UNDERSTANDING MIGRATION and REMITTANCES to IMPROVE FOREST MANAGEMENT PROJECTS and POLICIES Synthesis Report: Tajikistan
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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 -
The Impacts of Increasing Drought on Forest Dynamics, Structure, and Biodiversity in the United States
Global Change Biology (2016) 22, 2329–2352, doi: 10.1111/gcb.13160 SPECIAL FEATURE The impacts of increasing drought on forest dynamics, structure, and biodiversity in the United States JAMES S. CLARK1 , LOUIS IVERSON2 , CHRISTOPHER W. WOODALL3 ,CRAIGD.ALLEN4 , DAVID M. BELL5 , DON C. BRAGG6 , ANTHONY W. D’AMATO7 ,FRANKW.DAVIS8 , MICHELLE H. HERSH9 , INES IBANEZ10, STEPHEN T. JACKSON11, STEPHEN MATTHEWS12, NEIL PEDERSON13, MATTHEW PETERS14,MARKW.SCHWARTZ15, KRISTEN M. WARING16 andNIKLAUS E. ZIMMERMANN17 1Nicholas School of the Environment, Duke University, Durham, NC 27708, USA, 2Forest Service, Northern Research Station 359 Main Road, Delaware, OH 43015, USA, 3Forest Service 1992 Folwell Avenue,Saint Paul, MN 55108, USA, 4U.S. Geological Survey, Fort Collins Science Center Jemez Mountains Field Station, Los Alamos, NM 87544, USA, 5Forest Service, Pacific Northwest Research Station, Corvallis, OR 97331, USA, 6Forest Service, Southern Research Station, Monticello, AR 71656, USA, 7Rubenstein School of Environment and Natural Resources, University of Vermont, 04E Aiken Center, 81 Carrigan Dr., Burlington, VT 05405, USA, 8Bren School of Environmental Science and Management, University of California, Santa Barbara, CA 93106, USA, 9Department of Biology, Sarah Lawrence College, New York, NY 10708, USA, 10School of Natural Resources and Environment, University of Michigan, 2546 Dana Building, Ann Arbor, MI 48109, USA, 11U.S. Geological Survey, Southwest Climate Science Center and Department of Geosciences, University of Arizona, 1064 E. Lowell -
Predicting Future Mangrove Forest Migration in the Everglades Under Rising Sea Level
Predicting Future Mangrove Forest Migration in the Everglades Under Rising Sea Level Mangroves in the Everglades punctuate the vulnerability of mangrove ha) on an annual basis for the entire simu- forests to rising sea level and other climate lated landscape. Each land unit is defined Mangroves are highly productive changes. Global climate change has been by habitat type (forest, marsh, aquatic), ecosystems that provide valued habitat for projected to increase seawater tempera- land elevation, water level, and salinity fish and shorebirds. Mangrove forests are tures and accelerate the rise in sea level conditions. SELVA also calculates prob- universally composed of relatively few which may further compound ecosystem ability functions of disturbance for each tree species and a single overstory strata. stress in mangrove-dominated systems. forest unit relative to potential sea-level Three species of true mangroves are com- These forests are subject to coastal and rise, lightning, and hurricane strikes. In- mon to intertidal zones of the Caribbean inland processes of hydrology largely tertidal forest units are then simulated with and Gulf of Mexico Coast, namely, black controlled by regional climate, disturbance the MANGRO model based on unique sets mangrove (Avicennia germinans), white regimes, and human decisions about water of environmental factors and forest history. mangrove (Laguncularia racemosa), and management. MANGRO is a spatially explicit red mangrove (Rhizophora mangle). Man- Mangroves are halophytes, mean- stand simulation model constructed for grove forests occupy intertidal settings of ing they can tolerate the added stress of mangrove forests of the Neotropics (fig. the coastal margin of the Everglades along waterlogging and salinity conditions that 2). -
Miocene Exhumation of the Pamir Revealed by Detrital Geothermochronology of Tajik Rivers C
TECTONICS, VOL. 31, TC2014, doi:10.1029/2011TC003040, 2012 Miocene exhumation of the Pamir revealed by detrital geothermochronology of Tajik rivers C. E. Lukens,1 B. Carrapa,1,2 B. S. Singer,3 and G. Gehrels2 Received 4 October 2011; revised 6 February 2012; accepted 26 February 2012; published 18 April 2012. [1] The Pamir mountains are the western continuation of the Tibetan-Himalayan system, the largest and highest orogenic system on Earth. Detrital geothermochronology applied to modern river sands from the western Pamir of Tajikistan records the history of sediment source crystallization, cooling, and exhumation. This provides important information on the timing of tectonic processes, relief formation, and erosion during orogenesis. U-Pb geochronology of detrital zircons and 40Ar/39Ar thermochronology of white micas from five rivers draining distinct tectonic terranes in the western Pamir document Paleozoic through Cenozoic crystallization ages and a Miocene (13–21 Ma) cooling signal. Detrital zircon U-Pb ages show Proterozoic through Cenozoic ages and affinity with Asian rocks in Tibet. The detrital 40Ar/39Ar data set documents deep and regional exhumation of the Pamir mountains >30 Myr after Indo-Asia collision, which is best explained with widespread erosion of metamorphic domes. This exhumation signal coincides with deposition of over 6 km of conglomerates in the adjacent foreland, documenting high subsidence, sedimentation, and regional exhumation in the region. Our data are consistent with a high relief landscape and orogen-wide exhumation at 13–21 Ma and correlate with the timing of exhumation of the Pamir gneiss domes. This exhumation is younger in the Pamir than that observed in neighboring Tibet and is consistent with higher magnitude Cenozoic deformation and shortening in this part of the orogenic system. -
Vulnerability Assessment Bartang
Ecosystem-based Adaptation in Central Asia Vulnerability of High Mountain Ecosystems to Climate Change in Tajikistan’s Bartang Valley – Ecological, Social and Economic Aspects – with references to the project region in Kyrgyzstan Greifswald, December 2015 Ecosystem-based Adaptation in Central Asia Ecosystem-based Adaptation in Central Asia Vulnerability of High Mountain Ecosystems to Climate Change in Tajikistan’s Bartang Valley – Ecological, Social and Economic Aspects – with references to the project region in Kyrgyzstan Jonathan Etzold with contributions of Qumriya Vafodorova (Camp Tabiat) and Dr. Anne Zemmrich Michael Succow Foundation for the Protection of Nature Ellernholzstraße 1/3, 17487 Greifswald, Germany Tel.: +49 (0)3834 - 83542-18 Fax: +49 (0)3834 - 83542-22 E-mail: [email protected] www.succow-stiftung.de Cover picture: Darjomj village in Tajikistan © Jonathan Etzold Michael Succow Foundation for the Protection of Nature Content 1. Glossary and abbreviations of terms and transcription used in the text ............................................... 6 1.1 Glossary & abbreviations ........................................................................................................................... 6 1.2 Transcription................................................................................................................................................ 6 2. Introduction and scope of the report ......................................................................................................... -
An Indicator of Tree Migration in Forests of the Eastern United States
Forest Ecology and Management 257 (2009) 1434–1444 Contents lists available at ScienceDirect Forest Ecology and Management journal homepage: www.elsevier.com/locate/foreco An indicator of tree migration in forests of the eastern United States C.W. Woodall a,*, C.M. Oswalt b, J.A. Westfall c, C.H. Perry a, M.D. Nelson a, A.O. Finley d a USDA Forest Service, Northern Research Station, St. Paul, MN, United States b USDA Forest Service, Southern Research Station, Knoxville, TN, United States c USDA Forest Service, Northern Research Station, Newtown Square, PA, United States d Michigan State University, East Lansing, MI, United States ARTICLE INFO ABSTRACT Article history: Changes in tree species distributions are a potential impact of climate change on forest ecosystems. The Received 18 August 2008 examination of tree species shifts in forests of the eastern United States largely has been limited to Received in revised form 20 November 2008 simulation activities due to a lack of consistent, long-term forest inventory datasets. The goal of this Accepted 12 December 2008 study was to compare current geographic distributions of tree seedlings (trees with a diameter at breast height 2.5 cm) with biomass (trees with a diameter at breast height > 2.5 cm) for sets of northern, Keywords: southern, and general tree species in the eastern United States using a spatially balanced, region-wide Climate change forest inventory. Compared to mean latitude of tree biomass, mean latitude of seedlings was significantly Tree migration farther north (>20 km) for the northern study species, while southern species had no shift, and general United States Forest species demonstrated southern expansion. -
CBD First National Report
REPUBLIC OF TAJIKISTAN FIRST NATIONAL REPORT ON BIODIVERSITY CONSERVATION Dushanbe – 2003 1 REPUBLIC OF TAJIKISTAN FIRST NATIONAL REPORT ON BIODIVERSITY CONSERVATION Dushanbe – 2003 3 ББК 28+28.0+45.2+41.2+40.0 Н-35 УДК 502:338:502.171(575.3) NBBC GEF First National Report on Biodiversity Conservation was elaborated by National Biodiversity and Biosafety Center (NBBC) under the guidance of CBD National Focal Point Dr. N.Safarov within the project “Tajikistan Biodiversity Strategic Action Plan”, with financial support of Global Environmental Facility (GEF) and the United Nations Development Programme (UNDP). Copyright 2003 All rights reserved 4 Author: Dr. Neimatullo Safarov, CBD National Focal Point, Head of National Biodiversity and Biosafety Center With participation of: Dr. of Agricultural Science, Scientific Productive Enterprise «Bogparvar» of Tajik Akhmedov T. Academy of Agricultural Science Ashurov A. Dr. of Biology, Institute of Botany Academy of Science Asrorov I. Dr. of Economy, professor, Institute of Economy Academy of Science Bardashev I. Dr. of Geology, Institute of Geology Academy of Science Boboradjabov B. Dr. of Biology, Tajik State Pedagogical University Dustov S. Dr. of Biology, State Ecological Inspectorate of the Ministry for Nature Protection Dr. of Biology, professor, Institute of Plants Physiology and Genetics Academy Ergashev А. of Science Dr. of Biology, corresponding member of Academy of Science, professor, Institute Gafurov A. of Zoology and Parasitology Academy of Science Gulmakhmadov D. State Land Use Committee of the Republic of Tajikistan Dr. of Biology, Tajik Research Institute of Cattle-Breeding of the Tajik Academy Irgashev T. of Agricultural Science Ismailov M. Dr. of Biology, corresponding member of Academy of Science, professor Khairullaev R. -
Geowatch December 2007, Issue 34
GeoWatch December 2007, Issue 34 Table of Contents • Keynote: GeoSIG Celebrates 15th Year ...................................................................................................................................1 • Earthquake Monitoring System Above 3’200 m Altitude, Lake Sarez, Tajikistan .....................................................................1 • Latest Features and Improvements in GeoDAS.......................................................................................................................3 • EVACES’07 was held during 24-26 October 2007, Porto, Portugal .........................................................................................7 Keynote: GeoSIG Celebrates 15th Year We are proudly celebrating our 15th year. Within these 15 years, starting from a vision, we have strongly grown to a large, well-known, worldwide family with all of our customers, representatives, affiliates, employees and suppliers. We believe that it is our family that brings the best out of us by encouraging, demanding, listening, questioning, teaching, learning, researching and most importantly responsibly valuing all that we are standing for. Many of our liaisons are more than just business links which enabled GeoSIG to deliver optimum products, solutions and services with the best value regarding any specific requirement. With this opportunity we would most frankly like to thank to everyone that have contributed to the development and strength of this family and its continuing success towards many new endeavours. We like to smile with you… Earthquake Monitoring System Above 3’200 m Altitude, Lake Sarez, Tajikistan A massive landslide triggered by a strong earthquake in 1911 became a large dam along the Murghob River in the Pamir mountains of Tajikistan, now called the Usoi Dam. Lake sarez is the resulting lake that is formed above surrounding drainages at an elevation greater than 3200m. The lake is about 56 km long, 3.5 km wide and 500 m deep, which holds an estimated 17 km3 of water. -
Mapping the Flow of Forest Migration Through the City Under Climate Change Keeffe, Greg; Han, Qiyao
www.ssoar.info Mapping the flow of forest migration through the city under climate change Keeffe, Greg; Han, Qiyao Veröffentlichungsversion / Published Version Zeitschriftenartikel / journal article Empfohlene Zitierung / Suggested Citation: Keeffe, G., & Han, Q. (2019). Mapping the flow of forest migration through the city under climate change. Urban Planning, 4(1), 139-151. https://doi.org/10.17645/up.v4i1.1753 Nutzungsbedingungen: Terms of use: Dieser Text wird unter einer CC BY Lizenz (Namensnennung) zur This document is made available under a CC BY Licence Verfügung gestellt. Nähere Auskünfte zu den CC-Lizenzen finden (Attribution). For more Information see: Sie hier: https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0/deed.de Urban Planning (ISSN: 2183–7635) 2019, Volume 4, Issue 1, Pages 139–151 DOI: 10.17645/up.v4i1.1753 Article Mapping the Flow of Forest Migration through the City under Climate Change Qiyao Han * and Greg Keeffe School of Natural and Built Environment, Queen’s University Belfast, Belfast, BT7 1NN, UK; E-Mails: [email protected] (Q.H.), [email protected] (G.K.) * Corresponding author Submitted: 24 September 2018 | Accepted: 12 October 2018 | Published: 21 February 2019 Abstract Rapid climate change will create extreme problems for the biota of the planet. Much of it will have to migrate towards the poles at a rate far beyond normal speeds. In this context, the concept of assisted migration has been proposed to facilitate the migration of trees. Yet current practices of assisted migration focus on “where tree species should be in the future” and thus have many uncertainties. -
Diversity of the Mountain Flora of Central Asia with Emphasis on Alkaloid-Producing Plants
diversity Review Diversity of the Mountain Flora of Central Asia with Emphasis on Alkaloid-Producing Plants Karimjan Tayjanov 1, Nilufar Z. Mamadalieva 1,* and Michael Wink 2 1 Institute of the Chemistry of Plant Substances, Academy of Sciences, Mirzo Ulugbek str. 77, 100170 Tashkent, Uzbekistan; [email protected] 2 Institute of Pharmacy and Molecular Biotechnology, Heidelberg University, Im Neuenheimer Feld 364, 69120 Heidelberg, Germany; [email protected] * Correspondence: [email protected]; Tel.: +9-987-126-25913 Academic Editor: Ipek Kurtboke Received: 22 November 2016; Accepted: 13 February 2017; Published: 17 February 2017 Abstract: The mountains of Central Asia with 70 large and small mountain ranges represent species-rich plant biodiversity hotspots. Major mountains include Saur, Tarbagatai, Dzungarian Alatau, Tien Shan, Pamir-Alai and Kopet Dag. Because a range of altitudinal belts exists, the region is characterized by high biological diversity at ecosystem, species and population levels. In addition, the contact between Asian and Mediterranean flora in Central Asia has created unique plant communities. More than 8100 plant species have been recorded for the territory of Central Asia; about 5000–6000 of them grow in the mountains. The aim of this review is to summarize all the available data from 1930 to date on alkaloid-containing plants of the Central Asian mountains. In Saur 301 of a total of 661 species, in Tarbagatai 487 out of 1195, in Dzungarian Alatau 699 out of 1080, in Tien Shan 1177 out of 3251, in Pamir-Alai 1165 out of 3422 and in Kopet Dag 438 out of 1942 species produce alkaloids. The review also tabulates the individual alkaloids which were detected in the plants from the Central Asian mountains. -
Building Climate Resilience in Pyanj River Basin: Irrigation and Flood
Initial Environmental Examination April 2013 TAJ: Building Climate Resilience in the Pyanj River Basin Irrigation and Flood Management Prepared by the Ministry of Land Reclamation and Water Resources (MLRWR) and the State Unitary Enterprise for Housing and Communal Services Kochagi Manzillu Kommunali (KMK, formerly Tajikkomunservices) for the Asian Development Bank. ABBREVIATIONS ADB - Asian Development Bank AP - Affected Population/Person/Party CEP - Committee for Environmental Protection under the Government of Tajikistan EA - Executing Agency EC - Erosion Control EIA - Environmental Impact Assessment EMMP - Environmental Management and Monitoring Plan ES - Environmental Specialist ESM - Environmental Supervisor and Monitor Expert GBAO - Gorno-Badakhshan Autonomous Oblast (Province) GOST Gosudartsvennye Standarty (Russian Technical Standards) GoT - Government of Tajikistan IEE - Initial Environmental Examination LARC - Land Acquisition and Resettlement Committee LARP - Land Acquisition and Resettlement Plan MLRWR - Ministry of Land Reclamation and Water Resources NGO - Non Governmental Organization PC - Public Consultation PIU - Project Implementation Unit PMU - Project Management Unit SEE - State Ecological Expertise SOP - Standard Operation Procedure SR - Sensitive Receiver SSEMP - Site Specific Environmental Management Plan TD - Temporary Drainage TOR - Terms of Reference CONTENTS Page EXECUTIVE SUMMARY I I. INTRODUCTION 1 A. Background 1 B. Policy and Statutory Requirements in Tajikistan 1 C. Asian Development Bank Safeguard Policies 2009 5 II. DESCRIPTION OF THE PROJECT 6 A. Project Location. 11 III. DESCRIPTION OF EXISTING ENVIRONMENT IN THE PROJECT AREA 28 A. Physical Environment 28 B. Biological Environment 41 C. Socio-Economic and Physical Cultural Resources 46 IV. SCREENING OF POTENTIAL ENVIRONMENTAL IMPACTS OF THE PROJECT AND MITIGATION MEASURES 52 A. Beneficial impacts and maximization measures 53 A. Adverse impacts and mitigation measures 54 B. -
Effects on Ecosystems
10 Effects on Ecosystems J.M. MELILLO, T.V. CALLAGHAN, F.I. WOODWARD, E. SALATI, S.K. SINHA Contributors: /. Aber; V. Alexander; J. Anderson; A. Auclair; F. Bazzaz; A. Breymeyer; A. Clarke; C. Field; J.P. Grime; R. Gijford; J. Goudrian; R. Harris; I. Heaney; P. Holligan; P. Jarvis; L. Joyce; P. Levelle; S. Linder; A. Linkins; S. Long; A. Lugo, J. McCarthy, J. Morison; H. Nour; W. Oechel; M. Phillip; M. Ryan; D. Schimel; W. Schlesinger; G. Shaver; B. Strain; R. Waring; M. Williamson. CONTENTS Executive Summary 287 10.2.2.2.3 Decomposition 10.2.2.2.4 Models of ecosystem response to 10.0 Introduction 289 climate change 10.2.2.3 Large-scale migration of biota 10.1 Focus 289 10.2.2.3.1 Vegetation-climate relationships 10.2.2.3.2 Palaeo-ecological evidence 10.2 Effects of Increased Atmospheric CO2 and 10.2.2.4 Summary Climate Change on Terrestrial Ecosystems 289 10.2.1 Plant and Ecosystem Responses to 10.3 The Effects of Terrestrial Ecosystem Changes Elevated C02 289 on the Climate System 10.2.1.1 Plant responses 289 10.3.1 Carbon Cycling in Terrestrial Ecosystems 10.2.1.1.1 Carbon budget 289 10 3.1 1 Deforestation in the Tropics 10.2.1.1.2 Interactions between carbon dioxide and 10.3.1 2 Forest regrowth in the mid-latitudes of temperature 290 the Northern Hemisphere 10.2.1.1.3 Carbon dioxide and environmental 10 3.1.3 Eutrophication and toxification in the stress 290 mid-latitudes of the Northern Hemisphere 10.2.1.1.4 Phenology and senescence 291 10.3.2 Reforestation as a Means of Managing 10.2.1.2 Community and ecosystem responses to Atmospheric