List of Rivers of Mongolia

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Draining Into
Sl. No

River Name

Yenisei River

Russian Name

Russia

Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean Arctic Ocean

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Angara River Selenge River

Chikoy River

Menza River Katantsa River

Dzhida River

Zelter River

Orkhon River

Tuul River
Russia, flowing out of Lake Baikal

Сэлэнгэ мөрөн in Sükhbaatar, flowing into Lake Baikal

Russia

Зэлтэрийн гол, Bulgan/Selenge/Russia Орхон гол, Arkhangai/Övörkhangai/Bulgan/Selenge Туул гол, Khentii/Töv/Bulgan/Selenge Тамир гол, Arkhangai Хараа гол, Töv/Selenge/Darkhan-Uul Эгийн гол, Khövsgöl/Bulgan Үүрийн гол, Khövsgöl Уйлган гол, Khövsgöl Аригийн гол, Khövsgöl Тарвагтай гол, Bulgan Хануй гол, Arkhangai/Bulgan Идэр гол, Khövsgöl Чулуут гол, Arkhangai/Khövsgöl Суман гол, Arkhangai Дэлгэрмөрөн, Khövsgöl Бэлтэсийн Гол, Khövsgöl Бүгсийн Гол, Khövsgöl

10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49
Tamir River

Kharaa River

Eg River

Üür River Uilgan River

Arigiin River Tarvagatai River

Khanui River Ider River Chuluut River

Lesser Yenisei

Kyzyl-Khem Büsein River Shishged River Sharga River

Tengis River Amur River

Shilka River

Onon River

Kherlen River

Ongi River
Russia

Кызыл-Хем Шишгэд гол, Khövsgöl Шарга гол, Khövsgöl Тэнгис гол, Khövsgöl Russia/China

Russia

Онон гол
Sea of Okhotsk (Pacific Ocean) Sea of Okhotsk (Pacific Ocean) Sea of Okhotsk (Pacific Ocean) Endorheic basins Endorheic basins
Хэрлэн гол

Hulun Lake

Ulaan Lake
Khovd River Kharkhiraa River

Sangil gol Turuun River

Nariin gol

Great Lakes Depression Great Lakes Depression Great Lakes Depression Great Lakes Depression Great Lakes Depression Great Lakes Depression Great Lakes Depression Great Lakes Depression Great Lakes Depression Great Lakes Depression Great Lakes Depression Great Lakes Depression Great Lakes Depression

Ulungur Lake
Khar-Us Lake Uvs Nuur Basin Uvs Nuur Basin Uvs Nuur Basin Uvs Nuur Basin Uvs Nuur Basin Uvs Nuur Basin Uvs Nuur Basin Uvs Nuur Basin Uvs Nuur Basin Khyargas Lake Dörgön Lake

Teeliin gol

Flowing out of Khar Lake
Chono Kharaikh gol Draining into Khar Lake

Bulgan River Ulungur River

Dörgön Lake
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Recommended publications

Journal Biology 2004 3

Mongolian Journal of Biological Sciences 2004 Vol. 2(1): 39-42 Hydrochemical Characteristics of Selenge River and its Tributaries on the Territory of Mongolia Bazarova J.G. 1, Dorzhieva S.G.1, Bazarov B.G. 1, Barkhutova D.D.2, Dagurova O.P.2, Namsaraev B.B. 2 and Zhargalova S.O.2 1Baikal Institute of Nature Management of SB RAS, Ulan-Ude, 2Institute of General and Experimental Biology of SB RAS, Ulan-Ude, E-mail: [email protected] Abstract Hydrochemical research of the Selenge and its main tributary the Orkhon river on the territory of Mongolia has been conducted. Concentrations of the main water ions were measured. Distribution of - + heavy metals was determined. Dynamics of biogenic elements (NO3 , NH4 , phosphates) and degree of phenol pollution was determined. Key words: Baikal, biogenic, heavy metals, ions, phenol, Selenge River Introduction river is polluted along its entire length. To assess the current ecological condition in the Mongolian During the last 30-40 years Lake Baikal has part of the Selenge river basin, it is necessary to been influenced by various anthropogenic factors. implement hydrobiological and hydrochemical Industrial and household waste water have changed monitoring. It requires information not only of the chemical composition of Baikal with a chemical composition, but of biogenic components deterioration in water quality in the basin territory. in the processes of accumulation and According to sustainable development policy, transformation in water, bottom sediments and river protection of Baikal region is considered
The Influence of Climatic Change and Human Activity on Erosion Processes in Sub-Arid Watersheds in Southern East Siberia

HYDROLOGICAL PROCESSES Hydrol. Process. 17, 3181–3193 (2003) Published online in Wiley InterScience (www.interscience.wiley.com). DOI: 10.1002/hyp.1382 The influence of climatic change and human activity on erosion processes in sub-arid watersheds in southern East Siberia Leonid M. Korytny,* Olga I. Bazhenova, Galina N. Martianova and Elena A. Ilyicheva Institute of Geography, Siberian Branch of the Russian Academy of Sciences, 1 Ulanbatorskaya St., Irkutsk, 664033, Russia Abstract: A LUCIFS model variant is presented that represents the influence of climate and land use change on fluvial systems. The study considers trends of climatic characteristics (air temperature, annual precipitation totals, rainfall erosion index, aridity and continentality coefficients) for the steppe and partially wooded steppe watersheds of the south of East Siberia (the Yenisey River macro-watershed). It also describes the influence of these characteristics on erosion processes, one indicator of which is the suspended sediment yield. Changes in the river network structure (the order of rivers, lengths, etc.) as a result of agricultural activity during the 20th century are investigated by means of analysis of maps of different dates for one of the watersheds, that of the Selenga River, the biggest tributary of Lake Baikal. The study reveals an increase of erosion process intensity in the first two-thirds of the century in the Selenga River watershed and a reduction of this intensity in the last third of the century, both in the Selenga River watershed and in most of the other watersheds of the study area. Copyright 2003 John Wiley & Sons, Ltd. KEY WORDS LUCIFS; Yenisey watershed; fluvial system; climate change; land use change; river network structure; erosion processes.
Key Sites for Key Sites for Conservation

Directory of Important Bird Areas in Mongolia: KEY SITES FOR CONSERVATION A project of In collaboration with With the support of Printing sponsored by Field surveys supported by Directory of Important Bird Areas in Mongolia: KEY SITES FOR CONSERVATION Editors: Batbayar Nyambayar and Natsagdorj Tseveenmyadag Major contributors: Ayurzana Bold Schagdarsuren Boldbaatar Axel Bräunlich Simba Chan Richard F. A. Grimmett and Andrew W. Tordoff This document is an output of the World Bank study Strengthening the Safeguard of Important Areas of Natural Habitat in North-East Asia,ﬁ nanced by consultant trust funds from the government of Japan Ulaanbaatar, January 2009 An output of: The World Bank study Strengthening the Safeguard of Important Areas of Natural Habitat in North-East Asia,ﬁ nanced by consultant trust funds from the government of Japan Implemented by: BirdLife International, the Wildlife Science and Conservation Center and the Institute of Biology of the Mongolian Academy of Sciences In collaboration with: Ministry of Nature, Environment and Tourism Supporting organisations: WWF Mongolia, WCS Mongolia Program and the National University of Mongolia Editors: Batbayar Nyambayar and Natsagdorj Tseveenmyadag Major contributors: Ayurzana Bold, Schagdarsuren Boldbaatar, Axel Bräunlich, Simba Chan, Richard F. A. Grimmett and Andrew W. Tordoff Maps: Dolgorjav Sanjmyatav, WWF Mongolia Cover illustrations: White-naped Crane Grus vipio, Dalmatian Pelican Pelecanus crispus, Whooper Swans Cygnus cygnus and hunters with Golden Eagles Aquila chrysaetos (Batbayar Nyambayar); Siberian Cranes Grus leucogeranus (Natsagdorj Tseveenmyadag); Saker Falcons Falco cherrug and Yellow-headed Wagtail Motacilla citreola (Gabor Papp). ISBN: 978-99929-0-752-5 Copyright: © BirdLife International 2009. All rights reserved. The use and reproduction of any part of this publication is welcomed for non-commercial purposes only, provided that the source is acknowledged Suggested citation: Nyambayar, B.
INFLUENCE of SOIL-ECOLOGICAL CONDITIONS on VEGETATION ZONATION in a WESTERN MONGOLIAN LAKE SHORE- SEMI-DESERT ECOTONE with 6 Figures, 4 Tables and 4 Photos

72 Erdkunde Band 61/2007 INFLUENCE OF SOIL-ECOLOGICAL CONDITIONS ON VEGETATION ZONATION IN A WESTERN MONGOLIAN LAKE SHORE- SEMI-DESERT ECOTONE With 6 figures, 4 tables and 4 photos ANDREA STRAUSS and UDO SCHICKHOFF Keywords: Vegetation geography, soil geography, environmental change, Central Asia, semidesert environments Keywords: Vegetationsgeographie, Bodengeographie, Umweltforschung, Zentralasien, aride Räume Zusammenfassung: Der Einfluss bodenökologischer Bedingungen auf die Vegetationszonierung in einem Seeufer-Halb- wüsten-Ökoton der westlichen Mongolei Das Becken der Großen Seen in der Westmongolei ist geprägt von ausgedehnten Wüsten-, Halbwüsten- und Steppen- arealen sowie von Seen und umgebenden einzigartigen Feuchtgebieten. Diese Feuchtgebiete sind bedeutende Elemente der Landschaftsökosysteme semi-arider und arider Räume. Andererseits ist die Kenntnis selbst grundlegender Ökosystemkompo- nenten wie Vegetation und Böden noch sehr lückenhaft. Das Ziel der vorliegenden landschaftsökologischen Studie entlang eines Seeufer-Halbwüsten-Ökotons war es, das klein- räumige Muster von Standortfaktoren entlang eines ausgeprägten Umweltgradienten sowie den Einfluss dieses Musters auf die Vegetationszonierung zu analysieren. Um die Veränderungen in dem Übergangsbereich zwischen aquatischen und terres- trischen Lebensräumen adäquat zu erfassen, wurden die Daten mit einem Transekt-Ansatz aufgenommen. Pflanzengesell- schaften wurden nach der Braun-Blanquet-Methode klassifiziert. Die Vegetations- und Bodendaten wurden einer Detrended Correspondence
New Documents on Mongolia and the Cold War

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Tuul River Mongolia

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Trans-Baykal (Rusya) Bölgesi'nin Coğrafyasi

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Impacts of Late Quaternary Environmental Change on the Long-Tailed Ground Squirrel (Urocitellus Undulatus) in Mongolia

ZOOLOGICAL RESEARCH Impacts of late Quaternary environmental change on the long-tailed ground squirrel (Urocitellus undulatus) in Mongolia Bryan S. McLean1,*, Batsaikhan Nyamsuren2, Andrey Tchabovsky3, Joseph A. Cook4 1 University of Florida, Florida Museum of Natural History, Gainesville, FL 32611, USA 2 Department of Biology, School of Arts and Sciences, National University of Mongolia, Ulaan Baatar 11000, Mongolia 3 Laboratory of Population Ecology, A.N. Severtsov Institute of Ecology and Evolution, Moscow 119071, Russia 4 University of New Mexico, Department of Biology and Museum of Southwestern Biology, Albuquerque, NM 87131, USA ABSTRACT of range shifts into these lowland areas in response to Pleistocene glaciation and environmental change, Impacts of Quaternary environmental changes on followed by upslope movements and mitochondrial mammal faunas of central Asia remain poorly lineage sorting with Holocene aridification. Our study understood due to a lack of comprehensive illuminates possible historical mechanisms responsible phylogeographic sampling for most species. To for U. undulatus genetic structure and contributes to help address this knowledge gap, we conducted a framework for ongoing exploration of mammalian the most extensive molecular analysis to date of response to past and present climate change in central the long-tailed ground squirrel (Urocitellus undulatus Asia. Pallas 1778) in Mongolia, a country that comprises Keywords: Central Asia; Gobi Desert; Great Lakes the southern core of this species’ range. Drawing on Depression; Mongolia; Phylogeography material from recent collaborative ﬁeld expeditions, we genotyped 128 individuals at two mitochondrial INTRODUCTION genes (cytochrome b and cytochrome oxidase I; Urocitellus undulatus Pallas 1778 is a charismatic, 1 797 bp total). Phylogenetic inference supports the medium-bodied ground-dwelling sciurid distributed across existence of two deeply divergent infraspecific lineages central Asia, including portions of Siberia, Mongolia, (corresponding to subspecies U.
Colonization of Northern Eurasia by Modern Humans: Radiocarbon Chronology and Environment

Journal of Archaeological Science (2002) 29, 593–606 doi:10.1006/jasc.2001.0753, available online at http://www.idealibrary.com on Colonization of Northern Eurasia by Modern Humans: Radiocarbon Chronology and Environment P. M. Dolukhanov* Department of Archaeology, University of Newcastle upon Tyne, NE1 7RU, U.K. A. M. Shukurov School of Mathematics and Statistics, University of Newcastle upon Tyne, NE1 7RU, U.K. P. E. Tarasov Department of Geography, Moscow State University, Vorobyevy Gory, Moscow 119899, Russia G. I. Zaitseva Radiocarbon Laboratory, Institute for History of Material Culture, Russian Academy of Sciences, St Petersburg, Dvortsovaya nab. 18, 191186 Russia (Received 30 January 2001, revised manuscript accepted 25 July 2001) The distribution of frequencies of radiocarbon-dated Palaeolithic sites in northern Eurasia shows three peaks of 40–30, 24–18 and 17–1 ka . We argue that these peaks reﬂect the waves in the colonization of that area by Anatomically Modern Humans stemming from Central and Eastern Europe and caused by environmental stress. 2002 Elsevier Science Ltd. All rights reserved. Keywords: NORTHERN EURASIA, ANATOMICALLY MODERN HUMANS, RADIOCARBON, UPPER PALAEOLITHIC, LAST ICE AGE, PALAEOCLIMATE. Introduction glacial’’), and OIS 3 consisting of the Late Glacial Maximum (LGM) and the Late Glacial Recession. he present article is aimed at the discussion of the initial dispersal of anatomically modern T humans (AMH) in northern Eurasia, as Data and Methods inferred mainly from radiocarbon chronology and Radiocarbon age palaeoenvironmental evidence. In this respect this article may be viewed as a direct development of the The main resource of the present study consists of the previous publication, focused on East European Plain database of radiocarbon measurements of Siberia’s (Dolukhanov, Shukurov & Sokoloﬀ, 2001).
438962 1 En Bookbackmatter 213..218

Index A Average temperature, 4, 53, 55, 57, 87, 111, 162, 185 Accumulation, 12, 26, 27, 33, 44, 66, 109, 113, 140, 141, Average wind speed, 64 144–146, 152, 155, 162 Achit lake, 37, 116, 165, 208 Active layer, 122, 124–126, 130 B Active layer thickness, 124–126 Baatarkhaihan, 35 Adaatsag, 46 Baga Bogd, 3, 38, 43, 188 Agricultural land, 136, 195–199 Baga Buural, 47 Airag lake, 91, 208 Baga Gazriin Chuluu, 46, 47 Air temperature variation, 111 Baga Khavtag, 45 Aj Bogd, 35, 190 Baga Khentii, 39, 80, 110 Alag khairhan, 35 Baga Uul, 47 Alasha Gobi, 163, 165 Baishin Tsav, 46 Algae, 161, 166 Baitag Bogd, 45 Alluvial fans and sediments, 45, 46 Baruun Khuurai depression, 28, 158, 181 Alluvial-proluvial plains, 27, 29 Baruun Saikhan, 33, 43 Alluvial soils, 145, 157 Baruunturuun, 68, 136 Alpine belts, 66, 171, 185 Bayan, 3, 7, 34–36, 40, 69, 79, 88, 89, 91, 106, 109, 113 Alpine-type high mountains, 32 Bayanbor, 43 Alpine type relief, 44 Bayan Bumbun Ranges, 35 Altai region, 5, 28, 35, 42, 65, 144 Bayankhairhan, 39 Altai-Sayan ecoregion, 210 Bayantsagaan, 42, 43, 47, 49 Altai Tavan Bogd, 24, 35 Bayan-Ulgii, 7, 69, 113 Altankhukhii, 35 Biological diversity, 182 Altan Ulgii, 39 Birds, 161, 162, 169–175, 207, 208 Altitudinal belts, 6, 163, 177, 182–185, 187, 190, 192 Bogd, 3, 11, 34, 36, 38, 40, 42, 49, 101–103, 106, 181, Angarkhai, 38 188, 204, 208 Animal, 4, 6, 7, 11, 12, 16, 33, 72, 145, 169, 171, 172, Bogd Ulaan, 49 197, 205 Boreal, 6, 163, 164, 187, 210 Annual precipitation, 53, 60, 61, 71, 86, 92, 121, 186, Bor Khairhan, 39 188, 189, 192 Borzon
Part I Master Plan

PART I MASTER PLAN CHAPTER 1 INTRODUCTION I MASTER PLAN PART I MASTER PLAN CHAPTER 1 INTRODUCTION 1.1 Background of the Study In Mongolia some 50% of the total population of about 2.4 million are nomadic families. For the nomadic families Sum centers are key places for supplying their vital goods, and also for receiving public services such as administration, medical care, education, etc. As of November 1997, the electric power at 117 out of 314 Sum centers in total in Mongolia is being supplied from the national power transmission network. At the remaining 197 Sum centers, the electric power is supplied by the diesel engine generators by Sum center independently. Most of these diesels generating facilities were manufactured during the former Soviet Union era and installed long ago from 1963 to 1990. During the Social Republic era of the country, Mongolia depended on the Soviet Union for the supply of spare parts necessary for maintenance of the generating equipment and technical guidance. Due to the corruption of the Soviet Union's economy in 1991 and associated transition to a market economy, the following four factors caused troubles to the operation and maintenance of the Sum's generating facilities, i.e. (1) the lack of business operating senses, (2) the interruption of spare parts supply, (3) the lack of technical capability and (4) shortage of management budget. The operation of much equipment has been obliged to be kept stopped after failure, as operators cannot repair them. The affected generation quantity, and aggravated the conditions of daily lives of people in Sum center and caused serious effects to the socio-economic activities of the Sum centers.
Subject of the Russian Federation)

How to use the Atlas The Atlas has two map sections The Main Section shows the location of Russia’s intact forest landscapes. The Thematic Section shows their tree species composition in two different ways. The legend is placed at the beginning of each set of maps. If you are looking for an area near a town or village Go to the Index on page 153 and find the alphabetical list of settlements by English name. The Cyrillic name is also given along with the map page number and coordinates (latitude and longitude) where it can be found. Capitals of regions and districts (raiony) are listed along with many other settlements, but only in the vicinity of intact forest landscapes. The reader should not expect to see a city like Moscow listed. Villages that are insufficiently known or very small are not listed and appear on the map only as nameless dots. If you are looking for an administrative region Go to the Index on page 185 and find the list of administrative regions. The numbers refer to the map on the inside back cover. Having found the region on this map, the reader will know which index map to use to search further. If you are looking for the big picture Go to the overview map on page 35. This map shows all of Russia’s Intact Forest Landscapes, along with the borders and Roman numerals of the five index maps. If you are looking for a certain part of Russia Find the appropriate index map. These show the borders of the detailed maps for different parts of the country.