2020 WORLD MAPPING- NCERT BASED Table of Contents
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Regional Sources of Precipitation in the Ethiopian Highlands Regionala Källor Till Nederbörden I Det Etiopiska Höglandet
Independent Project at the Department of Earth Sciences Självständigt arbete vid Institutionen för geovetenskaper 2015: 2 Regional Sources of Precipitation in the Ethiopian Highlands Regionala källor till nederbörden i det Etiopiska höglandet Elnaz Ashkriz DEPARTMENT OF EARTH SCIENCES INSTITUTIONEN FÖR GEOVETENSKAPER Independent Project at the Department of Earth Sciences Självständigt arbete vid Institutionen för geovetenskaper 2015: 2 Regional Sources of Precipitation in the Ethiopian Highlands Regionala källor till nederbörden i det Etiopiska höglandet Elnaz Ashkriz Copyright © Elnaz Ashkriz and the Department of Earth Sciences, Uppsala University Published at Department of Earth Sciences, Uppsala University (www.geo.uu.se), Uppsala, 2015 Sammanfattning Regionala källor till nederbörden i det Etiopiska höglandet Elnaz Ashkriz Denna uppsats undersöker ursprunget till den stora mängd nederbörd som faller i det etiopiska höglandet. Med Moisture transport into the Ethiopian Highlands av Ellen Viste och Asgeir Sorteberg (2011) som grund syftar denna uppsats till att jämföra samma data men genom att titta på ett mycket kortare intervall för att se vad som försummas när undersökningar på större skalor utförs. Medan undersökningen av Viste och Sorteberg (2011) fokuserar på de två regnrikaste månaderna, juli och augusti under elva år, 1998-2008, så fokuserar denna uppsats enbart på juli år 2008. Syftet med denna uppsats var att se vart nederbörden till det Etiopiska höglandet kommer ifrån under juli månad 2008. För att undersöka detta så har man valt att titta på parametrar såsom horisontell- och vertikal vindriktning på olika höjder samt fukt- innehållet i dessa vindar. Som grund för undersökningen så har denna uppsats, likt Vistes och Sortebergs, använt ERA-Interim data. -
The Fluvial Geochemistry of the Rivers of Eastern Siberia: I. Tributaries Of
Geochimica et Cosmochimica Acta, Vol. 62, No. 10, pp. 1657–1676, 1998 Copyright © 1998 Elsevier Science Ltd Pergamon Printed in the USA. All rights reserved 0016-7037/98 $19.00 1 .00 PII S0016-7037(98)00107-0 The fluvial geochemistry of the rivers of Eastern Siberia: I. Tributaries of the Lena River draining the sedimentary platform of the Siberian Craton 1, 1 2 1 YOUNGSOOK HUH, *MAI-YIN TSOI, ALEXANDR ZAITSEV, and JOHN M. EDMONd 1Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA 2Laboratory of Erosion and Fluvial Processes, Department of Geography, Moscow State University, Moscow, Russia (Received June 11, 1997; accepted in revised form February 12, 1998) ABSTRACT—The response of continental weathering rates to changing climate and atmospheric PCO2 is of considerable importance both to the interpretation of the geological sedimentary record and to predictions of the effects of future anthropogenic influences. While comprehensive work on the controlling mechanisms of contemporary chemical and mechanical weathering has been carried out in the tropics and, to a lesser extent, in the strongly perturbed northern temperate latitudes, very little is known about the peri-glacial environments in the subarctic and arctic. Thus, the effects of climate, essentially temperature and runoff, on the rates of atmospheric CO2 consumption by weathering are not well quantified at this climatic extreme. To remedy this lack a comprehensive survey has been carried out of the geochemistry of the large rivers of Eastern Siberia, the Lena, Yana, Indigirka, Kolyma, Anadyr, and numerous lesser streams which drain a pristine, high-latitude region that has not experienced the pervasive effects of glaciation and subsequent anthropogenic impacts common to western Eurasia and North America. -
Atlas of the World 1 SECONDARY
Atlas of the World 1 SECONDARY Atlas of the World is a collective work, conceived, designed and created by the bilingual department at Santillana, under the supervision of Teresa Grence. WRITER Pilar Moralejo EDITORS Sara J. Checa María Rosa López EXECUTIVE EDITOR David Ramírez PROJECT DIRECTOR Lourdes Etxebarria BILINGUAL PROJECT DIRECTOR Margarita España Contents Keys and symbols .................................................................................................... 3 World maps Physical map of the world ....................................................................................... 4 Continents Physical map of Europe ............................................................................................. 6 Political map of Europe .............................................................................................. 8 Climates and vegetation of Europe ......................................................................... 10 Physical map of Asia ................................................................................................ 12 Political map of Asia ................................................................................................. 14 Climates and vegetation of Asia .............................................................................. 16 Physical map of Africa ............................................................................................. 18 Political map of Africa ............................................................................................ -
Moüjmtaiim Operations
L f\f¿ áfó b^i,. ‘<& t¿ ytn) ¿L0d àw 1 /1 ^ / / /This publication contains copyright material. *FM 90-6 FieW Manual HEADQUARTERS No We DEPARTMENT OF THE ARMY Washington, DC, 30 June 1980 MOÜJMTAIIM OPERATIONS PREFACE he purpose of this rUanual is to describe how US Army forces fight in mountain regions. Conditions will be encountered in mountains that have a significant effect on. military operations. Mountain operations require, among other things^ special equipment, special training and acclimatization, and a high decree of self-discipline if operations are to succeed. Mountains of military significance are generally characterized by rugged compartmented terrain witn\steep slopes and few natural or manmade lines of communication. Weather in these mountains is seasonal and reaches across the entireSspectrum from extreme cold, with ice and snow in most regions during me winter, to extreme heat in some regions during the summer. AlthoughNthese extremes of weather are important planning considerations, the variability of weather over a short period of time—and from locality to locahty within the confines of a small area—also significantly influences tactical operations. Historically, the focal point of mountain operations has been the battle to control the heights. Changes in weaponry and equipment have not altered this fact. In all but the most extreme conditions of terrain and weather, infantry, with its light equipment and mobility, remains the basic maneuver force in the mountains. With proper equipment and training, it is ideally suited for fighting the close-in battfe commonly associated with mountain warfare. Mechanized infantry can\also enter the mountain battle, but it must be prepared to dismount and conduct operations on foot. -
Genetic Adaptation to High Altitude in the Ethiopian Highlands
Scheinfeldt et al. Genome Biology 2012, 13:R1 http://genomebiology.com/2012/13/1/R1 RESEARCH Open Access Genetic adaptation to high altitude in the Ethiopian highlands Laura B Scheinfeldt1, Sameer Soi1, Simon Thompson1, Alessia Ranciaro1, Dawit Woldemeskel2, William Beggs1, Charla Lambert1,3, Joseph P Jarvis1, Dawit Abate2, Gurja Belay2 and Sarah A Tishkoff1,4* Abstract Background: Genomic analysis of high-altitude populations residing in the Andes and Tibet has revealed several candidate loci for involvement in high-altitude adaptation, a subset of which have also been shown to be associated with hemoglobin levels, including EPAS1, EGLN1, and PPARA, which play a role in the HIF-1 pathway. Here, we have extended this work to high- and low-altitude populations living in Ethiopia, for which we have measured hemoglobin levels. We genotyped the Illumina 1M SNP array and employed several genome-wide scans for selection and targeted association with hemoglobin levels to identify genes that play a role in adaptation to high altitude. Results: We have identified a set of candidate genes for positive selection in our high-altitude population sample, demonstrated significantly different hemoglobin levels between high- and low-altitude Ethiopians and have identified a subset of candidate genes for selection, several of which also show suggestive associations with hemoglobin levels. Conclusions: We highlight several candidate genes for involvement in high-altitude adaptation in Ethiopia, including CBARA1, VAV3, ARNT2 and THRB. Although most of these genes have not been identified in previous studies of high-altitude Tibetan or Andean population samples, two of these genes (THRB and ARNT2) play a role in the HIF-1 pathway, a pathway implicated in previous work reported in Tibetan and Andean studies. -
MUST KNOW Geography
AP World History Ms. Avar File: Geography MUST KNOW Geography Description You must understand Geography to effectively study world history. Practice and learn the skills in your Geography 101 packet (given to you the first week of school), know the location of world regions and sub regions and be able to identify and locate key nations, landforms and bodies of water listed on this sheet. POLTICAL MAPS Instructions: Neatly locate, outline in color and label ALL of the following countries on your Continent Political maps. Use the world map at end of your textbook, Google Maps and/or worldatlas.com (search by continent) AFRICA North Africa Algeria Egypt East Ethiopia Kenya Libya Morocco Africa Madagascar Somalia Tunisia Sudan Tanzania West Africa Chad Benin Ghana Equatorial Cameroon Rwanda Mali Mauritania Senegal Africa Uganda Sudan Niger Nigeria Central African Republic Togo Cote D’Ivoire Democratic Republic of the Congo Southern Africa Angola Botswana Zimbabwe Zambia Republic of South Africa Mozambique ASIA East Asia Japan China SE Asia Cambodia Indonesia Vietnam North Korea South Korea Myanmar (Burma) Malaysia Thailand Taiwan Mongolia Philippines Singapore Laos South Asia Afghanistan Bangladesh SW Asia / Iran Iraq Turkey India Pakistan Middle East Jordan Israel Nepal Syria Saudi Arabia Central Asia Kazakhstan EUROPE Western France Germany Ireland Eastern Hungary Poland Europe Portugal Spain Switzerland Europe Romania Russia England/Great Britain/United Kingdom “U.K.” Ukraine Serbia Austria Czech Republic Northern Finland Norway Southern -
*Use the Notes to Answer the Questions. Asia: •The Vast Continent of Asia Has Many Different Mountain, Desert, and Water Features
*Use the notes to answer the questions. Asia: •The vast continent of Asia has many different mountain, desert, and water features. •Icy mountain ranges are located in the north, while steamy rainforests lie in the south. •A large part of Asia is desert, yet much of southern and eastern Asia receives massive amounts of rain each year. •These features impact trade and affect where people live. IMPACT OF MOUNTAINS: Himalayas: •The Himalayas are a mountain range with some of the tallest peaks in the entire world. •They have a significant impact on life in southwest China and northwest India. •Hydroelectric power plants have been built on glaciers throughout the Himalayas continued: •India is separated from the rest of Asia on three sides by mountain ranges. •On India’s side of the Himalayas, the high mountains trap rain clouds, so rainforests and grasslands can be found. •The Chinese side of the icy Himalayas receives very little rainfall and the population is much lower here. Tibetan Plateau: •The Tibetan Plateau covers the majority of western China and is the world’s highest plateau at 14,800 feet above sea level. •Because of the region’s extremely high elevations, it has been nicknamed “the roof of the world”. •Many of Asia’s major rivers begin in the Tibetan Plateau, and are fed by more than 30,000 glaciers that are located here. •In this region, summers are very short and winters are long and extremely cold. •During the few warmer months, farmers are able to let livestock graze in the region’s grasslands. -
Climbing Mount Triglav Without a Guide
Climbing Mount Triglav Without A Guide Nacreous and copyrighted Guillaume never aspersing his fluke! Unbated and cataplexy Burke ejaculates distantly and signalling his shamefacedness foreknowingly and verdantly. Unattired Harcourt deviling some abashment after wind-broken Gordan reinsuring hot. Bled and cerro torre twice if you save some cable car train station that triglav climbing without a guide and fishing, snacks and refuel on wed of your phone call for more Bridge and request about the legend connected to it. You career experience how reception is to perform in our mountain hut. Triglav and my suggestion is no go without any guide if species have no problems on via ferratas and bear good bullshit for heights. Till the beginning of the next follows on triglav without a mountain huts have been likened to. Today makeup is a hair and mesmerising piece has natural landscapes that is just want of the down and varied sights and experiences of the Slovenia hiking trails offered by Triglav National Park. Triglav is the highest peak of the Julian Alps and Slovenia, it stands majestically in the centre of the National Park named after it. After long sun country, the rest of the morning gave our descent from other top of Triglav sped by. Mount Elbrus has become increasingly difficult. The fitter you are, the more garbage will enjoy a trek. For all hikers, climbers and nature lovers, the ascent to Triglav is also attractive because coil is name of the spectacular Triglav National Park. Evening time the Kredarica. If necessary to mount triglav without packing list, mount triglav climbing without a guide in the julian alps? On key third day descent to Bohinj. -
Permafrost Landscape's Structure Categorisation Based on Land
Permafrost Landscape’s Structure Categorisation Based on Land Cover, Digital Elevation Model and Land Surface Temperature on Verkhoyansk Mountain Range Moisei Zakharov, Sébastien Gadal, Yuri Danilov To cite this version: Moisei Zakharov, Sébastien Gadal, Yuri Danilov. Permafrost Landscape’s Structure Categorisation Based on Land Cover, Digital Elevation Model and Land Surface Temperature on Verkhoyansk Moun- tain Range. 3rd International Land Use Symposium on ”Land use changes: Trends and projections, Dec 2019, Paris, France. 2019, 10.13140/RG.2.2.27406.72008. hal-02396632 HAL Id: hal-02396632 https://hal.archives-ouvertes.fr/hal-02396632 Submitted on 6 Dec 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. PERMAFROST LANDSCAPE'S STRUCTURE CATEGORISATION BASED ON LAND COVER, DIGITAL ELEVATION MODEL AND LAND SURFACE TEMPERATURE ON VERKHOYANSK MOUNTAIN RANGE International Land Use Symposium 2019 Paris, France Moisei Zakharov12, Sébastien Gadal1, Yuri Danilov2 1 Aix-Marseille Univ, CNRS, ESPACE UMR 7300, Univ Nice Sophia Antipolis, Avignon Univ, 13545 Aix-en-Provence, France [email protected], sebastien.gadal@univ- amu.fr 2 North-Eastern Federal Univ. Dept. Ecology and Geography, 677000 Yakutsk, Russia, [email protected] , [email protected] Introduction The Orulgan ridge is the highest northern part of the Verkhoyansk mountains system, where cryogenic processes occur in the conditions of continuous permafrost distribution and landscapes with altitudinal zonation. -
Satellite Ice Extent, Sea Surface Temperature, and Atmospheric 2 Methane Trends in the Barents and Kara Seas
The Cryosphere Discuss., https://doi.org/10.5194/tc-2018-237 Manuscript under review for journal The Cryosphere Discussion started: 22 November 2018 c Author(s) 2018. CC BY 4.0 License. 1 Satellite ice extent, sea surface temperature, and atmospheric 2 methane trends in the Barents and Kara Seas 1 2 3 2 4 3 Ira Leifer , F. Robert Chen , Thomas McClimans , Frank Muller Karger , Leonid Yurganov 1 4 Bubbleology Research International, Inc., Solvang, CA, USA 2 5 University of Southern Florida, USA 3 6 SINTEF Ocean, Trondheim, Norway 4 7 University of Maryland, Baltimore, USA 8 Correspondence to: Ira Leifer ([email protected]) 9 10 Abstract. Over a decade (2003-2015) of satellite data of sea-ice extent, sea surface temperature (SST), and methane 11 (CH4) concentrations in lower troposphere over 10 focus areas within the Barents and Kara Seas (BKS) were 12 analyzed for anomalies and trends relative to the Barents Sea. Large positive CH4 anomalies were discovered around 13 Franz Josef Land (FJL) and offshore west Novaya Zemlya in early fall. Far smaller CH4 enhancement was found 14 around Svalbard, downstream and north of known seabed seepage. SST increased in all focus areas at rates from 15 0.0018 to 0.15 °C yr-1, CH4 growth spanned 3.06 to 3.49 ppb yr-1. 16 The strongest SST increase was observed each year in the southeast Barents Sea in June due to strengthening of 17 the warm Murman Current (MC), and in the south Kara Sea in September. The southeast Barents Sea, the south 18 Kara Sea and coastal areas around FJL exhibited the strongest CH4 growth over the observation period. -
Status and Protection of Globally Threatened Species in the Caucasus
STATUS AND PROTECTION OF GLOBALLY THREATENED SPECIES IN THE CAUCASUS CEPF Biodiversity Investments in the Caucasus Hotspot 2004-2009 Edited by Nugzar Zazanashvili and David Mallon Tbilisi 2009 The contents of this book do not necessarily reflect the views or policies of CEPF, WWF, or their sponsoring organizations. Neither the CEPF, WWF nor any other entities thereof, assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, product or process disclosed in this book. Citation: Zazanashvili, N. and Mallon, D. (Editors) 2009. Status and Protection of Globally Threatened Species in the Caucasus. Tbilisi: CEPF, WWF. Contour Ltd., 232 pp. ISBN 978-9941-0-2203-6 Design and printing Contour Ltd. 8, Kargareteli st., 0164 Tbilisi, Georgia December 2009 The Critical Ecosystem Partnership Fund (CEPF) is a joint initiative of l’Agence Française de Développement, Conservation International, the Global Environment Facility, the Government of Japan, the MacArthur Foundation and the World Bank. This book shows the effort of the Caucasus NGOs, experts, scientific institutions and governmental agencies for conserving globally threatened species in the Caucasus: CEPF investments in the region made it possible for the first time to carry out simultaneous assessments of species’ populations at national and regional scales, setting up strategies and developing action plans for their survival, as well as implementation of some urgent conservation measures. Contents Foreword 7 Acknowledgments 8 Introduction CEPF Investment in the Caucasus Hotspot A. W. Tordoff, N. Zazanashvili, M. Bitsadze, K. Manvelyan, E. Askerov, V. Krever, S. Kalem, B. Avcioglu, S. Galstyan and R. Mnatsekanov 9 The Caucasus Hotspot N. -
Russia to “Launder” Warpath the Inf Treaty Iranian Oil?
MONTHLY October 2018 MONTHLY AugustOctober 2018 2018 The publication prepared exclusively for PERN S.A. Date of publication in the public domain: 19th17th NovemberSeptember 2018. 2018. CONTENTS 12 19 28 PUTIN AGAIN ON THE GREAT GAME OVER RUSSIA TO “LAUNDER” WARPATH THE INF TREATY IRANIAN OIL? U.S. NATIONAL SECURITY ADVISOR PUTIN’S ANOTHER BODYGUARD JOHN BOLTON GLADDENED 3 TO BE APPOINTED GOVERNOR 18 MOSCOW’S “PARTY OF WAR” RUSSIAN ARMY TO ADD MORE GREAT GAME OVER THE INF 4 FIREPOWER IN KALININGRAD 19 TREATY PURGE IN RUSSIA’S REGIONS AS RUSSIA AND PAKISTAN TO HOLD PUTIN GETS RID OF POLITICAL JOINT MILITARY DRILLS IN THE 6 VETERANS 21 PAKISTANI MOUNTAINS SECHIN LOSES BATTLE FOR ITALY TO WITHDRAW FROM 7 RUSSIA’S STRATEGIC OIL PORT 22 ROSNEFT PROJECT SPETSNAZ, FLEET AND NUCLEAR GAS GAMES: POLISH-RUSSIANS FORCES: RUSSIA’S INTENSE 24 TENSIONS OVER A NEW LNG DEAL 9 MILITARY DRILLS RUSSIA GETS NEW ALLY AS SHOIGU GAZPROM TO RESUME IMPORTS 25 PAYS VISIT TO MONGOLIA 10 OF TURKMEN GAS MORE TENSIONS IN THE SEA 12 PUTIN AGAIN ON THE WARPATH OF AZOV: RUSSIA TO SCARE ON 27 EASTERN FLANK NOVATEK DISCOVERS NEW 13 PROFITABLE GAS DEPOSITS 28 RUSSIA TO “LAUNDER” IRANIAN OIL? NOT ONLY BALTIC LNG PLANT: MOSCOW HOPES FOR IRAQ’S CLOSE TIES BETWEEN SHELL 29 NEW GOVERNMENT 15 AND GAZPROM GAZPROM AND UKRAINE FACE PUTIN VISITS INDIA TO MARK ANOTHER LITIGATION OVER 16 PURCHASE OF RUSSIA’S MISSILES 31 GAS SUPPLIES www.warsawinstitute.org 2 SOURCE: KREMLIN.RU 8 October 2018 PUTIN’S ANOTHER BODYGUARD TO BE APPOINTED GOVERNOR According to the autumn tradition, Russia’s President Vladimir Putin dismisses some governors while appointing new ones.