The Lake Chad Basin Aquifer System
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The Disappearance of Lake Chad: History of a Myth
The disappearance of Lake Chad: history of a myth Géraud Magrin1 Université Paris 1 Panthéon-Sorbonne, France Abstract The article explores the hydropolitics of Lake Chad. Scientific and popular views on the fate of Lake Chad differ widely. The supposed 'disappearance' of the Lake through water abstraction and climate change is a popular myth that endures because it serves a large set of heterogeneous interests, including those supporting inter-basin water transfers. Meanwhile scientific investigations show substantial and continuing Lake level fluctuations over time, and do not support its projected disappearance. The task is to understand how the myth of the disappearing Lake has been engendered and used, by studying the discourses and the strategies of the main stakeholders involved. The Lake has been protected so far from massive water abstraction, and inter-basin transfer projects, due to the fragmentation of its political management, new security threats, and the piecemeal nature of the interests in play. Key words: Lake Chad; environmental myths; hydropolitics; political ecology; inter-basin transfers Résumé Cet article aborde le lac Tchad d’un point de vue hydropolitique. Les discours scientifique et du grand public sur l'état du lac Tchad diffèrent largement. La « disparition » supposée du lac sous l’effet des prélèvements anthropiques pour l’irrigation et du changement climatique est un mythe qui perdure car il sert un ensemble d'intérêts hétérogènes, dont ceux favorables à un projet de transfert d'eau inter-bassins. Or les recherches scientifiques montrent que le lac a toujours fluctué au cours du temps, et que les dynamiques récentes ne conduisent pas à sa disparition, si souvent annoncée. -
Sitwa Report on Infrastructure Development
SITWA PROJECT: STRENGTHENING THE INSTITUTIONS FOR TRANSBOUNDARY WATER MANAGEMENT IN AFRICA CONSULTANCY SERVICES TO ASSESS THE NEEDS AND PREPARE AN ACTION PLAN FOR SITWA/ANBO SUPPORT SERVICES IN INFRASTRUCTURE DEVELOPMENT IN THE AFRICAN RIVER BASIN ORGANIZATIONS SITWA REPORT ON INFRASTRUCTURE DEVELOPMENT This document has been produced with the financial assistance of the European Union. The views expressed herein can in no way be taken to reflect the official opinion of the European Union RAPPORT SITWA SUR LE DÉVELOPPEMENT DES INFRASTRUCTURES DANS LES OBF AFRICAINS 3 Table des matiÈRES Table des matières ...................................................................................... 3 AbrEviations ............................................................................................... 5 Acknowledgements .................................................................................... 7 Executive summary .................................................................................... 8 List of tables .............................................................................................. 9 List of figures ............................................................................................ 9 1. Background and objectives of the consultancy ........................................ 10 1.1 ANBO’s historical background and objectives ............................................................................. 10 1.2 Background and objectives of SITWA ......................................................................................... -
Biomass Burning and Water Balance Dynamics in the Lake Chad Basin in Africa
Article Biomass Burning and Water Balance Dynamics in the Lake Chad Basin in Africa Forrest W. Black 1 , Jejung Lee 1,*, Charles M. Ichoku 2, Luke Ellison 3 , Charles K. Gatebe 4 , Rakiya Babamaaji 5, Khodayar Abdollahi 6 and Soma San 1 1 Department of Earth and Environmental Sciences, University of Missouri-Kansas City, Kansas City, MO 64110, USA; [email protected] (F.W.B.); [email protected] (S.S.) 2 Graduate Program, College of Arts & Sciences, Howard University, Washington, DC 20059, USA; [email protected] 3 Science Systems and Applications, Inc., Lanham, MD 20706, USA; [email protected] 4 Atmospheric Science Branch SGG, NASA Ames Research Center, Mail Code 245-5, ofc. 136, Moffett Field, CA 94035, USA; [email protected] 5 National Space Research and Development Agency (NASRDA), PMB 437, Abuja, Nigeria; [email protected] 6 Faculty of Natural Resources and Earth Sciences, Shahrekord University, P.O. Box 115, Shahrekord 88186-34141, Iran; [email protected] * Correspondence: [email protected]; Tel.: +1-816-235-6495 Abstract: The present study investigated the effect of biomass burning on the water cycle using a case study of the Chari–Logone Catchment of the Lake Chad Basin (LCB). The Chari–Logone catchment was selected because it supplies over 90% of the water input to the lake, which is the largest basin in central Africa. Two water balance simulations, one considering burning and one without, were compared from the years 2003 to 2011. For a more comprehensive assessment of the effects of burning, albedo change, which has been shown to have a significant impact on a number of Citation: Black, F.W.; Lee, J.; Ichoku, environmental factors, was used as a model input for calculating potential evapotranspiration (ET). -
Models and Methods of Tectonic Geomorphology and the Reconstruction of Hominin Landscapes
This is a repository copy of Landscapes of human evolution : models and methods of tectonic geomorphology and the reconstruction of hominin landscapes. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/11178/ Version: Accepted Version Article: Bailey, G.N. orcid.org/0000-0003-2656-830X, Reynolds, Sally and King, G.C.P. (2011) Landscapes of human evolution : models and methods of tectonic geomorphology and the reconstruction of hominin landscapes. Journal of Human Evolution. pp. 257-80. ISSN 0047-2484 https://doi.org/10.1016/j.jhevol.2010.01.004 Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ This is an author-created pdf. Cite as: In press, J Hum Evol (2010), doi:10.1016/j.jhevol.2010.01.004 Landscapes of human evolution: models and methods of tectonic geomorphology and the reconstruction of hominin landscapes Geoffrey N. Bailey 1 Sally C. Reynolds 2, 3 Geoffrey C. -
Region: West Africa (14 Countries) (Benin, Burkina Faso, Cameroon, Chad, Côte D’Ivoire, Gambia, Ghana, Guinea, Guinea Bissau, Mali, Niger, Senegal, Togo)
Region: West Africa (14 Countries) (Benin, Burkina Faso, Cameroon, Chad, Côte d’Ivoire, Gambia, Ghana, Guinea, Guinea Bissau, Mali, Niger, Senegal, Togo) Project title: Emergency assistance for early detection and prevention of avian influenza in Western Africa Project number: TCP/RAF/3016 (E) Starting date: November 2005 Completion date: April 2007 Government counterpart Ministries of Agriculture responsible for project execution: FAO contribution: US$ 400 000 Signed: ..................................... Signed: ........................................ (on behalf of Government) Jacques Diouf Director-General (on behalf of FAO) Date of signature: ..................... Date of signature: ........................ I. BACKGROUND AND JUSTIFICATION In line with the FAO/World Organization for Animal Health (OIE) Global Strategy for the Progressive Control of Highly Pathogenic Avian Influenza (HPAI), this project has been developed to provide support to the regional grouping of West African countries to strengthen emergency preparedness against the eventuality of HPAI being introduced into this currently free area. There is growing evidence that the avian influenza, which has been responsible for serious disease outbreaks in poultry and humans in several Asian countries since 2003, is spread through a number of sources, including poor biosecurity at poultry farms, movement of poultry and poultry products and live market trade, illegal and legal trade in wild birds. Although unproven, it is also suspected that the virus could possibly be carried over long distances along the migratory bird flyways to regions previously unaffected (Table 1) is a cause of serious concern for the region. Avian influenza subtype H5N1 could be transported along these routes to densely populated areas in the South Asian Subcontinent and to the Middle East, Africa and Europe. -
Palaeoecology of Africa*
Intimations on Quaternary palaeoecology of Africa* E.M. van Zinderen+Bakker Palynological Research Unit of the C.S.I.R. and the University of the Orange Free State at Bloemfontein 1. THE BIOGEOGRAPHIC PATTERN OF AFRICA of with of is little The biogeography Africa, as compared that Europe known and it is only in recent years that more detailed studies have been made of cer- of tain areas. Taxonomists working on groups lower plants and animals and even on flowering plants will still find many rich new areas for collecting in Africa, while the results of these taxonomic studies are the basis of any biogeo- graphic investigation. The study of the factors responsible for the present-day pattern of distribution of plants and animals has been initiated in Africa only The which directed towards fairly recently. present intimations, are mostly botanical problems, are therefore general in nature and are often hypothetical. They are only intended to indicate possible historical approaches to the study of biogeography of Africa. The flora and fauna of Africa, the continent for which some of the most an- cient radiometric dates have been assessed, must in consequence be old in origin. The priscotropical flora of the forests, savannas, mountains and deserts of Africa has been isolated from the other continents since mesozoic times and has wealth of in the flora. Botanical developed a great species especially Cape Gondwana affinities are apparent in this southern flora, while boreal influences of found in the mountainfloras from the Sa- a comparatively younger age are hara and Ethiopia in the north right down the length of the continent to the Africa. -
Large Hydro-Electricity and Hydro-Agricultural Schemes in Africa
FAO AQUASTAT Dams Africa – 070524 DAMS AND AGRICULTURE IN AFRICA Prepared by the AQUASTAT Programme May 2007 Water Development and Management Unit (NRLW) Land and Water Division (NRL) Food and Agriculture Organization of the United Nations (FAO) Dams According to ICOLD (International Commission on Large Dams), a large dam is a dam with the height of 15 m or more from the foundation. If dams are 5-15 metres high and have a reservoir volume of more than three million m3, they are also classified as large dams. Using this definition, there are more than 45 000 large dams around the world, almost half of them in China. Most of them were built in the 20th century to meet the constantly growing demand for water and electricity. Hydropower supplies 2.2% of the world’s energy and 19% of the world’s electricity needs and in 24 countries, including Brazil, Zambia and Norway, hydropower covers more than 90% of national electricity supply. Half of the world’s large dams were built exclusively or primarily for irrigation, and an estimated 30-40% of the 277 million hectares of irrigated lands worldwide rely on dams. As such, dams are estimated to contribute to 12-16% of world food production. Regional inventories include almost 1 300 large and medium-size dams in Africa, 40% of which are located in South Africa (517) (Figure 1). Most of these were constructed during the past 30 years, coinciding with rising demands for water from growing populations. Information on dam height is only available for about 600 dams and of these 550 dams have a height of more than 15 m. -
Bibliography [PDF]
Ancient TL Vol. 30 No.1 2012 31 Bibliography Compiled by Daniel Richter _____________________________________________________________________________________________ From 1st November 2011 to 31st May 2012 Abafoni, J. D., Mallam, S. P., and Akpa, T. C. (2012). Comparison of OSL and ITL measurements on quartz grains extracted from sediments of the Chad Basin, N.E. Nigeria. Research Journal of Applied Sciences 6, 483-486. Altay Atlıhan, M., Şahiner, E., and Soykal Alanyalı, F. (2012). Dose estimation and dating of pottery from Turkey. Radiation Physics and Chemistry 81, 594-598. Amos, C. B., Lapwood, J. J., Nobes, D. C., Burbank, D. W., Rieser, U., and Wade, A. (2011). Palaeoseismic constraints on Holocene surface ruptures along the Ostler Fault, southern New Zealand. New Zealand Journal of Geology and Geophysics 54, 367-378. Andreucci, S., Bateman, M. D., Zucca, C., Kapur, S., Aksit, İ., Dunajko, A., and Pascucci, V. (2012). Evidence of Saharan dust in upper Pleistocene reworked palaeosols of North-west Sardinia, Italy: palaeoenvironmental implications. Sedimentology 59, 917-938. Anjar, J., Adrielsson, L., Bennike, O., Björck, S., Filipsson, H. L., Groeneveld, J., Knudsen, K. L., Larsen, N. K., and Möller, P. (2012). Palaeoenvironments in the southern Baltic Sea Basin during Marine Isotope Stage 3: a multi- proxy reconstruction. Quaternary Science Reviews 34, 81-92. Athanassas, C., Bassiakos, Y., Wagner, G. A., and Timpson, M. E. (2012). Exploring paleogeographic conditions at two paleolithic sites in Navarino, southwest Greece, dated by optically stimulated luminescence. Geoarchaeology 27, 237-258. Atkinson, O. A. C., Thomas, D. S. G., Goudie, A. S., and Parker, A. G. (2012). Holocene development of multiple dune generations in the northeast Rub‘ al-Khali, United Arab Emirates. -
Animal Genetic Resources Information Bulletin
127 WHITE FULANI CATTLE OF WEST AND CENTRAL AFRICA C.L. Tawah' and J.E.O. Rege2 'Centre for Animal and Veterinary Research. P.O. Box 65, Ngaoundere, Adamawa Province, CAMEROON 2International Livestock Research Institute, P.O. Box 5689, Addis Ababa, ETHIOPIA SUMMARY The paper reviews information on the White Fulani cattle under the headings: origin, classification, distribution, population statistics, ecological settings, utility, husbandry practices, physical characteristics, special genetic characteristics, adaptive attributes and performance characteristics. It was concluded that the breed is economically important for several local communities in many West and Central African countries. The population of the breed is substantial. However, introgression from exotic cattle breeds as well as interbreeding with local breeds represent the major threat to the breed. The review identified a lack of programmes to develop the breed as being inimical to its long-term existence. RESUME L'article repasse l'information sur la race White Fulani du point de vue: origine, classement, distribution, statistique de population, contexte écologique, utilité, pratiques de conduites, caractéristiques physiques, caractéristiques génétiques spéciales, adaptabilité, et performances. On conclu que la race est importante du point de vue économique pour diverses communautés rurales dans la plupart des régions orientales et centrale de l'Afrique. Le nombre total de cette race est important; cependant, l'introduction de races exotiques, ainsi que le croisement avec des races locales représente le risque le plus important pour cette race. Cet article souligne également le fait que le manque de programmes de développement à long terme représente un risque important pour la conservation de cette race. -
Seasonal Provenance Changes of Present-Day Saharan Dust
Atmos. Chem. Phys. Discuss., doi:10.5194/acp-2017-131, 2017 Manuscript under review for journal Atmos. Chem. Phys. Discussion started: 16 February 2017 c Author(s) 2017. CC-BY 3.0 License. 1 Seasonal provenance changes of present-day Saharan dust 2 collected on- and offshore Mauritania 3 4 Carmen A. Friese1, Hans van Hateren2,*, Christoph Vogt1,3, Gerhard Fischer1, Jan-Berend W. 5 Stuut1,2 6 1Marum-Center of Marine Environmental Sciences, University of Bremen, Bremen, 28359, Germany 7 2NIOZ-Royal Netherlands Institute for Sea Research, Department of Ocean Systems, and Utrecht University, 1790 8 AB, Den Burg Texel, Netherlands 9 3ZEKAM, Crystallography, Geosciences, University of Bremen, 28359, Germany 10 *Now at: Vrije Universiteit Amsterdam, Faculty of Earth Sciences, 1081 HV Amsterdam, the Netherlands 11 Correspondence to: Carmen A. Friese ([email protected]) 12 Abstract. 13 Saharan dust has a crucial influence on the earth climate system and its emission, transport, and deposition are 14 intimately related to environmental parameters. The alteration in the physical and chemical properties of Saharan 15 dust due to changes in environmental parameters is often used to reconstruct the climate of the past. However, to 16 better interpret possible climate changes the dust source regions need to be known. By analysing the mineralogical 17 composition of transported or deposited dust, potential dust source areas can be inferred. Summer dust transport 18 offshore Northwest Africa occurs in the Saharan air layer (SAL). In contrast, dust transport in continental dust 19 source areas occurs predominantly with the trade winds. Hence, the source regions and related mineralogical 20 tracers differ with season and sampling location. -
Rising Food Insecurity Across Lake Chad Basin Humanitarian Bulletin
Humanitarian Bulletin West and Central Africa April 2016 In this issue Lake Chad food insecurity on the rise P.1 Sahel food insecurity remains high P.3 New displacements in Côte d’Ivoire P.5 HIGHLIGHTS Ebola resurfaces in Guinea and Liberia P.6 Three million people in the Regional update on epidemics P.7 Lake Chad region are facing Sahel funding update P.8 severe food shortages. In Nigeria’s Borno and Yobe states, 800,000 people need immediate assistance. Rising food insecurity across Lake Chad Basin Clashes between herders and farmers in Côte d’Ivoire Food insecurity in the Lake Chad region, already at crisis levels, is expected to further deepen as families exhaust their last reserves and the lean season progresses. displace over 6,000 people. Between January and April, Three million people are currently facing severe food shortages. The majority of the food insecure people are in Nigeria’s north-eastern Borno and Yobe states. DRC reports 5,757 cholera cases. Ebola resurfaces for the third time in Liberia, Guinea sees its first flare-up. KEY FIGURES People 2.4M displaced in Lake Chad Basin Severely food 2.9M insecure people in Lake Chad Basin People facing 6.7M crisis level of food insecurity in the Sahel SAHEL FUNDING US $1.9 billion requested in 2016 12% funded Humanitarian Bulletin | 2 In Borno, 1.6 million Immediate emergency assistance required people are in emergency According to a joint UN multi-sectoral assessment, carried out in April, in Borno alone, some 1.6 million people are facing severe food insecurity, with more than 550,000 in phase of food insecurity. -
Petro-Geochemistry, Genesis and Economic Aspect of Syenitic and Mafic Rocks in Mindif Complex, Far North Cameroon, Central Africa
International Journal of Geosciences, 2019, 10, 1081-1114 https://www.scirp.org/journal/ijg ISSN Online: 2156-8367 ISSN Print: 2156-8359 Petro-Geochemistry, Genesis and Economic Aspect of Syenitic and Mafic Rocks in Mindif Complex, Far North Cameroon, Central Africa Nguo Sylvestre Kanouo1*, Lianxun Wang2, Arnaud Patrice Kouske3, Syprien Bovari Yomeun2, Emmanuel Archelaus Afanga Basua2 1Mineral Exploration and Ore Genesis Unit, Department of Mining Engineering and Mineral Processing, Faculty of Mines and Petroleum Industries, University of Maroua, Maroua, Cameroon 2School of Earth Sciences, China University of Geosciences, Wuhan, China 3Department of Civil Engineering, The University Institute of Technology, University of Douala, Douala, Cameroon How to cite this paper: Kanouo, N.S., Abstract Wang, L., Kouske, A.P., Yomeun, S.B. and Basua, E.A.A. (2019) Petro-Geochemistry, Syenitic and mafic rocks in Mindif Complex (Far North of Cameroon) were Genesis and Economic Aspect of Syenitic surveyed and characterized to classify them, understand their formation his- and Mafic Rocks in Mindif Complex, Far tory, and assess their economic interest. Syenitic bodies (hololeucocratic North Cameroon, Central Africa. Interna- tional Journal of Geosciences, 10, 1081-1114. microsyenites; mesocratic aplitic quartz-syenite; leucocratic porphyritic https://doi.org/10.4236/ijg.2019.1012062 quartz-biotite syenite, and leucocratic porphyritic biotite-syenite) are sili- ca-oversaturated to silica-saturated, alkaline, and metaluminous. Hololeu- Received: June 16, 2019 cocratic microsyenites are structural oriented rocks, cooled in shallow Accepted: December 6, 2019 Published: December 9, 2019 depth from low trace and REE dry residual alkaline melts. Mesocratic ap- litic quartz-syenite also crystallized in shallow depth from a much Ba-rich Copyright © 2019 by author(s) and less dry residual melt.