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Wetlands of the Nile Basin the Many Eco for Their Liveli This Chapt Distribution, Functions and Contribution to Contribution Livelihoods They Provide
important role particular imp into wetlands budget (Sutch 11 in the Blue N icantly 1110difi Wetlands of the Nile Basin the many eco for their liveli This chapt Distribution, functions and contribution to contribution livelihoods they provide. activities, ane rainfall (i.e. 1 Lisa-Maria Rebelo and Matthew P McCartney climate chan: food securit; currently eX' arc under tb Key messages water resour support • Wetlands occur extensively across the Nile Basin and support the livelihoods ofmillions of related ;;ervi people. Despite their importance, there are big gaps in the knowledge about the current better evalu: status of these ecosystems, and how populations in the Nile use them. A better understand systematic I ing is needed on the ecosystem services provided by the difl:erent types of wetlands in the provide. Nile, and how these contribute to local livelihoods. • While many ofthe Nile's wetlands arc inextricably linked to agricultural production systems the basis for making decisions on the extent to which, and how, wetlands can be sustainably used for agriculture is weak. The Nile I: • Due to these infi)fl11atio!1 gaps, the future contribution of wetlands to agriculture is poorly the basin ( understood, and wetlands are otten overlooked in the Nile Basin discourse on water and both the E agriculture. While there is great potential for the further development of agriculture and marsh, fen, fisheries, in particular in the wetlands of Sudan and Ethiopia, at the same time many that is stat wetlands in the basin are threatened by poor management practices and populations. which at \, In order to ensure that the future use of wetlands for agriculture will result in net benefits (i.e. -
Outcomes of the EU Horizon 2020 DAFNE PROJECT the Omo
POLICY BRIEF October 2020 Outcomes of the EU Horizon 2020 DAFNE PROJECT The Omo-Turkana River Basin Progress towards cooperative frameworks KEY POLICY MESSAGES The OTB has reached a stage of pivotal importance for future development; the time to establish a cooperative framework on water governance is now. Transparency and accountability must be improved in order to facilitate the sharing of data and information, increasing trust and reducing the perception of risk. Benefit-sharing which extends beyond energy could enhance regional integration and improve sustainable development within the basin . THE OMO-TURKANA RIVER BASIN potential for hydropower and irrigation schemes that are, if scientifically and equitably managed, crucial to lift millions within and outside the basin out of extreme poverty; this has led to transboundary cooperation in recent years. This policy brief is derived from research conducted under the €5.5M four-year EU Horizon 2020 and Swiss funded ‘DAFNE’ project which concerns the promotion of integrated and adaptive water resources management, explicitly addressing the WEF Nexus and aiming to promote a sustainable economy in regions where new infrastructure and expanding The Omo-Turkana River Basin (OTB) – for the agriculture has to be balanced with social, purposes of the DAFNE Project – comprises of economic and environmental needs. The project two main water bodies: the Omo River in takes a multi- and interdisciplinary approach to Ethiopia and Lake Turkana which it drains into. the formation of a decision analytical While the Omo River lies entirely within Ethiopian territory, Lake Turkana is shared by framework (DAF) for participatory and both Kenya and Ethiopia, with the majority of integrated planning, to allow the evaluation of Lake Turkana residing within Kenya. -
Historical Survey of Limmu Genet Town from Its Foundation up to Present
INTERNATIONAL JOURNAL OF SCIENTIFIC & TECHNOLOGY RESEARCH VOLUME 6, ISSUE 07, JULY 2017 ISSN 2277-8616 Historical Survey Of Limmu Genet Town From Its Foundation Up To Present Dagm Alemayehu Tegegn Abstract: The process of modern urbanization in Ethiopia began to take shape since the later part of the nineteenth century. The territorial expansion of emperor Menelik (r. 1889 –1913), political stability and effective centralization and bureaucratization of government brought relative acceleration of the pace of urbanization in Ethiopia; the improvement of the system of transportation and communication are identified as factors that contributed to this new phase of urban development. Central government expansion to the south led to the appearance of garrison centers which gradually developed to small- sized urban center or Katama. The garrison were established either on already existing settlements or on fresh sites and also physically they were situated on hill tops. Consequently, Limmu Genet town was founded on the former Limmu Ennarya state‘s territory as a result of the territorial expansion of the central government and system of administration. Although the history of the town and its people trace many year back to the present, no historical study has been conducted on. Therefore the aim of this study is to explore the history of Limmu Genet town from its foundation up to present. Keywords: Limmu Ennary, Limmu Genet, Urbanization, Development ———————————————————— 1. Historical Background of the Study Area its production. The production and marketing of forest coffee spread the fame and prestige of Limmu Enarya ( The early history of Limmu Oromo Mohammeed Hassen, 1994). The name Limmu Ennarya is The history of Limmu Genet can be traced back to the rise derived from a combination of the name of the medieval of the Limmu Oromo clans, which became kingdoms or state of Ennarya and the Oromo clan name who settled in states along the Gibe river basin. -
Somalia Water Sector: Ffgfg Experience for IWRM Fgfgfgfg
fffg Somalia Water Sector: Ffgfg Experience for IWRM fgfgfgfg Eng . Ahmed Mohamed Hassan MoEWR Ministry of Energy and Water Resources Federal Government of Somalia List of contents • Somalia: general background • Major river basin Somalia • Drivers shaping the Somali water sector • Existing Legal and Regulatory Framework • Major Challenges for river basin • The Rivers’ role in Somalia’s Economic Development • Conclusions Somalia – General background Land areas: 637 655 sq. km Population: 15,3 million 2018, 35 million 2050 (est) Urban 40% GDP per capita: 500 USD/year Key Economic sectors: - Agriculture: 63% - Service: 30% - Industry: 7% The Major Water Resources Shared Rivers and Watercourses within Horn of African region ❑The Juba (Genale-Dawa) River Basin ❑ The Lag Dhere River Basin ❑ The Shabelle River Basin ❑ Ogaden Basin ❑ The Nugal Basin ❑ The Daroor Basin ❑ The Coastal Basin ❑The Merti Groundwater Aquifer ❑ The Shabelle Groundwater Aquifer Drivers shaping the Somali water sector Water is life in Somalia – a reality shaping unity, growth and wellbeing Rain provides 300 mm/yr. Transboundary sources add. Climate change unknown Population growth: A water vision: Imported grain Double number of Sustainable, equitable and feeds Somalia. secure water for national people, half unity, growth and well- Paid by livestock amount of water being, for all and in har- export & diaspora per person mony with nature transfers The global community wants to support: sector ready for priori- tization and investments, but needs institutional strengthening -
Local History of Ethiopia Ma - Mezzo © Bernhard Lindahl (2008)
Local History of Ethiopia Ma - Mezzo © Bernhard Lindahl (2008) ma, maa (O) why? HES37 Ma 1258'/3813' 2093 m, near Deresge 12/38 [Gz] HES37 Ma Abo (church) 1259'/3812' 2549 m 12/38 [Gz] JEH61 Maabai (plain) 12/40 [WO] HEM61 Maaga (Maago), see Mahago HEU35 Maago 2354 m 12/39 [LM WO] HEU71 Maajeraro (Ma'ajeraro) 1320'/3931' 2345 m, 13/39 [Gz] south of Mekele -- Maale language, an Omotic language spoken in the Bako-Gazer district -- Maale people, living at some distance to the north-west of the Konso HCC.. Maale (area), east of Jinka 05/36 [x] ?? Maana, east of Ankar in the north-west 12/37? [n] JEJ40 Maandita (area) 12/41 [WO] HFF31 Maaquddi, see Meakudi maar (T) honey HFC45 Maar (Amba Maar) 1401'/3706' 1151 m 14/37 [Gz] HEU62 Maara 1314'/3935' 1940 m 13/39 [Gu Gz] JEJ42 Maaru (area) 12/41 [WO] maass..: masara (O) castle, temple JEJ52 Maassarra (area) 12/41 [WO] Ma.., see also Me.. -- Mabaan (Burun), name of a small ethnic group, numbering 3,026 at one census, but about 23 only according to the 1994 census maber (Gurage) monthly Christian gathering where there is an orthodox church HET52 Maber 1312'/3838' 1996 m 13/38 [WO Gz] mabera: mabara (O) religious organization of a group of men or women JEC50 Mabera (area), cf Mebera 11/41 [WO] mabil: mebil (mäbil) (A) food, eatables -- Mabil, Mavil, name of a Mecha Oromo tribe HDR42 Mabil, see Koli, cf Mebel JEP96 Mabra 1330'/4116' 126 m, 13/41 [WO Gz] near the border of Eritrea, cf Mebera HEU91 Macalle, see Mekele JDK54 Macanis, see Makanissa HDM12 Macaniso, see Makaniso HES69 Macanna, see Makanna, and also Mekane Birhan HFF64 Macargot, see Makargot JER02 Macarra, see Makarra HES50 Macatat, see Makatat HDH78 Maccanissa, see Makanisa HDE04 Macchi, se Meki HFF02 Macden, see May Mekden (with sub-post office) macha (O) 1. -
Paranthropus Boisei: Fifty Years of Evidence and Analysis Bernard A
Marshall University Marshall Digital Scholar Biological Sciences Faculty Research Biological Sciences Fall 11-28-2007 Paranthropus boisei: Fifty Years of Evidence and Analysis Bernard A. Wood George Washington University Paul J. Constantino Biological Sciences, [email protected] Follow this and additional works at: http://mds.marshall.edu/bio_sciences_faculty Part of the Biological and Physical Anthropology Commons Recommended Citation Wood B and Constantino P. Paranthropus boisei: Fifty years of evidence and analysis. Yearbook of Physical Anthropology 50:106-132. This Article is brought to you for free and open access by the Biological Sciences at Marshall Digital Scholar. It has been accepted for inclusion in Biological Sciences Faculty Research by an authorized administrator of Marshall Digital Scholar. For more information, please contact [email protected], [email protected]. YEARBOOK OF PHYSICAL ANTHROPOLOGY 50:106–132 (2007) Paranthropus boisei: Fifty Years of Evidence and Analysis Bernard Wood* and Paul Constantino Center for the Advanced Study of Hominid Paleobiology, George Washington University, Washington, DC 20052 KEY WORDS Paranthropus; boisei; aethiopicus; human evolution; Africa ABSTRACT Paranthropus boisei is a hominin taxon ers can trace the evolution of metric and nonmetric var- with a distinctive cranial and dental morphology. Its iables across hundreds of thousands of years. This pa- hypodigm has been recovered from sites with good per is a detailed1 review of half a century’s worth of fos- stratigraphic and chronological control, and for some sil evidence and analysis of P. boi se i and traces how morphological regions, such as the mandible and the both its evolutionary history and our understanding of mandibular dentition, the samples are not only rela- its evolutionary history have evolved during the past tively well dated, but they are, by paleontological 50 years. -
Annex a Eastern Nile Water Simulation Model
Annex A Eastern Nile Water Simulation Model Hydrological boundary conditions 1206020-000-VEB-0017, 4 December 2012, draft Contents 1 Introduction 1 2 Hydraulic infrastructure 3 2.1 River basins and hydraulic infrastructure 3 2.2 The Equatorial Lakes basin 3 2.3 White Nile from Mongalla to Sobat mouth 5 2.4 Baro-Akobo-Sobat0White Nile Sub-basin 5 2.4.1 Abay-Blue Nile Sub-basin 6 2.4.2 Tekeze-Setit-Atbara Sub-basin 7 2.4.3 Main Nile Sub-basin 7 2.5 Hydrological characteristics 8 2.5.1 Rainfall and evaporation 8 2.5.2 River flows 10 2.5.3 Key hydrological stations 17 3 Database for ENWSM 19 3.1 General 19 3.2 Data availability 19 3.3 Basin areas 20 4 Rainfall and effective rainfall 23 4.1 Data sources 23 4.2 Extension of rainfall series 23 4.3 Effective rainfall 24 4.4 Overview of average monthly and annual rainfall and effective rainfall 25 5 Evaporation 31 5.1 Reference evapotranspiration 31 5.1.1 Penman-Montheith equation 32 5.1.2 Aerodynamic resistance ra 32 5.1.3 ‘Bulk’ surface resistance rs 33 5.1.4 Coefficient of vapour term 34 5.1.5 Net energy term 34 5.2 ET0 in the basins 35 5.2.1 Baro-Akobo-Sobat-White Nile 35 5.2.2 Abay-Blue Nile 36 5.2.3 Tekeze-Setit-Atbara 37 5.3 Open water evaporation 39 5.4 Open water evaporation relative to the refrence evapotranspiration 40 5.5 Overview of applied evapo(transpi)ration values 42 6 River flows 47 6.1 General 47 6.2 Baro-Akobo-Sobat-White Nile sub-basin 47 6.2.1 Baro at Gambela 47 Annex A Eastern Nile Water Simulation Model i 1206020-000-VEB-0017, 4 December 2012, draft 6.2.2 Baro upstream -
Lake Turkana and the Lower Omo the Arid and Semi-Arid Lands Account for 50% of Kenya’S Livestock Production (Snyder, 2006)
Lake Turkana & the Lower Omo: Hydrological Impacts of Major Dam & Irrigation Development REPORT African Studies Centre Sean Avery (BSc., PhD., C.Eng., C. Env.) © Antonella865 | Dreamstime © Antonella865 Consultant’s email: [email protected] Web: www.watres.com LAKE TURKANA & THE LOWER OMO: HYDROLOGICAL IMPACTS OF MAJOR DAM & IRRIGATION DEVELOPMENTS CONTENTS – VOLUME I REPORT Chapter Description Page EXECUTIVE(SUMMARY ..................................................................................................................................1! 1! INTRODUCTION .................................................................................................................................... 12! 1.1! THE(CONTEXT ........................................................................................................................................ 12! 1.2! THE(ASSIGNMENT .................................................................................................................................. 14! 1.3! METHODOLOGY...................................................................................................................................... 15! 2! DEVELOPMENT(PLANNING(IN(THE(OMO(BASIN ......................................................................... 18! 2.1! INTRODUCTION(AND(SUMMARY(OVERVIEW(OF(FINDINGS................................................................... 18! 2.2! OMO?GIBE(BASIN(MASTER(PLAN(STUDY,(DECEMBER(1996..............................................................19! 2.2.1! OMO'GIBE!BASIN!MASTER!PLAN!'!TERMS!OF!REFERENCE...........................................................................19! -
Genale Dawa III Dam Threatens Somalia's Water and Food Security
Genale Dawa III Dam Threatens Somalia's Water and Food Security Luuq, Somalia February 12, 2018 Prepared By: Hussein Amiin - [email protected] Professional Water Resources Engineer with over 10 years of Experience in Hydrologic and Hydraulic Analysis and Modeling Guled Ahmed (Wiliq) MSCE in Water Resources Management, over 15 years of Professional Engineering in Water Infrastructure Development Executive Summary: Juba river is one of two perennial rivers in Somalia that accounts for majority of the country’s agricultural output. Juba river also known as Genale Dawa river in Ethiopia, originates from the Ethiopian highlands. Three tributaries in Ethiopia converge near the Somalia national boundary to form the Juba river. The three tributaries are Genale, Dawa and Gestro rivers. Approximately 70% of the basin area for the Juba river lies within Ethiopia. The Ethiopian highlands originate about 90% of the precipitation forming the Juba river in Somalia. The Ethiopian Ministry of Water Resources (MoWR) has been conducting several high level feasibility studies of the potential hydropower of the country in order to harness the energy and grow their economy. Some of those studies were completed and are currently at implementation stage while others are ongoing. The studies that the MoWR has been conducting include Genale Dawa III (GD-3), Genale Dawa V (GD-5) and Genale Dawa VI (GD-6) as cascading system. The GD-3 is currently in construction and will be completed in early 2018; while the GD-5 is still unknown whether it has been abandoned or is part of a long term vision. Two British firms were awarded the contract to design and construct GD-6 dam, the first quarter of 2017. -
Observations of Pale and Rüppell's Fox from the Afar Desert
Dinets et al. Pale and Rüppell’s fox in Ethiopia Copyright © 2015 by the IUCN/SSC Canid Specialist Group. ISSN 1478-2677 Research report Observations of pale and Rüppell’s fox from the Afar Desert, Ethiopia Vladimir Dinets1*, Matthias De Beenhouwer2 and Jon Hall3 1 Department of Psychology, University of Tennessee, Knoxville, Tennessee 37996, USA. Email: [email protected] 2 Biology Department, University of Leuven, Kasteelpark Arenberg 31-2435, BE-3001 Heverlee, Belgium. 3 www.mammalwatching.com, 450 West 42nd St., New York, New York 10036, USA. * Correspondence author Keywords: Africa, Canidae, distribution, Vulpes pallida, Vulpes rueppellii. Abstract Multiple sight records of pale and Rüppell’s foxes from northwestern and southern areas of the Afar De- sert in Ethiopia extend the ranges of both species in the region. We report these sightings and discuss their possible implications for the species’ biogeography. Introduction 2013 during a mammalogical expedition. Foxes were found opportu- nistically during travel on foot or by vehicle, as specified below. All coordinates and elevations were determined post hoc from Google The Afar Desert (hereafter Afar), alternatively known as the Afar Tri- Earth. Distances were estimated visually. angle, Danakil Depression, or Danakil Desert, is a large arid area span- ning Ethiopia, Eritrea, Djibouti and Somaliland (Mengisteab 2013). Its fauna remains poorly known, as exemplified by the fact that the first Results possible record of Canis lupus dates back only to 2004 (Tiwari and Sillero-Zubiri 2004; note that the identification in this case is still On 14 May 2007, JH saw a fox in degraded desert near the town of uncertain). -
Remote Sensing and Regionalization for Integrated Water Resources Modeling,In Upper and Middle Awash River Basin, Ethiopia
REMOTE SENSING AND REGIONALIZATION FOR INTEGRATED WATER RESOURCES MODELING IN UPPER AND MIDDLE AWASH RIVER BASIN, ETHIOPIA HABTE GEBEYEHU LIKASA February, 2013 SUPERVISORS: DR. ING. T.H.M. (TOM) RIENTJES DR. IR. C. (CHRISTIAAN) VAN DER TOL REMOTE SENSING AND REGIONALIZATION FOR INTEGRATED WATER RESOURCES MODELING IN UPPER AND MIDDLE AWASH RIVER BASIN, ETHIOPIA HABTE GEBEYEHU LIKASA Enschede, the Netherlands, [February, 2013] Thesis submitted to the Faculty of Geo-Information Science and Earth Observation of the University of Twente in partial fulfillment of the requirements for the degree of Master of Science in Geo-information Science and Earth Observation. Specialization: [Water Resources and Environmental Management)] SUPERVISORS: DR. ING. T.H.M. (TOM) RIENTJES DR. IR. C. (CHRISTIAAN) VAN DER TOL THESIS ASSESSMENT BOARD: Dr. ir. C.M.M. (Chris) Mannaerts (Chair) Dr. Paolo Reggiani (External Examiner, Deltares Delft, The Netherlands) Etc DISCLAIMER This document describes work undertaken as part of a programme of study at the Faculty of Geo-Information Science and Earth Observation of the University of Twente. All views and opinions expressed therein remain the sole responsibility of the author, and do not necessarily represent those of the Faculty. ABSTRACT Water resources have an enormous impact on the economic development and environmental protection. Water resources available in different forms and can be obtained from different sources. However mostly, water resources assessment and management relies on available stream flow measurements. But, in developing country like Ethiopia most of river basins are ungauged. Therefore, applying remote sensing and regionalization for integrated water resources modeling in poorly gauged river basin is crucial. -
Lieberman 2001E.Pdf
news and views Another face in our family tree Daniel E. Lieberman The evolutionary history of humans is complex and unresolved. It now looks set to be thrown into further confusion by the discovery of another species and genus, dated to 3.5 million years ago. ntil a few years ago, the evolutionary history of our species was thought to be Ureasonably straightforward. Only three diverse groups of hominins — species more closely related to humans than to chim- panzees — were known, namely Australo- pithecus, Paranthropus and Homo, the genus to which humans belong. Of these, Paran- MUSEUMS OF KENYA NATIONAL thropus and Homo were presumed to have evolved between two and three million years ago1,2 from an early species in the genus Australopithecus, most likely A. afarensis, made famous by the fossil Lucy. But lately, confusion has been sown in the human evolutionary tree. The discovery of three new australopithecine species — A. anamensis3, A. garhi 4 and A. bahrelghazali5, in Kenya, Ethiopia and Chad, respectively — showed that genus to be more diverse and Figure 1 Two fossil skulls from early hominin species. Left, KNM-WT 40000. This newly discovered widespread than had been thought. Then fossil is described by Leakey et al.8. It is judged to represent a new species, Kenyanthropus platyops. there was the finding of another, as yet poorly Right, KNM-ER 1470. This skull was formerly attributed to Homo rudolfensis1, but might best be understood, genus of early hominin, Ardi- reassigned to the genus Kenyanthropus — the two skulls share many similarities, such as the flatness pithecus, which is dated to 4.4 million years of the face and the shape of the brow.