Modelling Net Primary Productivity and Above-Ground Biomass for Mapping of Spatial Biomass Distribution in Kazakhstan
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Our Arctic Nation a U.S
Connecting the United States to the Arctic OUR ARCTIC NATION A U.S. Arctic Council Chairmanship Initiative Cover Photo: Cover Photo: Hosting Arctic Council meetings during the U.S. Chairmanship gave the United States an opportunity to share the beauty of America’s Arctic state, Alaska—including this glacier ice cave near Juneau—with thousands of international visitors. Photo: David Lienemann, www. davidlienemann.com OUR ARCTIC NATION Connecting the United States to the Arctic A U.S. Arctic Council Chairmanship Initiative TABLE OF CONTENTS 01 Alabama . .2 14 Illinois . 32 02 Alaska . .4 15 Indiana . 34 03 Arizona. 10 16 Iowa . 36 04 Arkansas . 12 17 Kansas . 38 05 California. 14 18 Kentucky . 40 06 Colorado . 16 19 Louisiana. 42 07 Connecticut. 18 20 Maine . 44 08 Delaware . 20 21 Maryland. 46 09 District of Columbia . 22 22 Massachusetts . 48 10 Florida . 24 23 Michigan . 50 11 Georgia. 26 24 Minnesota . 52 12 Hawai‘i. 28 25 Mississippi . 54 Glacier Bay National Park, Alaska. Photo: iStock.com 13 Idaho . 30 26 Missouri . 56 27 Montana . 58 40 Rhode Island . 84 28 Nebraska . 60 41 South Carolina . 86 29 Nevada. 62 42 South Dakota . 88 30 New Hampshire . 64 43 Tennessee . 90 31 New Jersey . 66 44 Texas. 92 32 New Mexico . 68 45 Utah . 94 33 New York . 70 46 Vermont . 96 34 North Carolina . 72 47 Virginia . 98 35 North Dakota . 74 48 Washington. .100 36 Ohio . 76 49 West Virginia . .102 37 Oklahoma . 78 50 Wisconsin . .104 38 Oregon. 80 51 Wyoming. .106 39 Pennsylvania . 82 WHAT DOES IT MEAN TO BE AN ARCTIC NATION? oday, the Arctic region commands the world’s attention as never before. -
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PLATINUM The Journal of Threatened Taxa (JoTT) is dedicated to building evidence for conservaton globally by publishing peer-reviewed artcles online OPEN ACCESS every month at a reasonably rapid rate at www.threatenedtaxa.org. All artcles published in JoTT are registered under Creatve Commons Atributon 4.0 Internatonal License unless otherwise mentoned. JoTT allows allows unrestricted use, reproducton, and distributon of artcles in any medium by providing adequate credit to the author(s) and the source of publicaton. Journal of Threatened Taxa Building evidence for conservaton globally www.threatenedtaxa.org ISSN 0974-7907 (Online) | ISSN 0974-7893 (Print) SMALL WILD CATS SPECIAL ISSUE Short Communication Insights into the feeding ecology of and threats to Sand Cat Felis margarita Loche, 1858 (Mammalia: Carnivora: Felidae) in the Kyzylkum Desert, Uzbekistan Alex Leigh Brighten & Robert John Burnside 12 March 2019 | Vol. 11 | No. 4 | Pages: 13492–13496 DOI: 10.11609/jot.4445.11.4.13492-13496 For Focus, Scope, Aims, Policies, and Guidelines visit htps://threatenedtaxa.org/index.php/JoTT/about/editorialPolicies#custom-0 For Artcle Submission Guidelines, visit htps://threatenedtaxa.org/index.php/JoTT/about/submissions#onlineSubmissions For Policies against Scientfc Misconduct, visit htps://threatenedtaxa.org/index.php/JoTT/about/editorialPolicies#custom-2 For reprints, contact <[email protected]> The opinions expressed by the authors do not refect the views of the Journal of Threatened Taxa, Wildlife Informaton Liaison Development Society, Zoo Outreach Organizaton, or any of the partners. The journal, the publisher, the host, and the part- Publisher & Host ners are not responsible for the accuracy of the politcal boundaries shown in the maps by the authors. -
Ecoregions of Nevada Ecoregion 5 Is a Mountainous, Deeply Dissected, and Westerly Tilting Fault Block
5 . S i e r r a N e v a d a Ecoregions of Nevada Ecoregion 5 is a mountainous, deeply dissected, and westerly tilting fault block. It is largely composed of granitic rocks that are lithologically distinct from the sedimentary rocks of the Klamath Mountains (78) and the volcanic rocks of the Cascades (4). A Ecoregions denote areas of general similarity in ecosystems and in the type, quality, Vegas, Reno, and Carson City areas. Most of the state is internally drained and lies Literature Cited: high fault scarp divides the Sierra Nevada (5) from the Northern Basin and Range (80) and Central Basin and Range (13) to the 2 2 . A r i z o n a / N e w M e x i c o P l a t e a u east. Near this eastern fault scarp, the Sierra Nevada (5) reaches its highest elevations. Here, moraines, cirques, and small lakes and quantity of environmental resources. They are designed to serve as a spatial within the Great Basin; rivers in the southeast are part of the Colorado River system Bailey, R.G., Avers, P.E., King, T., and McNab, W.H., eds., 1994, Ecoregions and subregions of the Ecoregion 22 is a high dissected plateau underlain by horizontal beds of limestone, sandstone, and shale, cut by canyons, and United States (map): Washington, D.C., USFS, scale 1:7,500,000. are especially common and are products of Pleistocene alpine glaciation. Large areas are above timberline, including Mt. Whitney framework for the research, assessment, management, and monitoring of ecosystems and those in the northeast drain to the Snake River. -
Achieving Ecosystem Stability of Degraded Land in Karakalpakstan and Kyzylkum Desert
United Nations Development Programme/Global Environment Facility Government of Uzbekistan Achieving Ecosystem Stability of Degraded Land in Karakalpakstan and Kyzylkum Desert PIMS 3148 Project Final Evaluation Report Max Kasparek Tulkin Radjabov November 2012 Acknowledgements We would like to thank the staff and other people connected with the Ecosystem Stability Project who provid‐ ed a very constructive atmosphere during the final evaluation, which was carried out in a highly collegial spirit throughout. The project team gave us free access to all necessary information and facilitated meetings with the relevant people. We liked in particular the inspiring and sometimes controversial discussions. We wish to thank in particular the UNDP Country Office (Energy and Environment Programme), the Project Manager and all pro‐ ject staff and experts, the members of the Project Steering Committee and the partners in the Ministry of Agri‐ culture and other governmental agencies. The full support of the project team made it possible to conduct the tight travel schedule with a full meeting programme. Our sincerest thanks are also due to local stakeholders for providing information and for their great hospitality! Max Kasparek &Tulkin Radjabov Project Executing Partners Executing Agency: Forestry Department of the Ministry of Agriculture and Water Resources of the Government of Uzbekistan Principal Participating Academy of Sciences, Goskomzem, the Uzbekistan Hydrometeorological Partners: Service, and the State Committee for Nature Protection GEF Implementing Agency: United Nations Development Programme (UNDP) Evaluation Responsibility This Final Evaluation is undertaken by the UNDP Country Office (Energy & Environment Programme) in Uzbeki‐ stan in liaison with the UNDP Bratislava Regional Centre as the GEF Implementing Agency for this project. -
RBMP SEA Report ENG FINAL
European Union Water Initiative Plus for Eastern Partnership Countries (EUWI+) STRATEGIC ENVIRONMENTAL ASSESSMENT (SEA) OF THE DRAFTALAZANI-IORI RIVER BASIN MANAGEMENT PLAN SEA Report November 2020 2 This SEA report was prepared by the national SEA team established for the pilot project “The Application of a Strategic Environmental Assessment (SEA) for the Draft Alazani-Iori River Basin Management Plan” (hereinafter also the SEA pilot project): Ms. Elina Bakradze (water and soil quality aspects), Ms. Anna Rukhadze (biodiversity, habitats and protected areas), Ms. Lela Serebryakova (health related aspects), Mr. Giorgi Guliashvili (hydrology and natural hazards), Mr. Davit Darsavelidze (socio-economic aspects), Mr. Irakli Kobulia (cultural heritage aspects and GIS) and the UNECE national consultant Ms. Irma Melikishvili (the team leader also covering climate change aspects), under the guidance and supervision of the UNECE international consultant Mr. Martin Smutny. Maps: The thematic maps presented in the SEA Report are produced by Mr. Irakli Kobulia on the basis of the GIS database provided by the EUWI + programme. The SEA Report also includes maps developed in the framework of the EUWI + programme (under result 2) by the REC Caucasus, subcontractor of the EUWI+ programme. The SEA pilot project was carried out under the supervision of Mr. Alisher Mamadzhanov, the EUWI+ programme leader from UNECE with the support provided by Ms. Christine Kitzler and Mr. Alexander Belokurov, UNECE and Ms. Eliso Barnovi, the EUWI+ Country Representative -
Redalyc.The Arid and Dry Plant Formations of South America And
Darwiniana ISSN: 0011-6793 [email protected] Instituto de Botánica Darwinion Argentina López, Ramiro P.; Larrea Alcázar, Daniel; Macía, Manuel J. The arid and dry plant formations of south America and their floristic connections: new data, new interpretation? Darwiniana, vol. 44, núm. 1, julio, 2006, pp. 18-31 Instituto de Botánica Darwinion Buenos Aires, Argentina Available in: http://www.redalyc.org/articulo.oa?id=66944102 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative DARWINIANA 44(1): 18-31. 2006 ISSN 0011-6793 THE ARID AND DRY PLANT FORMATIONS OF SOUTH AMERICA AND THEIR FLORISTIC CONNECTIONS: NEW DATA, NEW INTERPRETATION? Ramiro P. López1, Daniel Larrea Alcázar2 & Manuel J. Macía3 1Associate Researcher, Herbario Nacional de Bolivia. Campus Universitario, Cotacota, calle 27 s/n, Casilla 3- 35121, La Paz, Bolivia; [email protected]; (author for correspondence). 2Postgrado en Ecología Tropical, Instituto en Ciencias Ambientales y Ecológicas, Universidad de Los Andes. La Hechicera s/n, Mérida 5101, Mérida, Venezuela. 3Real Jardín Botánico de Madrid (CSIC), Plaza de Murillo 2, E-28014 Madrid, España. Abstract. López, R. P., D. Larrea Alcázar & M. J. Macía. 2006. The arid and dry plant formations of South Ame- rica and their floristic connections: new data, new interpretation? Darwiniana 44(1): 18-31. In this study we aimed at testing two hypothesis about the biogeography of South America: (1) the existence of a marked discontinuity in the Andes of central Peru that separates the floras of northern and southern South America and (2) the occurrence of a more or less continuous semi-deciduous forest in South America during the Pleistocene. -
Burning Man Geology Black Rock Desert.Pdf
GEOLOGY OF THE BLACK ROCK DESERT By Cathy Busby Professor of Geology University of California Santa Barbara http://www.geol.ucsb.edu/faculty/busby BURNING MAN EARTH GUARDIANS PAVILION 2012 LEAVE NO TRACE Please come find me and Iʼll give you a personal tour of the posters! You are here! In one of the most amazing geologic wonderlands in the world! Fantastic rock exposure, spectacular geomorphic features, and a long history, including: 1. PreCambrian loss of our Australian neighbors by continental rifting, * 2. Paleozoic accretion of island volcanic chains like Japan (twice!), 3. Mesozoic compression and emplacement of a batholith, 4. Cenozoic stretching and volcanism, plus a mantle plume torching the base of the continent! Let’s start with what you can see on the playa and from the playa: the Neogene to Recent geology, which is the past ~23 million years (= Ma). Note: Recent = past 15,000 years http://www.terragalleria.com Then we’ll “build” the terrane you are standing on, beginning with a BILLION years ago, moving through the Paleozoic (old life, ~540-253 Ma), Mesozoic (age of dinosaurs, ~253-65 Ma)) and Cenozoic (age of mammals, ~65 -0 Ma). Neogene to Recent geology Black Rock Playa extends 100 miles, from Gerlach to the Jackson Mountains. The Black Rock Desert is divided into two arms by the Black Rock Range, and covers 1,000 square miles. Empire (south of Gerlach)has the U.S. Gypsum mine and drywall factory (brand name “Sheetrock”), and thereʼs an opal mine at base of Calico Mtns. Neogene to Recent geology BRP = The largest playa in North America “Playa” = a flat-bottomed depression, usually a dry lake bed 3,500ʼ asl in SW, 4,000ʼ asl in N Land speed record: 1997 - supersonic car, 766 MPH Runoff mainly from the Quinn River, which heads in Oregon ~150 miles north. -
Analysis of Dust Aerosol Retrievals Using Satellite Data in Central Asia
Article Analysis of Dust Aerosol Retrievals Using Satellite Data in Central Asia Longlei Li * and Irina N. Sokolik School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-404-754-1177 Received: 8 June 2018; Accepted: 19 July 2018; Published: 24 July 2018 Abstract: Several long-term monitoring of aerosol datasets from the Moderate Resolution Imaging Spectroradiometer (MODIS) on board Terra/Aqua, Multi-angle Imaging SpectroRadiometer (MISR), Sea-Viewing Wide Field-of-View Sensor (SeaWiFS) were used to derive the dust aerosol optical depth (DOD) in Central Asia based on the Angstrom exponent parameter and/or the particle shape. All sensors agree very well on the interannual variability of DOD. The seasonal analysis of DOD and dust occurrences identified the largest dust loading and the most frequent dust occurrence in the spring and summer, respectively. No significant trend was found during the research period in terms of both DOD and the dust occurrence. Further analysis of Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) aerosol products on a case-by-case basis in most dust months of 2007 suggested that the vertical structure is varying in terms of the extension and the dust loading from one event to another, although dust particles of most episodes have similar physical characteristics (particle shape and size). Our analysis on the vertical structure of dust plumes, the layer-integrated color ratio and depolarization ratio indicates a varied climate effect (e.g., the direct radiative impact) by mineral dust, dependent on the event being observed in Central Asia. -
01. Antarctica (√) 02. Arabia
01. Antarctica (√) 02. Arabia: https://en.wikipedia.org/wiki/Arabian_Desert A corridor of sandy terrain known as the Ad-Dahna desert connects the largeAn-Nafud desert (65,000 km2) in the north of Saudi Arabia to the Rub' Al-Khali in the south-east. • The Tuwaiq escarpment is a region of 800 km arc of limestone cliffs, plateaux, and canyons.[citation needed] • Brackish salt flats: the quicksands of Umm al Samim. √ • The Wahiba Sands of Oman: an isolated sand sea bordering the east coast [4] [5] • The Rub' Al-Khali[6] desert is a sedimentary basin elongated on a south-west to north-east axis across the Arabian Shelf. At an altitude of 1,000 m, the rock landscapes yield the place to the Rub' al-Khali, vast wide of sand of the Arabian desert, whose extreme southern point crosses the centre of Yemen. The sand overlies gravel or Gypsum Plains and the dunes reach maximum heights of up to 250 m. The sands are predominantly silicates, composed of 80 to 90% of quartz and the remainder feldspar, whose iron oxide-coated grains color the sands in orange, purple, and red. 03. Australia: https://en.wikipedia.org/wiki/Deserts_of_Australia Great Victoria Western Australia, South Australia 348,750 km2 134,650 sq mi 1 4.5% Desert Great Sandy Desert Western Australia 267,250 km2 103,190 sq mi 2 3.5% Tanami Desert Western Australia, Northern Territory 184,500 km2 71,200 sq mi 3 2.4% Northern Territory, Queensland, South Simpson Desert 176,500 km2 68,100 sq mi 4 2.3% Australia Gibson Desert Western Australia 156,000 km2 60,000 sq mi 5 2.0% Little Sandy Desert Western Australia 111,500 km2 43,100 sq mi 6 1.5% South Australia, Queensland, New South Strzelecki Desert 80,250 km2 30,980 sq mi 7 1.0% Wales South Australia, Queensland, New South Sturt Stony Desert 29,750 km2 11,490 sq mi 8 0.3% Wales Tirari Desert South Australia 15,250 km2 5,890 sq mi 9 0.2% Pedirka Desert South Australia 1,250 km2 480 sq mi 10 0.016% 04. -
Panthera Pardus) Range Countries
Profiles for Leopard (Panthera pardus) Range Countries Supplemental Document 1 to Jacobson et al. 2016 Profiles for Leopard Range Countries TABLE OF CONTENTS African Leopard (Panthera pardus pardus)...................................................... 4 North Africa .................................................................................................. 5 West Africa ................................................................................................... 6 Central Africa ............................................................................................. 15 East Africa .................................................................................................. 20 Southern Africa ........................................................................................... 26 Arabian Leopard (P. p. nimr) ......................................................................... 36 Persian Leopard (P. p. saxicolor) ................................................................... 42 Indian Leopard (P. p. fusca) ........................................................................... 53 Sri Lankan Leopard (P. p. kotiya) ................................................................... 58 Indochinese Leopard (P. p. delacouri) .......................................................... 60 North Chinese Leopard (P. p. japonensis) ..................................................... 65 Amur Leopard (P. p. orientalis) ..................................................................... 67 Javan Leopard -
Remote Sensing
remote sensing Article Quantitative Assessment of Vertical and Horizontal Deformations Derived by 3D and 2D Decompositions of InSAR Line-of-Sight Measurements to Supplement Industry Surveillance Programs in the Tengiz Oilfield (Kazakhstan) Emil Bayramov 1,2,*, Manfred Buchroithner 3 , Martin Kada 2 and Yermukhan Zhuniskenov 1 1 School of Mining and Geosciences, Nazarbayev University, 53 Kabanbay Batyr Ave, Nur-Sultan 010000, Kazakhstan; [email protected] 2 Methods of Geoinformation Science, Institute of Geodesy and Geoinformation Science, Technical University of Berlin, 10623 Berlin, Germany; [email protected] 3 Institute of Cartography, Helmholtzstr. 10, 01069 Dresden, Germany; [email protected] * Correspondence: [email protected] Abstract: This research focused on the quantitative assessment of the surface deformation veloci- ties and rates and their natural and man-made controlling factors at Tengiz Oilfield in Kazakhstan using the Small Baseline Subset remote sensing technique followed by 3D and 2D decompositions and cosine corrections to derive vertical and horizontal movements from line-of-sight (LOS) mea- Citation: Bayramov, E.; Buchroithner, surements. In the present research we applied time-series of Sentinel-1 satellite images acquired M.; Kada, M.; Zhuniskenov, Y. during 2018–2020. All ground deformation derivatives showed the continuous subsidence at the Quantitative Assessment of Vertical Tengiz oilfield with increasing velocity. 3D and 2D decompositions of LOS measurements to vertical and Horizontal Deformations movement showed that the Tengiz Oil Field 2018–2020 continuously subsided with the maximum Derived by 3D and 2D annual vertical deformation velocity around 70 mm. Based on the LOS measurements, the maximum Decompositions of InSAR annual subsiding velocity was observed to be 60 mm. -
Secondary Education in Kazakhstan
Reviews of National Policies for Education Reviews of Secondary Education in Kazakhstan This is the first OECD review of policies for secondary education in Kazakhstan. N Reviews of National Policies for Education This report evaluates the education reform agenda of Kazakhstan – its feasibility and ational Policies for Education focus – by taking stock of present-day strengths and weaknesses. It provides guidance on adjusting reform implementation plans in line with international experiences and best Secondary Education practices. This review also consolidates much of the previously dispersed (national) data on primary and secondary schools in Kazakhstan into a common analytical base of evidence. in Kazakhstan Contents Executive summary Chapter 1. Overview of the education system of Kazakhstan Chapter 2. Equity and effectiveness of schooling in Kazakhstan Chapter 3. Assessment of learning outcomes and teaching quality in Kazakhstan Chapter 4. Good policies for better teachers and school leadership in Kazakhstan Chapter 5. Education expenditure and financing mechanisms in Kazakhstan Chapter 6. Vocational education and training in Kazakhstan Chapter 7. Recommendations of the OECD review of secondary education in Kazakhstan S econdary Education in Kazakhstan Consult this publication on line at http://dx.doi.org/10.1787/9789264205208-en. This work is published on the OECD iLibrary, which gathers all OECD books, periodicals and statistical databases. Visit www.oecd-ilibrary.org for more information. ISBN 978-92-64-20521-5 91 2013 06 1 P 9HSTCQE*cafcbf+ Reviews of National Policies for Education Secondary Education in Kazakhstan This work is published on the responsibility of the Secretary-General of the OECD. The opinions expressed and arguments employed herein do not necessarily reflect the official views of the Organisation or of the governments of its member countries.