Keywords: Flood control, Dujiangyan, History, Irrigation, Land use 1. Introduction Warring States Period of China by the Kingdom of Qin. It is located in the Min River in Sichuan Floods are frequent and devastating events Province, China, near the capital Chengdu. It is still worldwide. The Asian continent is much affected in use today and still irrigates over 5,300 square by floods, particularly in China, India and kilometers of land in the region. -
Sichuan Province Sìchuān Shěng 四川省 81.27 Million Est
◀ Shikumen Comprehensive index starts in volume 5, page 2667. Sichuan Province Sìchuān Shěng 四川省 81.27 million est. 2007 pop. 485,000 square km Sichuan Province, renowned worldwide for its Sichuan) had fully developed. In that year the armies of cuisine, is one of China’s agricultural heart- the Qin state from northern China incorporated the ter- lands, thanks in part to the 2,300-year-old ir- ritories of Ba and Shu into the Qin empire, although the rigation system still in use. The province, one names of the two kingdoms are still used to refer to the Chongqing area (part of Sichuan until a 1997 administra- of China’s most populous, played a key role tive reorganization) and the Chengdu area, respectively. in the early years of Deng Xiaoping’s reform Governors of Qin established a regional capital at program to decentralize the economy. The 12 Chengdu, and Qin engineers built the Dujiangyan wa- May 2008 earthquake killed more than seventy terworks on the Min River west of the city, making the thousand people in Sichuan. Chengdu Plain a productive agricultural center. However, Sichuan’s geography—surrounded by mountain ranges and the Yangzi (Chang) River gorges—kept it relatively ichuan (Szechwan) Province is located on the up- isolated from the rest of China. The Qin constructed a per reaches of the Yangzi (Chang) River. With a highway from their capital near the Huang (Yellow) River land area of 485,000 square kilometers (slightly southwest into Sichuan, carving ledges into the steep smaller than Spain) and an estimated population of 81.27 mountain slopes. -
China's Water Security: Current Status, Emerging Challenges and Future
Environmental Science & Policy 54 (2015) 106–125 Contents lists available at ScienceDirect Environmental Science & Policy jo urnal homepage: www.elsevier.com/locate/envsci Review China’s water security: Current status, emerging challenges and future prospects a,b, Yong Jiang * a Department of Integrated Water Systems and Governance, UNESCO-IHE Institute for Water Education, Westvest 7, 2611AX Delft, The Netherlands b Institute for Environmental Studies, VU University Amsterdam, De Boelelaan 1085, 1081HV Amsterdam, The Netherlands A R T I C L E I N F O A B S T R A C T Article history: China has been facing increasingly severe water scarcity that seriously threatens the socio-economic Received 17 January 2015 development and its sustainability of this country. This paper is intended to analyze and assess the water Received in revised form 3 June 2015 security of China. It first attempts to characterize the current status of water security within a risk-based, Accepted 4 June 2015 integrated framework that encompasses five key aspects critical to water sustainability, including water Available online 10 July 2015 availability, water use patterns, wastewater generation and pollution control, water institutions and management, and health of aquatic systems and societal vulnerability. Based on the above assessment, Keywords: the paper then analyzes emerging challenges for water security brought by climate change, population Water resources growth and rapid urbanization, and the water-food-energy nexus. In the end, the paper discusses China’s Water security future prospects on water security, including current achievements, government actions and policy Water use Wastewater initiatives, and recommendations for management improvement aimed at increasing water security. -
Sichuan Basin
Sichuan Basin Spread across the vast territory of China are hundreds of basins, where developed sedimentary rocks originated from the Paleozoic to the Cenozoic eras, covering over four million square kilometers. Abundant oil and gas resources are entrapped in strata ranging from the eldest Sinian Suberathem to the youngest quaternary system. The most important petroliferous basins in China include Tarim, Junggar, Turpan, Qaidam, Ordos, Songliao, Bohai Bay, Erlian, Sichuan, North Tibet, South Huabei and Jianghan basins. There are also over ten mid- to-large sedimentary basins along the extensive sea area of China, with those rich in oil and gas include the South Yellow Sea, East Sea, Zhujiangkou and North Bay basins. These basins, endowing tremendous hydrocarbon resources with various genesis and geologic features, have nurtured splendid civilizations with distinctive characteristics portrayed by unique natural landscape, specialties, local culture, and the people. In China, CNPC’s oil and gas operations mainly focus in nine petroliferous basins, namely Tarim, Junggar, Turpan, Ordos, Qaidam, Songliao, Erlian, Sichuan, and the Bohai Bay. Located within Sichuan Province and Chongqing Municipality in Southwest Featuring the most typical terrain, the southernmost China, Sichuan Basin is close to Qinghai- position, and the lowest altitude among China’s big Tibet Plateau in the west, Qinling Mountains basins, Sichuan Basin comprises the central and and the Loess Plateau in the north, the eastern portions of Sichuan Province as well as the mountainous regions in the western Hunan greater part of Chongqing Municipality. Located at and Hubei in the east, and Yunnan-Guizhou the upper reaches of the Yangtze River as the largest Plateau in the south. -
World's Top 10 Rivers at Risk
World’s top 10 rivers at risk World’s top 10 rivers at risk Wong, CM, Williams, CE, Pittock, J, Collier, U and P Schelle. March 2007. World’s top 10 rivers at risk. WWF International. Gland, Switzerland. This report was designed by The Clarion Portfolio. Cover image: Fisherman on Zhangdu Lake, the project area of the WWF HSBC Yangtze Programme, Hubei Province, China. © WWF-Canon / Yifei ZHANG Executive Summary Executive Summary “What makes a river so restful to people is that it doesn’t have any doubt - it is sure to get where it is going, and it doesn’t want to go Hal Boyle anywhere else.” Pulitzer prize-winning columnist Perhaps there was a time when that was true, but no longer. Even the greatest of the world’s rivers can no longer be assured of reaching the sea unhindered. These days the Rio Grande/Rio Bravo River, on the border of the U.S. and Mexico, often fails to reach the Gulf of Mexico, its strength sapped by dams and irrigation works diverting water to farmers’ fi elds and city water supplies. The Indus, the Nile, the Murray-Darling, the Colorado, these are but a few of the once mighty rivers that now struggle to touch the ocean. In fact, water extraction is only one of the daunting challenges that a river faces as it makes its way to its terminus. Dams and channelization destroy habitats, cut rivers off from their fl oodplains, and alter the natural ebb and fl ow on which a river’s plants and animals depend. -
Exploring the Relationship Between the Arid Valley Boundary's
International Journal of Geo-Information Article Exploring the Relationship between the Arid Valley Boundary’s Displacement and Climate Change during 1999–2013 in the Upper Reaches of the Min River, China Yalin Guo, Qing Wang * and Min Fan School of Environment and Resource, Southwest University of Science and Technology, Mianyang 621010, Sichuan, China; [email protected] (Y.G.); fi[email protected] (M.F.) * Correspondence: [email protected]; Tel.: +86-28-6608-9459 Academic Editor: Wolfgang Kainz Received: 2 March 2017; Accepted: 24 April 2017; Published: 6 May 2017 Abstract: The arid valley is a unique type of ecological fragile landscape in the Hengduan Mountain Area, China. The boundary of the arid valley is one of the response indicators to mountainous climate change. Based on the meteorological data from 1999 to 2013 and the SPOT remote sensing images in 1999 and 2013 this study explored the response characteristics of the arid valley boundary to regional climate change in the upper reaches of the Min River in the Hengduan Mountains. The results are as follows: (1) During 1999–2013, the temperature, precipitation, and evaporation increased, and the sunshine duration and relative humidity showed decreasing trends at the rates of 0.008 ◦C/a, 2.25 mm/a, 5.51 mm/a, −8.72 h/a, and −0.19%/a, respectively. Meanwhile, the climate showed the warm-dry tendency in the southern region and the warm-humid tendency in the central and northern areas. (2) On the whole, the arid valley boundary mainly distributed between 1601–3200 m and moved downward to 2428 m at the speed of −0.76 ± 0.26 m/a along with global warming. -
Carleton College 1966 50Th Reunion Newsletter
ISSUE 8: SEPTEMBER 2015 Carleton College 1966 50th Reunion Newsletter RATIONALE FOR FURTHER READING. 1. What was the cost to one of our classmates when he critiqued comments made by President Nason in the Carletonian? 2. The term ‘fatuous blather’ was made famous by Content this individual. 3. Like many of us, Joe DuBray, a long-time 1. An insight into the nature of President Nason’s com- contributor to Carleton, responded somewhat ments to the Carletonian regarding an issue that he felt was critical for the Carleton community. At least one of reluctantly to the request to make a more our classmates took him to task on that message. significant contribution. Read about his 2. Joe DuBray demonstrates how, with help from College thoughts and eventual outcomes regarding this staff, he was able to match his personal interests in indige- request. nous languages and their preservation and his giving to 4. Learn about Hinckley’s recent trip to China. Carleton. 5. Why is Sichuan food healthy? What is a nak? 3. Tom Hinckley spent three weeks in Sichuan Province in 6. Who or what is the Earth Liberation Front? China with a faculty colleague in Anthropology and two former students. This was his 10th trip to that part of 7. Go to the Reunion Web Page and Stories and China and is part of a long-term engagement with two mi- learn about the classmate who was an nority communities in the mountains of Sichuan. ambassador to Tanzania and Jordan! Carleton: Then then, still not an easy choice for my family.