DOCSLIB.ORG

DRAINAGE BASIN of the ARAL SEA and OTHER TRANSBOUNDARY SURFACE WATERS in CENTRAL ASIA Chapter 3

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
DRAINAGE BASIN of the ARAL SEA and OTHER TRANSBOUNDARY SURFACE WATERS in CENTRAL ASIA Chapter 3 68 DRAINAGE BASIN OF THE ARAL SEA AND OTHER TRANSBOUNDARY SURFACE WATERS IN CENTRAL ASIA Chapter 3 ARAL SEA AND OTHER WATERS IN CENTRAL ASIA 69 71 AMU DARYA RIVER BASIN 75 ZERAVSHAN RIVER BASIN 76 SYR DARYA RIVER BASIN 83 ARAL SEA 84 CHU-TALAS RIVER BASINS 89 ILI RIVER BASIN 91 LAKE BALQASH 91 MURGAB RIVER BASIN 91 TEJEN RIVER BASIN Chapter 3 70 ARAL SEA AND OTHER WATERS IN CENTRAL ASIA This chapter deals with major transboundary rivers in Central Asia which have a desert sink, or discharge either into one of the rivers (or their tributaries) or the Aral Sea or an another enclosed lake. It also includes lakes located within the basin of the Aral Sea. Practically all of the renewable water resources in this area are used predominantly for irrigation, and the national economies are developing under conditions of increasing freshwater shortages. TRANSBOUNDARY WATERS IN THE BASIN OF THE ARAL SEA AND OTHER TRANSBOUNDARY SURFACE WATERS IN CENTRAL ASIA1 Basin/sub-basin(s) Total area (km²) Recipient Riparian countries Lakes in the basin Amu Darya …2 Aral Sea AF, KG, TJ, UZ, TM - Surkhan Darya 13,500 Amu Darya TJ, UZ - Kafirnigan 11,590 Amu Darya TJ, UZ - Pyanj 113,500 Amu Darya AF, TJ -- Bartang … Pyanj AF, TJ -- Pamir … Pyanj AF, TJ - Vakhsh 39,100 Amu Darya KG, TJ Aral Sea Zeravshan …2 Desert sink TJ, UZ Syr Darya …2 Aral Sea KZ, KG, TJ, UZ - Naryn … Syr Darya KG, UZ - Kara Darya 28,630 Syr Darya KG, UZ - Chirchik 14,240 Syr Darya KZ, KG, UZ -Chatkal 7,110 Chirchik KG, UZ Chu 62,500 Desert sink KZ, KG Talas 52,700 Desert sink KZ, KG Assa … Desert sink KZ, KG Ili 413,000 Lake Balqash CN, KZ Lake Balqash Murgab 46,880 Desert sink AF, TM - Abikajsar … Murgab AF, TM Tejen 70,260 Desert sink AF, IR, TM 1 The assessment of water bodies in italics was not included in the present publication. 2 The basin area is difficult to determine, see the assessment below. Chapter 3 ARAL SEA AND OTHER WATERS IN CENTRAL ASIA 71 AMU DARYA RIVER BASIN1 Afghanistan, Kyrgyzstan, Tajikistan, Turkmenistan and Uzbekistan share the basin of the Amu Darya River. While some literature sources quote a basin area of up to 534,700 km2, the water divide can only be correctly established in the mountainous part of the basin; therefore many hydrologists refrain from giving figures for the total basin area. A N 40o S T Y Z R G K Y Suu yzyl Samarqand K U Zeravshan Z Lake Karakul B C E TAJIKISTAN Dushanbe H K M urghab I I Nurek g a n Lake y Reservoir a N S r t Sarez ar A a B k n s D A T a u n g a i h n A k r i h r f u s a ir S h m N K a k P a V arya mu Da j akhan D A rya anj an V Py Py A N 75o S T Kilometres AFGHANISTAN K I The boundaries and names shown and the designations used on this map A 0 50 100 150 do not imply official endorsement or acceptance by the United Nations. 70o P UNEP/DEWA/GRID-Europe 2007 Hydrology The confluence of the two transboundary rivers, the ervoir, 10.5 billion m3); therefore, floods often Pyanj and the Vakhsh (see the separate assessment be- occur between the rivers’ confluence and the low), is taken as the beginning of the Amu Darya. Tyuyamuyunsk reservoir on the Amu Darya (7,270 million m3). Downstream of this reservoir, Of these two, only the Vakhsh is regulated (Nurek res- the Amu Darya is fully regulated. Discharge characteristics of the Amu Darya River upstream of the Karakum Canal 3 Qav 1,970 m /s Average for: 1959–2005 Mean monthly values: October – 1,740 m3/s November – 957 m3/s December – 898 m3/s January – 816 m3/s February – 820 m3/s March – 979 m3/s April – 1,670 m3/s May – 2,670 m3/s June – 3,800 m3/s July – 4,500 m3/s August – 3,470 m3/s September – 1,950m3/s Source: Hydrometeorological Service of Uzbekistan. 1 Based on information provided by the State Agency for Environment Protection and Forestry of Kyrgyzstan, the Ministry of Agriculture and Nature Protec- tion of Tajikistan, the Ministry of Nature Protection of Turkmenistan and the State Committee for Nature Protection of Uzbekistan. Chapter 3 72 ARAL SEA AND OTHER WATERS IN CENTRAL ASIA Like other rivers in Central Asia, the Amu Darya is subject Pressure factors, transboundary impact and trends to strong hydraulic processes (e.g. deformation of the river The pressures, transboundary impact and trends for the bed, meandering, bank erosion). transboundary rivers in the Amu Darya River basin are described in the following sections. In general, the joint In addition to the Pyanj and the Vakhsh, a number of other sustainable use and protection of water resources of transboundary waters are located in the Amu Darya basin, these transboundary rivers is a particular challenge for including the Pamir, Kafirnigan, Surkhan Darya and Zer- this region. avshan rivers (assessed separately below). SURKHAN DARYA RIVER2 The Surkhan Darya is a transboundary tributary to the Amu Darya and has its source in Tajikistan. The catchment area is 13,500 km2; the major part of this area is located in Uzbekistan. Hydrology The natural flow of the river is heavily disturbed by water part, the inflow into the Jujnosurkhansk reservoir (Uzbeki- management activities in the catchment area. Whereas stan) is only 74.2 m3/s (see the following table). some 120 m3/s are estimated to originate in the mountain Discharge characteristics of the Surkhan Darya (Uzbekistan) (Inflow into the reservoir; summary values for the Shurchi gauging stations on the Surkhan Darya and the gauging station at the river mouth) 3 Qav 74.2 m /s Average for 1970–2005 Mean monthly values: October – 25.3 m3/s November – 34.4 m3/s December – 42.01 m3/s January – 45.3 m3/s February – 47.6 m3/s March – 72.8 m3/s April – 157 m3/s May – 196 m3/s June – 166 m3/s July – 72.3 m3/s August – 17.2 m3/s September – 15.3 m3/s Source: Hydrometeorological Service of Uzbekistan. KAFIRNIGAN RIVER3 The common border between Tajikistan and Uzbekistan is formed by the Kafirnigan River and it is of some 30 km. Most of the Kafirnigan’s catchment area of 11,590 km2 belongs to Tajikistan. Hydrology The average discharge is on the order of 170 m3/s. As a As a consequence of heavy rainfall, mudflow has rule, the maximum discharge occurs in May (Tartki gaug- a considerable impact on the ecological regime ing station, located some 50 km upstream of the river and the safe operation of hydrotechnical mouth, upstream catchment area some 9,780 km2). installations. 2 Source: Environmental Performance Review of Tajikistan, UNECE, 2004. 3 Source: Environmental Performance Review of Tajikistan, UNECE, 2004. Chapter 3 ARAL SEA AND OTHER WATERS IN CENTRAL ASIA 73 Discharge characteristics of the Kafirnigan at Tartki (Tajikistan) 3 Qav 169 m /s Average for 1929–2005 Mean monthly values: October – 60.0 m3/s November – 62.9 m3/s December – 63.1 m3/s January – 59.6 m3/s February – 62.2 m3/s March – 187 m3/s April – 295 m3/s May – 405 m3/s June – 389 m3/s July – 270 m3/s August – 129 m3/s September – 70.1 m3/s Source: Hydrometeorological Service of Uzbekistan. PYANJ RIVER4 Afghanistan and Tajikistan share the catchment area of the Pyanj River, located in the Amu Darya River basin, as shown in the following table. Of the Pyanj’s total catchment area, 107,000 km2 are in the mountains and the rest (6,500 km2) in the lowland part of the catchment area. Sub-basin of the Pyanj River Area Country Country’s share Afghanistan 47,670 km2 42% 113,500 km2 Tajikistan 65,830 km2 58% Source: Hydrometeorological Service of Uzbekistan. Hydrology The Pyanj and Pamir rivers form the bor- der between Afghanistan and Tajikistan. Usually the confluence of the rivers Vakhan Darya (Afghanistan) and Pamir (forming the border between Afghanistan and Tajikistan) is considered as the beginning of the River Pyanj. However, hydrologists consider the source of the Vakhan Darya in Afghanistan as the beginning of the River Pyanj, as the Vakhan Darya is the “natural prolongation” of the Pyanj towards the east. The total length of the Vakhan Darya/Py- anj is 1,137 km; from the confluence of the Vakhan Darya and Pamir, the river is 921 km long. The lake percentage is 0.42%, based on data for 1987. 4 Based on information provided by the Hydrometeorological Service of Uzbekistan. Chapter 3 74 ARAL SEA AND OTHER WATERS IN CENTRAL ASIA Discharge characteristics of the Pyanj River at Nijniy Pyanj (Tajikistan), 35 km upstream of the confluence with the Vakhsh River 3 Qav 1,012 m /s Average for 1965–1992 Mean monthly values: October – 643 m3/s November – 516 m3/s December – 445 m3/s January – 389 m3/s February – 406 m3/s March – 503 m3/s April – 828 m3/s May – 1,290 m3/s June – 2,000 m3/s July – 2,300 m3/s August – 1,960 m3/s September – 1,050 m3/s Source: Hydrometeorological Service of Uzbekistan. Downstream of the confluence of the Vakhan Darya and the Syr Darya basins, the Pyanj catchment area has the follow- Pamir, a number of tributaries join the Pyanj, such as the ing relevant specific features: The Sarez Lake (16.1 km3), Gunt, the Bartang, the Jasgulem, the Vanj and the Kyzylsu formed by an earthquake in the upper part of the Bartang (right-hand-side tributaries), and the Koktsha (a left-hand- River, is a potential threat to the population (some 5 million side tributary which flows exclusively through Afghanistan).
Load more

Recommended publications
  • Kyzylorda Oblast, Kazakhstan Challenges
    for Kyzylorda Oblast Youth Health Center Oblast Youth for Kyzylorda © Umirbai Tumenbayev, official photographer © Umirbai Tumenbayev, The Kyzylorda Oblast Medical Center, Kyzylorda Oblast, Kazakhstan Kyzylorda City General overview Kyzylorda Oblast (region) is situated along the summer, precipitation generally evaporates, and Syrdariya River in the south-western part of the it is only in winter that the soil receives moisture. Republic of Kazakhstan in central Eurasia. The There are many days with strong wind, and dust region covers an area of 226 000 km2 with a storms can occur in summer. The remaining part distance of 1000 km between its northernmost of the shrinking Aral Sea – the Small Aral Sea – is and southernmost borders (1). Comprising seven located in the southern part of the region. The districts and the capital city – also called Kyzylorda Aral Sea has been described as “one of the worst – the region is more than 190 years old, one of environmental disasters of the world”(2). The the oldest in the country. It borders on Aktobe salinity of the remaining water exceeds 100 g/l. Oblast in the north-west, Karaganda Oblast in In 2008, a project to construct a seawall made the north, South Kazakhstani Oblast in the south- it possible to increase the water level slowly in east, and the Republic of Uzbekistan in the south. the northern part of the Aral. Currently, the level It has a wide range of mineral resources, the of salinity is decreasing, which has resulted in most important being hydrocarbons, non-ferrous the appearance of some species of fish.
    [Show full text]
  • The Silk Roads: an ICOMOS Thematic Study
    The Silk Roads: an ICOMOS Thematic Study by Tim Williams on behalf of ICOMOS 2014 The Silk Roads An ICOMOS Thematic Study by Tim Williams on behalf of ICOMOS 2014 International Council of Monuments and Sites 11 rue du Séminaire de Conflans 94220 Charenton-le-Pont FRANCE ISBN 978-2-918086-12-3 © ICOMOS All rights reserved Contents STATES PARTIES COVERED BY THIS STUDY ......................................................................... X ACKNOWLEDGEMENTS ..................................................................................................... XI 1 CONTEXT FOR THIS THEMATIC STUDY ........................................................................ 1 1.1 The purpose of the study ......................................................................................................... 1 1.2 Background to this study ......................................................................................................... 2 1.2.1 Global Strategy ................................................................................................................................ 2 1.2.2 Cultural routes ................................................................................................................................. 2 1.2.3 Serial transnational World Heritage nominations of the Silk Roads .................................................. 3 1.2.4 Ittingen expert meeting 2010 ........................................................................................................... 3 2 THE SILK ROADS: BACKGROUND, DEFINITIONS
    [Show full text]
  • Selected Works of Chokan Valikhanov Selected Works of Chokan Valikhanov
    SELECTED WORKS OF CHOKAN VALIKHANOV CHOKAN OF WORKS SELECTED SELECTED WORKS OF CHOKAN VALIKHANOV Pioneering Ethnographer and Historian of the Great Steppe When Chokan Valikhanov died of tuberculosis in 1865, aged only 29, the Russian academician Nikolai Veselovsky described his short life as ‘a meteor flashing across the field of oriental studies’. Set against his remarkable output of official reports, articles and research into the history, culture and ethnology of Central Asia, and more important, his Kazakh people, it remains an entirely appropriate accolade. Born in 1835 into a wealthy and powerful Kazakh clan, he was one of the first ‘people of the steppe’ to receive a Russian education and military training. Soon after graduating from Siberian Cadet Corps at Omsk, he was taking part in reconnaissance missions deep into regions of Central Asia that had seldom been visited by outsiders. His famous mission to Kashgar in Chinese Turkestan, which began in June 1858 and lasted for more than a year, saw him in disguise as a Tashkent mer- chant, risking his life to gather vital information not just on current events, but also on the ethnic make-up, geography, flora and fauna of this unknown region. Journeys to Kuldzha, to Issyk-Kol and to other remote and unmapped places quickly established his reputation, even though he al- ways remained inorodets – an outsider to the Russian establishment. Nonetheless, he was elected to membership of the Imperial Russian Geographical Society and spent time in St Petersburg, where he was given a private audience by the Tsar. Wherever he went he made his mark, striking up strong and lasting friendships with the likes of the great Russian explorer and geographer Pyotr Petrovich Semyonov-Tian-Shansky and the writer Fyodor Dostoyevsky.
    [Show full text]
  • Shipbuilding in the Aral Sea and the Amu Darya River
    International Journal of Recent Technology and Engineering (IJRTE) ISSN: 2277-3878, Volume-8 Issue-4, November 2019 Shipbuilding in the Aral Sea and the Amu Darya River Fazliddin Jumaniyozov Abstract— This article is focused on the history of the the collection also contains information on the first steps of emergence and development of shipbuilding in the Khorezm oasis shipbuilding in the Aral and The Amudarya. The researcher in the 19th and 20th centuries. The history of Butakov's study of from Bukhara Z.O. Koryagdiev tried to cover the problem in the Aral Sea and the discovery of sea routes in Amu Darya river some way. For example, you can read some details about the has a two-hundred-year period. During this time, the navy and the seafaring reached a high level and almost ended. During this Alibobo Port in Gurlen. The port is said to be located in a period, the major part of cargo transported to the Khorezm oasis very picturesque place - opposite Badaytokay, the ships of by ships was a huge flotilla in this area. The deterioration of the Guzmān are constantly flowing to cross the river, and during ecological situation, the extreme degradation of the river and the the holidays, thousands gather. The Alibobo area, which is complication of ships, the efficiency of rail, automobile, airfreight located on a river, even in the hardest part of the river, is safe. and passenger transport - all led to the limitation of ships' “At the bridge on the road to Alibobo, there was a special movement on the rivers of Central Asia.
    [Show full text]
  • Land Und Leute 22
    Vorwort 11 Herausragende Sehenswürdigkeiten 12 Das Wichtigste in Kurze 14 Entfernungstabelle 20 Zeichenlegende 20 LAND UND LEUTE 22 Tadschikistan im Überblick 24 Landschaft und Natur 25 Gewässer und Gletscher 27 Klima und Reisezeit 28 Flora 29 Fauna 32 Umweltprobleme 37 Geschichte 42 Die Anfänge 42 Vom griechisch-baktrischen Reich bis zur Kushan-Dynastie 47 Eroberung durch die Araber und das Somonidenreich 49 Türken, Mongolen und das Emirat von Buchara 49 Russischer Einfluss und >Great Game< 50 Sowjetische Zeit 50 Unabhängigkeit und Burgerkrieg 52 Endlich Frieden 53 Tadschikistan im 21. Jahrhundert 57 Regierung 57 Wirtschaftslage 58 Kritik und Opposition 58 Tourismus 60 Politisches System in Theorie und Praxis 61 Administrative Gliederung 63 Wirtschaft 65 Bevölkerung und Kultur 69 Religionen und Minderheiten 71 Städtebau und Architektur 74 Volkskunst 77 Sprache 79 Literatur 80 Musik 85 Brauche 89 http://d-nb.info/1071383132 Feste 91 Heilige Statten 94 Die tadschikische Küche 95 ZENTRALTADSCHIKISTAN 102 Duschanbe 104 Geschichte 104 Spaziergang am Rudaki-Prospekt 110 Markt und Mahalla 114 Parks am Varzob-Fluss 115 Museen 119 Denkmaler 122 Duschanbe live 128 Duschanbe-Informationen 131 Die Umgebung von Duschanbe 145 Festung Hisor 145 Varzob-Schlucht 148 Romit-Tal 152 Tal des Karatog 153 Wasserkraftwerk Norak 154 Das Rasht-Tal 156 Ob-i Garm 158 Gharm 159 Jirgatol 159 Reiseveranstalter in Zentral­ tadschikistan 161 DER PAMIR 162 Das Dach der Welt 164 Ein geografisches Kurzportrait 167 Die Bewohner des Pamirs 170 Sprache und Religion 186 Reisen
    [Show full text]
  • The Aral Sea
    The Aral Sea edited by David L. Alles Western Washington University e-mail: [email protected] Last Updated 2011-11-4 Note: In PDF format most of the images in this web paper can be enlarged for greater detail. 1 Introduction The Aral Sea was once the world's fourth largest lake, slightly bigger than Lake Huron, and one of the world's most fertile regions. Today it is little more than a string of lakes scattered across central Asia east of the Caspian Sea. The sea disappeared for several reasons. One is that the Aral Sea is surrounded by the Central Asian deserts, whose heat evaporates 60 square kilometers (23 sq. miles) of water from its surface every year. Second is four decades of agricultural development and mismanagement along the Syr Darya and Amu Darya rivers that have drastically reduced the amount of fresh water flowing into the sea. The two rivers were diverted starting in the 1960s in a Soviet scheme to grow cotton in the desert. Cotton still provides a major portion of foreign currency for many of the countries along the Syr Darya and Amu Darya rivers. By 2003, the Aral Sea had lost approximately 75% of its area and 90% of its pre- 1960 volume. Between 1960 and January 2005, the level of the northern Aral Sea fell by 13 meters (~ 43 ft) and the larger southern portion of the sea by 23 meters (75.5 ft) which means that water can now only flow from the north basin to the south (Roll, et al., 2006).
    [Show full text]
  • Oberhänsli, H., Boroffka, N., Sorrel, P., Krivonogov, S. (2007)
    Originally published as: Oberhänsli, H., Boroffka, N., Sorrel, P., Krivonogov, S. (2007): Climate variability during the past 2,000 years and past economic and irrigation activities in the Aral Sea basin. - Irrigation and Drainage Systems, 21, 3-4, 167-183 DOI: 10.1007/s10795-007-9031-5. Irrigation and Drainage Systems, 21, 3-4, 167-183, 10.1007/s10795-007-9031-5 1 Climate variability during the past 2000 years and past economic and irrigation 2 activities in the Aral Sea basin 3 4 Hedi Oberhänsli1, Nikolaus Boroffka2, Philippe Sorrel3, Sergey Krivonogov,4 5 6 1) GeoForschungsZentrum, Telegraphenberg, D-14473 Potsdam, Germany. 7 2) Deutsches Archäologisches Institut, Im Dol 2-6, D-14195 Berlin, Germany. 8 3) Laboratoire "Morphodynamique Continentale et Côtière" (UMR 6143 CNRS), 9 Université de Caen Basse-Normandie, 24 rue des Tilleuls, F-14000 CAEN, France. 10 4) United Institute of Geoloy, Geophysics and Mineralogy of the Russian Academy of 11 Sciences, Siberian Division, Novosibirsk regional Center of Geoinformational 12 Technologies, Academic Koptyug prospekt 3, 630090 Novosibirsk, Russia. 13 14 Abstract 15 The lake level history, here based on the relative abundance of Ca (gypsum), is used for 16 tracing past hydrological conditions in Central Asia. Lake level was close to a minimum 17 before approximately AD 300, at about AD 600, AD 1220 and AD 1400. Since 1960 the 18 lake level is lowering again. Lake water level was lowest during the 14th or early 15th 19 centuries as indicated by a coeval settlement, which today is still under water near the 20 well-dated mausoleum of Kerderi.
    [Show full text]
  • Federal Research Division Country Profile: Tajikistan, January 2007
    Library of Congress – Federal Research Division Country Profile: Tajikistan, January 2007 COUNTRY PROFILE: TAJIKISTAN January 2007 COUNTRY Formal Name: Republic of Tajikistan (Jumhurii Tojikiston). Short Form: Tajikistan. Term for Citizen(s): Tajikistani(s). Capital: Dushanbe. Other Major Cities: Istravshan, Khujand, Kulob, and Qurghonteppa. Independence: The official date of independence is September 9, 1991, the date on which Tajikistan withdrew from the Soviet Union. Public Holidays: New Year’s Day (January 1), International Women’s Day (March 8), Navruz (Persian New Year, March 20, 21, or 22), International Labor Day (May 1), Victory Day (May 9), Independence Day (September 9), Constitution Day (November 6), and National Reconciliation Day (November 9). Flag: The flag features three horizontal stripes: a wide middle white stripe with narrower red (top) and green stripes. Centered in the white stripe is a golden crown topped by seven gold, five-pointed stars. The red is taken from the flag of the Soviet Union; the green represents agriculture and the white, cotton. The crown and stars represent the Click to Enlarge Image country’s sovereignty and the friendship of nationalities. HISTORICAL BACKGROUND Early History: Iranian peoples such as the Soghdians and the Bactrians are the ethnic forbears of the modern Tajiks. They have inhabited parts of Central Asia for at least 2,500 years, assimilating with Turkic and Mongol groups. Between the sixth and fourth centuries B.C., present-day Tajikistan was part of the Persian Achaemenian Empire, which was conquered by Alexander the Great in the fourth century B.C. After that conquest, Tajikistan was part of the Greco-Bactrian Kingdom, a successor state to Alexander’s empire.
    [Show full text]
  • Download File
    For non-commercial distribution only All photos used in this compendium were provided by the Knowledge Management Initiative (KMI) participants. The compendium is available in English and Russian. The electronic version of the compendium can be found at: www.preventionweb.net Hard copies are available at: UNISDR CA, 37/1 Bokhtar str, 6th floor, 734000, Dushanbe, Tajikistan. UNICEF RO CEE/CIS, Avenue de la Paix 5, 1202 Genève, Switzerland. Any comments and suggestions regarding the Compendium can be addressed to: Mr. Parviz Mahmudov, Education coordinator, UNISDR CA [email protected] Mr. Asim Rehman, Regional Emergency Preparedness and DRR Specialist, UNICEF CEE/CIS [email protected] Design: Zafar Mahmoudov, Advocacy and Communications Consultant, UNISDR CA Editor: Stephen Boyle The views expressed in this Compendium are those of the respective authors and do not necessarily reflect the position of ECHO, UNISDR and UNICEF. Acknowledgements The Compendium of Good Practices and Tools on Disaster Risk Reduction in Education in Central Asia has been developed as a result of the Knowledge Management Initiative, implemented by the United Nations International Strategy for Disaster Reduction in Central Asia (UNISDR) and the United Nations Children’s Fund (UNICEF) within the framework of the Disaster Preparedness Programme of the European Commission’s Humanitarian Aid Department (DIPECHO) and financed by ECHO. UNISDR and UNICEF express their gratitude to all participants who submitted examples of their experiences on disaster risk reduction in education: Mr. Timur Idrisov, NGO “Little Earth”, Tajikistan; Ms. Lyudmila Bakhareva, NGO “Man and elements”, Kazakhstan; Mr. Alexandr Kravchuk, UNDP Kazakhstan, Kazakhstan; Mr. Khusan Tursunov, NGO “HAYOT”, Uzbekistan; Ms.
    [Show full text]
  • The Republic of Tajikistan Ministry of Energy and Industry
    The Republic of Tajikistan Ministry of Energy and Industry DATA COLLECTION SURVEY ON THE INSTALLMENT OF SMALL HYDROPOWER STATIONS FOR THE COMMUNITIES OF KHATLON OBLAST IN THE REPUBLIC OF TAJIKISTAN FINAL REPORT September 2012 Japan International Cooperation Agency NEWJEC Inc. E C C CR (1) 12-005 Final Report Contents, List of Figures, Abbreviations Data Collection Survey on the Installment of Small Hydropower Stations for the Communities of Khatlon Oblast in the Republic of Tajikistan FINAL REPORT Table of Contents Summary Chapter 1 Preface 1.1 Objectives and Scope of the Study .................................................................................. 1 - 1 1.2 Arrangement of Small Hydropower Potential Sites ......................................................... 1 - 2 1.3 Flowchart of the Study Implementation ........................................................................... 1 - 7 Chapter 2 Overview of Energy Situation in Tajikistan 2.1 Economic Activities and Electricity ................................................................................ 2 - 1 2.1.1 Social and Economic situation in Tajikistan ....................................................... 2 - 1 2.1.2 Energy and Electricity ......................................................................................... 2 - 2 2.1.3 Current Situation and Planning for Power Development .................................... 2 - 9 2.2 Natural Condition ............................................................................................................
    [Show full text]
  • Diversity and Ecology of Periphytonic Algae in the Arys River Basin, Kazakhstan
    Journal of Ecology & Natural Resources ISSN: 2578-4994 Diversity and Ecology of Periphytonic Algae in the Arys River Basin, Kazakhstan 1 2 Barinova SS *, Krupa EG Research Article 1Institute of Evolution, University of Haifa, Israel Volume 1 Issue 1 2 Republican State Enterprise on the Right of Economic Use "Institute of Zoology", Received Date: June 27, 2017 Ministry of Education and Science, Science Committee, Republic of Kazakhstan Published Date: July 15, 2017 DOI: 10.23880/jenr-16000106 *Corresponding author: Barinova SS, Institute of Evolution, University of Haifa, Mount Carmel, 199 Abba Khoushi Ave., Haifa 3498838, Israel, E-mail: [email protected] Abstract No one information about algal community diversity from the Arys River basin was before this study. The first data about algal and cyanobacteria species diversity was represented for the Arys River basin and compared it to freshwater algae patterns of the related mountain regions. Altogether 82 species were found in 28 samples of phytoperiphyton on 13 sampling stations of the Arys River and its tributaries. Diatoms prevail in studied algal flora. Bioindication characterize the Arys River waters as temperate, moderately oxygenated, fresh, neutral water affected by a low to moderate level of organic pollution, Class II-III of water quality. The pattern of algae and cyanobacteria diversity distribution depends on altitude and local climatic and environmental conditions. Bacillariophyta species was richest in high mountain habitats, green algae, cyanobacteria and charophytes avoid high mountain habitats and have negative correlation with altitude. These results can be used as indicator of environmental changes in the mountainous areas. Three floristic groups were recognized in the studied river communities corresponding to the upper, middle and lower parts of the watershed.
    [Show full text]
  • Sharing of Experiences on Water Governance in the Context of Disaster Risk Reduction in the Chu-Talas Basin
    SESSION 3 EEF.DEL/24/15 12 May 2015 Second Preparatory Meeting of the 23rd OSCE Economic and Environmental Forum ENGLISH only SHARING OF EXPERIENCES ON WATER GOVERNANCE IN THE CONTEXT OF DISASTER RISK REDUCTION IN THE CHU-TALAS BASIN Commission of the Republic of Kazakhstan and the Kyrgyz Republic on the Use of Water Management Facilities of Intergovernmental Status on the Rivers Chu and Talas GENERAL INFORMATION ON THE CHU AND TALAS Chu basin Talas basin ´ The catchment area - ´ The catchment area - 38 400 km2 (Large Arna) 52 700 km2 ´ The length of the river - ´ The length of the river - 661 1186 km km ´ Power supply - snow-glacier ´ Power supply - snow-glacier ´ Water resources - 6.64 km3 ´ Water resources – 1.74 km3 ´ Irrigated areas - 476.0 t.ga: ´ Irrigated areas – 162.7 t.ga: Kazakhstan - 114,7- 24% Kazakhstan – 60.0 - 37% Kyrgyzstan - 361,3-76% Kyrgyzstan – 102.7-63% ´ Population - 2 095 th. ´ Population – 686.3 th. Commission of the Republic of Kazakhstan and the Kyrgyz Republic on the Use of Water Management Facilities of Intergovernmental Status on the Rivers Chu and Talas STEPS TO ENSURE STABILITY IN USE WATER RESOURCES OF CHU AND TALAS 1996 - decision-making by water management authorities in Kazakhstan and Kyrgyzstan on the joint solution of water problems, 2000, Jan. 21, Astana - the signing of the Intergovernmental “Agreement on the Use of Water Management Facilities of Intergovernmental Status on the Chu and Talas Rivers”, August 2004 - the establishment of the Commission, May 2011, Bishkek - an International Conference to commemorate a decade of a bilateral “Agreement”.
    [Show full text]