Energy in Africa Challenges and Opportunities
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Durham Research Online
Durham Research Online Deposited in DRO: 13 April 2015 Version of attached le: Published Version Peer-review status of attached le: Peer-reviewed Citation for published item: Kaislaniemi, L. and van Hunen, J. (2014) 'Dynamics of lithospheric thinning and mantle melting by edge-driven convection : application to Moroccan Atlas mountains.', Geochemistry, geophysics, geosystems., 15 (8). pp. 3175-3189. Further information on publisher's website: http://dx.doi.org/10.1002/2014GC005414 Publisher's copyright statement: c 2014. The Authors. This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modications or adaptations are made. Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. Durham University Library, Stockton Road, Durham DH1 3LY, United Kingdom Tel : +44 (0)191 334 3042 | Fax : +44 (0)191 334 2971 https://dro.dur.ac.uk PUBLICATIONS Geochemistry, -
Morocco): Clues from Trace Elements and Sr–Nd–Pb–Hf Isotopes
Lithos 205 (2014) 247–265 Contents lists available at ScienceDirect Lithos journal homepage: www.elsevier.com/locate/lithos Lithospheric origin for Neogene–Quaternary Middle Atlas lavas (Morocco): Clues from trace elements and Sr–Nd–Pb–Hf isotopes Delphine Bosch a,⁎, René C. Maury b,M'hammedElAzzouzib,c,ClaireBollingerd, Hervé Bellon b, Patrick Verdoux e a UMR-UM2-CNRS 5243 Géosciences Montpellier, Université de Montpellier II, place E. Bataillon, c.c. 060, 34095 Montpellier, France b UMR-CNRS 6538 Domaines océaniques, Institut Universitaire Européen de la Mer (IUEM), IUEM, Université de Brest, Université Européenne de Bretagne, place Nicolas Copernic, 29280 Plouzané, France c Faculté des Sciences, Université Mohammed-V, av. Ibn Batouta, BP 1014, 10100 Rabat, Maroc d UMS-CNRS 3113 Pôle de spectrométrie océan, IUEM, Université de Brest, Université Européenne de Bretagne, place Nicolas Copernic, 29280 Plouzané, France e Laboratoire de Géochimie Isotopique environnementale, Université de Nîmes/Site GIS, UMR-CNRS 7330, rue Georges Besse, 30035 Nîmes Cedex 1, France article info abstract Article history: This study presents new geochemical data on 26 mafic lavas from the Middle Atlas and Central Morocco volcanic Received 17 April 2014 provinces, including Miocene nephelinites and Pliocene–Quaternary (3.9–0.6 Ma) nephelinites, basanites, alkali Accepted 11 July 2014 and subalkaline basalts. Most of them represent near-primary magmas, although some alkali basalts were derived Available online 21 July 2014 from the minor fractionation of olivine and diopside phenocrysts. These evolved samples and the subalkaline basalt display higher 207Pb/204Pb and Zr/Nb ratios and lower εNd consistent with their contamination by lower crustal Keywords: Intraplate alkali basalts granulites during an open fractionation process. -
The Renewable Energy Transition in Africa Powering Access, Resilience and Prosperity
The Renewable Energy Transition in Africa Powering Access, Resilience and Prosperity On behalf of the Disclaimer This publication and the material herein are provided “as is”. All reasonable precautions have been taken by the Authors to verify the reliability of the material in this publication. However, neither the Authors nor any of its officials, agents, data or other third- party content providers provides a warranty of any kind, either expressed or implied, and they accept no responsibility or liability for any consequence of use of the publication or material herein. The information contained herein does not necessarily represent the views of all countries analysed in the report. The mention of specific companies or certain projects or products does not imply that they are endorsed or recommended by the Authors in preference to others of a similar nature that are not mentioned. The designations employed, and the presentation of material herein, do not imply the expression of any opinion on the part of the Authors concerning the legal status of any region, country, territory, city or area or of its authorities, or concerning the delimitation of frontiers or boundaries. Foreword Energy is the key to development in Africa and the founda- drawn up a roadmap to achieve inclusive and sustainable tion for industrialisation. Like in Europe and other parts of the growth and development. One of the important topics covered world, the expansion of renewables goes beyond the provision is access to affordable, reliable and sustainable energy for all of reliable energy and climate protection. Economic develop- – SDG 7 of the 2030 Agenda. -
HFO Power Plant in Mali, Africa
Udenrigsudvalget 2018-19 URU Alm.del - endeligt svar på spørgsmål 103 Offentligt HFO power plant in Mali, Africa SUMMARY Trucost, part of S&P Global was commissioned to conduct analysis of the potential CO2e savings relating to a heavy fuel oil (HFO) power plant installation in Mali (Africa). This African HFO project can feasibly provide GHG savings based on detailed analysis and materiality of carbon savings. These are considered low with an associated net benefit of 15 tCO2e/DKK million invested. With social cost of carbon incorporated, this is equivalent to 0.012 DKK/DKK invested. DATA AVAILABLE The maximum working capacity of the new HFO power plant in Kayes, Mali is 81 MWe (IFU, 2016b) The actual working capacity is 81% of maximum capacity for the HFO power plant in Mali (IFU, 2016b) The guaranteed output for Mali power plant is 578,160 MWh/annum (IFU, 2016b) and based on this it was calculated that the plant operates for 24 hours/day Kayes, Mali HFO plant is a greenfield project, thus construction emissions are included The project life considered for the analysis is 20 years Ecoinvent factors were used for calculating the lifetime emissions of both alternative and baseline scenario (EcoInvent, 2016) RATIONALE OF FUNDING In Mali as well as generally in Africa, there is an increasing demand for electricity, which needs to be met. The annual demand for energy is increasing at the rate of 10% per annum in Mali (African Development Bank, 2015). IFU is considering an investment developing a HFO power plant to help meet this need. -
Seismic Velocity Structure of the Continental Lithosphere from Controlled Source Data
Seismic Velocity Structure of the Continental Lithosphere from Controlled Source Data Walter D. Mooney US Geological Survey, Menlo Park, CA, USA Claus Prodehl University of Karlsruhe, Karlsruhe, Germany Nina I. Pavlenkova RAS Institute of the Physics of the Earth, Moscow, Russia 1. Introduction Year Authors Areas covered J/A/B a The purpose of this chapter is to provide a summary of the seismic velocity structure of the continental lithosphere, 1971 Heacock N-America B 1973 Meissner World J i.e., the crust and uppermost mantle. We define the crust as 1973 Mueller World B the outer layer of the Earth that is separated from the under- 1975 Makris E-Africa, Iceland A lying mantle by the Mohorovi6i6 discontinuity (Moho). We 1977 Bamford and Prodehl Europe, N-America J adopted the usual convention of defining the seismic Moho 1977 Heacock Europe, N-America B as the level in the Earth where the seismic compressional- 1977 Mueller Europe, N-America A 1977 Prodehl Europe, N-America A wave (P-wave) velocity increases rapidly or gradually to 1978 Mueller World A a value greater than or equal to 7.6 km sec -1 (Steinhart, 1967), 1980 Zverev and Kosminskaya Europe, Asia B defined in the data by the so-called "Pn" phase (P-normal). 1982 Soller et al. World J Here we use the term uppermost mantle to refer to the 50- 1984 Prodehl World A 200+ km thick lithospheric mantle that forms the root of the 1986 Meissner Continents B 1987 Orcutt Oceans J continents and that is attached to the crust (i.e., moves with the 1989 Mooney and Braile N-America A continental plates). -
Berber Languages and Linguistics Mena B
Berber Languages and Linguistics Mena B. Lafkioui LAST MODIFIED: 24 MAY 2018 DOI: 10.1093/OBO/9780199772810-0219 Introduction Berber (aka Tamazight) is a branch of the Afro-Asiatic language phylum and counts about forty languages, which entirely cover North Africa, stretching from Morocco to Egypt, as well as from the Mediterranean Sea to the Sahara and the northern and western Sahel, including Mali, Niger, and Burkina Faso. The number of Berber speakers is estimated at more than forty million, of which the majority lives in Morocco (about 70 percent speaks Berber, mainly along with other languages). Berber has a general “continuum” makeup, which means that one Berber language gradually merges into another Berber language when they are contiguous. As a result, Berber forms a tightly knit and coherent bloc, which makes its subclassification very tricky. On the typological level, three major subdivisions can be made. The first is Northern Berber, which mainly contains Tarifit (including Senhaja Berber; North, Northeast, and Northwest Morocco), Tamazight of the Middle Atlas (Central Morocco), Figuig Berber (East Morocco), Kabyle Berber (North Algeria), Tashawit (Aures, Northeast Algeria), and some oasis languages like Berber of Mzab (South Algeria) and of Ouargla (South Algeria). The second is Southern Berber, which comprises languages such as Zenaga (Mauritania), Tashelhit (South Morocco), and Tetserret and Tuareg Berber (Sahara, Sahel). The third is Eastern Berber, which includes languages such as Berber spoken in Siwa (West Egypt), Sokna and El-Fogaha (Fezzan, Central Libya), Yefren and Zuara (Tripolitania, North Libya), and Ghadames (East Libya), as well as all the Berber languages of Tunisia (e.g., Jerba, Tamazret, and Sened). -
Best Practices on Renewable Energy in Africa
BEST PRACTISES ON RENEWABLE ENERGY IN AFRICA THE CURRENT STATUS Tracking SDG7: The Energy Progress Report 2018 Renewable energy in Africa: The current status 2014–16. Among the strongest performers were Bangladesh, Kenya, Ethiopia, and Tanzania, which expanded access by more than 5 percentage points annually between 2014 and 2016. Electricity and energy are key issues today targets and the SDG7 goal: to “ensure ac- 90 GW 2. Already, concentrated solar po- on the African continent: about two-thirds cess to affordable, reliable, sustainable wer, photovoltaics and wind turbines are • Socioeconomic1.of its electrificationpopulation does not havepatterns: any ac- Access and modern to electricity energy for all” isuntil strongly 2030. associateddeployed across with the poverty,continent. with access cess to electricity services. The situation rates four timesin Sub-Saharan higher Africa in theis especially top quintile con- Solutions of household to the energy expenditure access issue in comparedMany programmes to theand initiatives bottom are quintileim- across the 20cerning countries and rural with areas the are particularlylargest access Africa deficit.lie in the transition Differences to renewable in electricity plemented access to promote by thegender use of renew- of head of household wereaffected. also Today, found half of to all beenergy material use in energy.in a minority Its potential of on thethe continenttop 20 isaccess-deficit able energy, such countries.as Electric Africa, the Af- Africa includes traditional biomass con- considerable. Several resources are re- rican–EU Renewable Energy Cooperation sumption, which has the dual disadvan- levant in different areas, wind for exam- Programme (RECP) and AREI (African Re- • Methodologiestage of to being estimate dangerous electrification: for human health pleWithin has a bettercountries quality differentin Northern andmethodologies newable Energy can Initiative). -
Enhancing China–Africa Cooperation in the Renewable Energy Sector
Issue 176 March 2021 Enhancing China–Africa Cooperation in the Renewable Energy Sector Access to affordable and sustainable electricity is of fundamental importance to development in much of Africa. But, while access to electricity is improving, contributions from non-hydropower renewable China–Africa energy sources remain small. At the same time, China – the powerhouse of cooperation solar energy technologies – has made limited contribution to harnessing on renewable Africa’s renewable energy. Combining insights from recent webinars and research, this Policy Briefing discusses how China–Africa energy could cooperation on renewable energy could lead to improvements lead to in access to and supply of affordable and sustainable energy in improvements Africa. Recommendations for African and Chinese policymakers and in access to businesses include the adoption of transparent, competitive, and locally inclusive energy procurement and use mechanisms. and supply of affordable and Key messages sustainable – Access to electricity in Africa has improved over the past five years but, partly due to the Covid-19 pandemic, investment is declining. energy. – Challenges to the deployment of renewable energy in Africa could be overcome through effective cooperation with China, a global leader in renewables. – This would bring mutual benefits. Africa presents untapped market potential due to its rich endowment in renewable energy sources. Improved access to affordable and sustainable electricity and technology transfer would benefit citizens across Africa. – It would also contribute towards meeting global and national commitments on climate change and access to electricity in the SDGs. – But, for local communities to benefit, a more transparent and Seife Ayele, inclusive governance framework must be established. -
Treating Animals Protecting Livelihoods
SPANA Annual Review 2008 Treating Animals Protecting Livelihoods The SPANA Annual Review is an opportunity for me to praise our amazing supporters who remain the core resource for the work which SPANA does. But it also allows me to recognise the efforts of SPANA’s staff in ensuring that in these very challenging times we can continue to deliver SPANA Chairman Derek Knottenbelt OBE true value for money. In many of our countries, animal feed and fuel Our supporters have continued to provide resources prices doubled in 2008. It is inevitable that in those – no doubt themselves making personal sacrifices circumstances the poorest will suffer most and the to allow that. That’s why SPANA is special and quite animals will suffer with their communities. different from many other charities of its type. We are a family which rallies round when times get bad. I can None of us can be unaware of the world’s financial assure SPANA supporters that economies are being crisis. In SPANA’s countries the effects of the made but they are being made sensibly and with a economic downturn are magnified enormously long-term strategy. Chairman’s Introduction by the singular lack of help for the poorest people. Inevitably it is they who suffer the most in hard times. I appeal to every SPANA supporter to continue to But SPANA’s philosophy of providing appropriate help as far as you can; if it’s tough for us it’s a whole veterinary and educational help has been the lot tougher for an Ethiopian gharry pony or a Malian cornerstone of its work since 1923. -
Emergency Plan of Action (Epoa) Morocco/Mena Zone: Cold Wave
P a g e | 1 Emergency Plan of Action (EPoA) Morocco/Mena zone: Cold wave DREF Operation n° MDRMA009 Glide n° For DREF; Date of issue: 24 /01/2018 Expected timeframe: 3 months, Expected end date: 24/04/2018 Category allocated to the of the disaster or crisis: Yellow DREF allocated: CHF 249530 Total number of people affected: 70,0000 Number of people to be assisted: 17,500 (3,500 families). Host National Society: Moroccan Red Crescent society (MRCS) : 100 volunteers , 10 staff , 7 branches: Red Cross Red Crescent Movement partners actively involved in the operation: None- Other partner organizations actively involved in the operation: Association Mohammed V, Local governance, Royal Army, Ministry of transport, Ministry of health A. Situation analysis Description of the disaster At the start of 2018, temperatures are below seasonal norms in various parts of the world. In Morocco, starting from 5 January, temperatures are generally below normal. Heavy snowfall has affected the High Atlas and the Middle Atlas, from 900 meters above sea level, with temperatures as low as minus 5 ° C, where the average tempratures in January (the coldest of the 3 winter months) hovers around 18 degrees Celsius. This average includes a low of 7 degrees and a high of 23 degrees. In the interior of the country, several roads have been cut due to snow, according to the Ministry of Transport. With its terrain mountains accustomed to very harsh winters, this area is the most affected by the cold wave that has raged between 5 and 9 January, 20181. The cold also affects, to a lesser extent, the Atlantic coast. -
A History of Human Impact on Moroccan Mountain Landscapes
Afr Archaeol Rev (2015) 32:233–248 DOI 10.1007/s10437-015-9186-7 ORIGINAL ARTICLE A History of Human Impact on Moroccan Mountain Landscapes Rachid Cheddadi1 & Majda Nourelbait2 & Ouafaa Bouaissa1 & Jalal Tabel1 & Ali Rhoujjati3 & José Antonio López-Sáez4 & Francisca Alba-Sánchez5 & Carla Khater6 & Aziz Ballouche7 & Laurent Dezileau8 & Henry Lamb9 Published online: 9 June 2015 # Springer Science+Business Media New York 2015 Abstract The present study aims to review palaeoecological evidence for environ- mental changes induced by human activities over the last few millennia in the montane landscapes of Morocco. The study is based on well-dated pollen and geochemical records from the Rif and the Middle Atlas mountains, to show spatial and temporal variation in the onset and intensity of exploitation of forest, soil and mineral resources. Before ca. 2000 BP, anthropogenic impact was minimal. At about that time, abrupt * Rachid Cheddadi [email protected] 1 Institut des Sciences de l’Évolution, UMR UM2-CNRS-IRD 5554, University of Montpellier 2, place Eugène-Bataillon, 34095 Montpellier Cedex 05, France 2 Laboratoire Géosciences Marines et Sciences des Sols, Unité associée au CNRST (URAC 45), Département de Géologie, Université Chouaib Doukkali, 24000 El Jadida, Morocco 3 Faculté des Sciences et Techniques, Département de Géologie, Labo. Géo-Ressources (URAC 42), Bd A. Khattabi, BP 549, 40000 Guéliz, Marrakech, Morocco 4 G.I. Arqueobiología, Instituto de Historia, CCHS, CSIC, Albasanz 26-28, 28037 Madrid, Spain 5 Departamento de Botánica, -
The Future of Africa Energy Supply
IASS STUDY Institute for Advanced Sustainability Studies (IASS) Potsdam, March 2016 The Future of Africa’s Energy Supply Potentials and Development Options for Renewable Energy Rainer Quitzow, Sybille Roehrkasten, David Jacobs, Benjamin Bayer, El Mostafa Jamea, Yvonne Waweru, Patrick Matschoss This study was conducted with financial support from the German Ministry for Economic Cooperation and Development (BMZ). The content of the study is the sole responsibility of the authors. Table of Contents Table of Contents Table of Contents List of Tables 4 List of Figures 4 List of Boxes 4 Acknowledgements 5 List of Abbreviations 6 Executive Summary 9 1. Objectives and Structure of the Report 13 2. Status Quo of Renewable Energy in Africa 15 2.1. Key issues and challenges in Africa’s energy development 15 2.2. The African energy mix: status quo and major trends 16 2.2.1 Overview of primary energy demand in Africa 16 2.2.2 Electricity generation 16 2.2.3 Residential and transport sectors 18 2.3. Current status of renewables in African electricity sector 19 2.3.1 Renewable energy policies 19 2.3.2 Electricity generation from renewables 19 2.3.3 Trends in installed renewable energy capacity 21 2.3.4 Trends in renewable energy investments 21 IASS Study_1 Table of Contents 3. Potentials for Growth and Development 25 3.1. Scenarios, potentials and targets 25 3.1.1 Scenarios for 2020 25 3.1.2 Key country-level targets and technical potential of renewable energy technologies 26 3.2. Drivers and opportunities for renewable energy deployment in Africa 28 3.2.1 Benefiting from declining renewable energy costs 28 3.2.2 Benefiting from rapid deployment and stable costs 28 3.2.3 Renewable energy as a cost-effective option for rural electrification 29 3.2.4 Benefiting from increased energy security 29 3.2.5 Benefiting from innovations and local value creation 29 3.2.6 Benefiting from low-carbon, climate-resilient development 30 3.2.7 Resource endowments and country-specific opportunity structures for renewable energy expansion 30 3.3.