World's Top 10 Rivers at Risk
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
INDUS DELTA, PAKISTAN: Economic Costs of Reduction in Freshwater Flows
water allocationdecisions. factored intoriverbasinplanning,or benefits of water-basedecosystemsarerarely economic users ofwater.Yettheeconomic schemes, Pakistan’secosystems,too,are hydropower dams, reservoirs,irrigationand as water tolarge-scale,commercialusessuch imperative that favours theallocationof Contrary tothedominantdevelopment economically norecologicallyoptimal. decisions beingmadethatareneither needs has oftenledtowaterallocation Failure torecognisedownstreamecosystem heavily byupstreamwaterabstraction. end of rivers,havebeenimpactedmost the at lie and marineregions,becausethey Coastal ecosystems. needs ofdownstream many cases, left insufficientflowtomeetthe of large volumesofwaterfromrivershas,in particular there isconcernthattheabstraction exacting a heavytollontheenvironment.In This impressive irrigationsystemis,however, world. the irrigated torain-fedlandratioin highest the farmland, affordingPakistan system feedsmorethan15millionhectaresof than 1.65 million km(IRIN2001).The more watercourses witharunninglengthof 89,000 conveyance lengthof57,000km,and head works, 43maincanalswitha or barrages 19 three majorstoragereservoirs, comprises Pakistan’s vastirrigationnetwork Pakistan Water-based developmentsin flows reduction infreshwater economic costsof INDUS DELTA,PAKISTAN: VALUATION #5:May2003 CASE STUDIESINWETLAND Integrating Wetland Economic Values into River Basin Management Managing freshwater flows in the The economic costs and losses arising from Indus River such omissions can be immense, and often The Indus River has -
Landscape Analysis of Geographical Names in Hubei Province, China
Entropy 2014, 16, 6313-6337; doi:10.3390/e16126313 OPEN ACCESS entropy ISSN 1099-4300 www.mdpi.com/journal/entropy Article Landscape Analysis of Geographical Names in Hubei Province, China Xixi Chen 1, Tao Hu 1, Fu Ren 1,2,*, Deng Chen 1, Lan Li 1 and Nan Gao 1 1 School of Resource and Environment Science, Wuhan University, Luoyu Road 129, Wuhan 430079, China; E-Mails: [email protected] (X.C.); [email protected] (T.H.); [email protected] (D.C.); [email protected] (L.L.); [email protected] (N.G.) 2 Key Laboratory of Geographical Information System, Ministry of Education, Wuhan University, Luoyu Road 129, Wuhan 430079, China * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel: +86-27-87664557; Fax: +86-27-68778893. External Editor: Hwa-Lung Yu Received: 20 July 2014; in revised form: 31 October 2014 / Accepted: 26 November 2014 / Published: 1 December 2014 Abstract: Hubei Province is the hub of communications in central China, which directly determines its strategic position in the country’s development. Additionally, Hubei Province is well-known for its diverse landforms, including mountains, hills, mounds and plains. This area is called “The Province of Thousand Lakes” due to the abundance of water resources. Geographical names are exclusive names given to physical or anthropogenic geographic entities at specific spatial locations and are important signs by which humans understand natural and human activities. In this study, geographic information systems (GIS) technology is adopted to establish a geodatabase of geographical names with particular characteristics in Hubei Province and extract certain geomorphologic and environmental factors. -
Estimation of Paleo-Discharge of the Lost Saraswati River, North West India
EGU2020-21212 https://doi.org/10.5194/egusphere-egu2020-21212 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Estimation of paleo-discharge of the lost Saraswati River, north west India Zafar Beg, Kumar Gaurav, and Sampat Kumar Tandon Indian Institute of Science Education and Research Bhopal, Earth and Environment Sciences, India ([email protected], [email protected], [email protected] ) The lost Saraswati has been described as a large perennial river which was 'lost' in the desert towards the end of the 'Indus-Saraswati civilisation'. It has been suggested that this paleo river flowed in the Sutlej-Yamuna interfluve, parallel to the present-day Indus River. Today, in this interfluve an ephemeral river- the Ghaggar flows along the abandoned course of the ‘lost’ Saraswati River. We examine the hypothesis given by Yashpal et al. (1980) that two Himalayan-fed rivers Sutlej and Yamuna were the tributaries of the lost Saraswati River, and constituted the bulk of its paleo-discharge. Subsequently, the recognition of the occurrence of thick fluvial sand bodies in the subsurface and the presence of a large number of Harappan sites in the interfluve region have been used to suggest that the Saraswati River was a large perennial river. Further, the wider course of about 4-7 km recognised from satellite imagery of Ghaggar-Hakra belt in between Suratgarh and Anupgarh in the Thar strengthens this hypothesis. In this study, we have developed a methodology to estimate the paleo-discharge and paleo- width of the lost Saraswati River. -
How Geography "Mapped" East Asia, Part One: China by Craig Benjamin, Big History Project, Adapted by Newsela Staff on 01.26.17 Word Count 1,354 Level 1020L
How Geography "Mapped" East Asia, Part One: China By Craig Benjamin, Big History Project, adapted by Newsela staff on 01.26.17 Word Count 1,354 Level 1020L TOP: The Stalagmite Gang peaks at the East Sea area of Huangshan mountain in China. Photo by: Education Images/UIG via Getty Images MIDDLE: Crescent Moon Lake and oasis in the middle of the desert. Photo by: Tom Thai, Flickr. BOTTOM: Hukou Waterfall in the Yellow River. Photo by: Wikimedia The first in a two-part series In what ways did geography allow for the establishment of villages and towns — some of which grew into cities — in various regions of East Asia? What role did climate play in enabling powerful states and civilizations to appear in some areas while other locations remained better suited for a nomadic lifestyle? Let's begin to answer these questions with a story about floods in China. China's two great rivers — the Yangtze and the Yellow — have flooded regularly for as long as we can measure in the historical and geological record. Catastrophic floodwaters This article is available at 5 reading levels at https://newsela.com. Nothing can compare, though, to the catastrophic floods of August 19, 1931. The Yangtze river rose an astonishing 53 feet above its normal level in just one day. It unleashed some of the most destructive floodwaters ever seen. The floods were caused by a "perfect storm" of conditions. Monsoon rains, heavy snowmelt, and unexpected rains pounded huge areas of southern China. All this water poured into the Yangtze. The river rose and burst its banks for hundreds of miles. -
IUCN TECHNICAL EVALUATION MOUNT SANQINGSHAN NATIONAL PARK (CHINA) – ID No. 1292
WORLD HERITAGE NOMINATION – IUCN TECHNICAL EVALUATION MOUNT SANQINGSHAN NATIONAL PARK (CHINA) – ID No. 1292 1. DOCUMENTATION i) Date nomination received by IUCN: April 2007 ii) Additional information offi cially requested from and provided by the State Party: IUCN requested supplementary information on 14 November 2007 after the fi eld visit and on 19 December 2007 after the fi rst IUCN World Heritage Panel meeting. The fi rst State Party response was offi cially received by the World Heritage Centre on 6 December 2007, followed by two letters from the State Party to IUCN dated 25 January 2008 and 28 February 2008. iii) UNEP-WCMC Data Sheet: 11 references (including nomination document) iv) Additional literature consulted: Dingwall, P., Weighell, T. and Badman, T. (2005) Geological World Heritage: A Global Framework Strategy. IUCN, Gland, Switzerland; Hilton-Taylor, C. (compiler) (2006) IUCN Red List of Threatened Species. IUCN, Gland, Switzerland; IUCN (ed.) (2006) Enhancing the IUCN Evaluation Process of World Heritage Nominations: A Contribution to Achieving a Credible and Balanced World Heritage List. IUCN, Gland, Switzerland; Management Committee (2007) Abstract of the Master Plan of Mount Sanqingshan National Park. Mount Sanqingshan National Park; Management Committee (2007) Mount Sanqingshan International Symposium on Granite Geology and Landscapes. Mount Sanqingshan National Park; Migon, P. (2006) Granite Landscapes of the World. Oxford University Press; Migon, P. (2006) Sanqingshan – The Hidden Treasure of China. Available online; Peng, S.L., Liao, W.B., Wang, Y.Y. et al. (2007) Study on Biodiversity of Mount Sanqingshan in China. Science Press, Beijing; Shen, W. (2001) The System of Sacred Mountains in China and their Characteristics. -
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. -
The Geographic, Geological and Oceanographic Setting of the Indus River
16 The Geographic, Geological and Oceanographic Setting of the Indus River Asif Inam1, Peter D. Clift2, Liviu Giosan3, Ali Rashid Tabrez1, Muhammad Tahir4, Muhammad Moazam Rabbani1 and Muhammad Danish1 1National Institute of Oceanography, ST. 47 Clifton Block 1, Karachi, Pakistan 2School of Geosciences, University of Aberdeen, Aberdeen AB24 3UE, UK 3Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA 4Fugro Geodetic Limited, 28-B, KDA Scheme #1, Karachi 75350, Pakistan 16.1 INTRODUCTION glaciers (Tarar, 1982). The Indus, Jhelum and Chenab Rivers are the major sources of water for the Indus Basin The 3000 km long Indus is one of the world’s larger rivers Irrigation System (IBIS). that has exerted a long lasting fascination on scholars Seasonal and annual river fl ows both are highly variable since Alexander the Great’s expedition in the region in (Ahmad, 1993; Asianics, 2000). Annual peak fl ow occurs 325 BC. The discovery of an early advanced civilization between June and late September, during the southwest in the Indus Valley (Meadows and Meadows, 1999 and monsoon. The high fl ows of the summer monsoon are references therein) further increased this interest in the augmented by snowmelt in the north that also conveys a history of the river. Its source lies in Tibet, close to sacred large volume of sediment from the mountains. Mount Kailas and part of its upper course runs through The 970 000 km2 drainage basin of the Indus ranks the India, but its channel and drainage basin are mostly in twelfth largest in the world. Its 30 000 km2 delta ranks Pakiistan. -
Transboundary River Basin Overview – Salween
0 [Type here] Irrigation in Africa in figures - AQUASTAT Survey - 2016 Transboundary River Basin Overview – Salween Version 2011 Recommended citation: FAO. 2011. AQUASTAT Transboundary River Basins – Salween River Basin. Food and Agriculture Organization of the United Nations (FAO). Rome, Italy The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views or policies of FAO. FAO encourages the use, reproduction and dissemination of material in this information product. Except where otherwise indicated, material may be copied, downloaded and printed for private study, research and teaching purposes, or for use in non-commercial products or services, provided that appropriate acknowledgement of FAO as the source and copyright holder is given and that FAO’s endorsement of users’ views, products or services is not implied in any way. All requests for translation and adaptation rights, and for resale and other commercial use rights should be made via www.fao.org/contact-us/licencerequest or addressed to [email protected]. -
Water Wars: the Brahmaputra River and Sino-Indian Relations
U.S. Naval War College U.S. Naval War College Digital Commons CIWAG Case Studies 10-2013 Water Wars: The Brahmaputra River and Sino-Indian Relations Mark Christopher Follow this and additional works at: https://digital-commons.usnwc.edu/ciwag-case-studies Recommended Citation Christopher, Mark, "MIWS_07 - Water Wars: The Brahmaputra River and Sino-Indian Relations" (2013). CIWAG Case Studies. 7. https://digital-commons.usnwc.edu/ciwag-case-studies/7 This Book is brought to you for free and open access by U.S. Naval War College Digital Commons. It has been accepted for inclusion in CIWAG Case Studies by an authorized administrator of U.S. Naval War College Digital Commons. For more information, please contact [email protected]. Draft as of 121916 ARF R W ARE LA a U nd G A E R R M R I E D n o G R R E O T U N P E S C U N E IT EG ED L S OL TA R C TES NAVAL WA Water Wars: The Brahmaputra River and Sino-Indian Relations Mark Christopher United States Naval War College Newport, Rhode Island Water Wars: The Brahmaputra River and Sino-Indian Relations Mark Christopher Center on Irregular Warfare & Armed Groups (CIWAG) US Naval War College, Newport, RI [email protected] CHRISTOPHER: WATER WARS CIWAG Case Studies Bureaucracy Does Its Thing (in Afghanistan) – Todd Greentree Operationalizing Intelligence Dominance – Roy Godson An Operator’s Guide to Human Terrain Teams – Norman Nigh Organizational Learning and the Marine Corps: The Counterinsurgency Campaign in Iraq – Richard Shultz Piracy – Martin Murphy Reading the Tea Leaves: Proto-Insurgency in Honduras – John D. -
Effects of Reflective Warning Markers on Wildlife
Effects of reflective warning markers on wildlife Yi-Hao Fang1,2,3,4,5,*, Ying Gao1,2,3,4,5,*, Yin Yang1,2,3,4,6, Kun Tan1,2,3,4, Yan-Peng Li1,2,3,4, Guo-Peng Ren1,2,3,4, Zhi-Pang Huang1,2,3,4, Liang-Wei Cui2,3,4,5 and Wen Xiao1,2,3,4 1 Institute of Eastern-Himalaya Biodiversity Research, Dali University, Dali, Yunnan, China 2 Collaborative Innovation Center for Biodiversity and Conservation in the Three Parallel Rivers Region of China, Dali University, Dali, Yunnan, China 3 The Provincial Innovation Team of Biodiversity Conservation and Utility of the Three Parallel Rivers Region from Dali University, Dali University, Dali, Yunnan, China 4 The Key Laboratory of Yunnan Education Department on Er'hai Catchment Conservation and Sustainable Development, Dali University, Dali, Yunnan, China 5 Faculty of Biodiversity Conservation and Utilization, Southwest Forestry University, Kunming, Yunnan, China 6 School of Archaeology & Anthropology, Australian National University, Canberra, Australia * These authors contributed equally to this work. ABSTRACT Light pollution has become one of the top issues in environmental pollution, especially concerning how secondary light pollution, such as from traffic reflective materials, influences animal distribution and behavior. In this study, 15 camera traps were set up at sites with or without reflective warning markers (RWM) in coniferous forests on Cangshan Mountain located in Dali Prefecture, China. The results showed that the number of independent photographs and species at sites without RWMs were significantly higher than those at sites with RWMs. Significant differences were found between daytime and nighttime composition of bird species and non-flying mammals between two sites. -
Holocene Environmental Archaeology of the Yangtze River Valley in China: a Review
land Review Holocene Environmental Archaeology of the Yangtze River Valley in China: A Review Li Wu 1,2,*, Shuguang Lu 1, Cheng Zhu 3, Chunmei Ma 3, Xiaoling Sun 1, Xiaoxue Li 1, Chenchen Li 1 and Qingchun Guo 4 1 Provincial Key Laboratory of Earth Surface Processes and Regional Response in the Yangtze-Huaihe River Basin, School of Geography and Tourism, Anhui Normal University, Wuhu 241002, China; [email protected] (S.L.); [email protected] (X.S.); [email protected] (X.L.); [email protected] (C.L.) 2 State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China 3 School of Geograpy and Ocean Science, Nanjing University, Nanjing 210023, China; [email protected] (C.Z.); [email protected] (C.M.) 4 School of Environment and Planning, Liaocheng University, Liaocheng 252000, China; [email protected] * Correspondence: [email protected] Abstract: The Yangtze River Valley is an important economic region and one of the cradles of human civilization. It is also the site of frequent floods, droughts, and other natural disasters. Conducting Holocene environmental archaeology research in this region is of great importance when studying the evolution of the relationship between humans and the environment and the interactive effects humans had on the environment from 10.0 to 3.0 ka BP, for which no written records exist. This Citation: Wu, L.; Lu, S.; Zhu, C.; review provides a comprehensive summary of materials that have been published over the past Ma, C.; Sun, X.; Li, X.; Li, C.; Guo, Q. -
Water Conflict Pathways and Peacebuilding Strategies by David Michel
PEACEWORKS Water Conflict Pathways and Peacebuilding Strategies By David Michel NO. 164 | AUGUST 2020 NO. 164 | AUGUST 2020 ABOUT THE REPORT This report explores water-related conflict pathways and articulates potential peace- building strategies to mitigate conflict risks. The report is grounded in a survey of the ECONOMICS & ENVIRONMENT academic literature on natural resources conflict, case studies of three major basins, and participant interviews and documentary analyses of water diplomacy processes. ABOUT THE AUTHOR David Michel is a senior researcher with the Stockholm International Peace Research Institute. He previously served as a senior manager at the Stockholm International Water Institute. He has over twenty years of experience working with governments, civil society, and the private sector to build cooperative solutions to policy challenges posed by global environmental change. Cover photo: A woman walks along a dry lake bed near the Rawal Dam in Pakistan on June 22, 2018. (Photo by B. K. Bangash/AP) The views expressed in this report are those of the author alone. They do not necessarily reflect the views of the United States Institute of Peace. An online edition of this and related reports can be found on our website (www.usip.org), together with additional information on the subject. © 2020 by the United States Institute of Peace United States Institute of Peace 2301 Constitution Avenue NW Washington, DC 20037 Phone: 202.457.1700 Fax: 202.429.6063 E-mail: [email protected] Web: www.usip.org Peaceworks No. 164. First published 2020. ISBN: 978-1-60127-810-4 Contents Water Insecurity and Conflict Risks 3 Water Conflict Pathways 7 Case Study: The Indus River Basin 10 Case Study: Mali 14 Case Study: Myanmar 18 Water Governance and Water Diplomacy 22 Peacebuilding Strategies for Water Resources Conflicts 26 USIP.ORG 1 Summary Growing populations and economies, unsustainable management practices, and mounting environmental pressures are exerting increasing strains on the world’s vital freshwater resources.