Floods and Droughts in the Zambezi River Basin What Can Be Done?
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
GUIDE to CIVIL SOCIETY in NAMIBIA 3Rd Edition
GUIDE TO CIVIL SOCIETY IN NAMIBIA GUIDE TO 3Rd Edition 3Rd Compiled by Rejoice PJ Marowa and Naita Hishoono and Naita Marowa PJ Rejoice Compiled by GUIDE TO CIVIL SOCIETY IN NAMIBIA 3rd Edition AN OVERVIEW OF THE MANDATE AND ACTIVITIES OF CIVIL SOCIETY ORGANISATIONS IN NAMIBIA Compiled by Rejoice PJ Marowa and Naita Hishoono GUIDE TO CIVIL SOCIETY IN NAMIBIA COMPILED BY: Rejoice PJ Marowa and Naita Hishoono PUBLISHED BY: Namibia Institute for Democracy FUNDED BY: Hanns Seidel Foundation Namibia COPYRIGHT: 2018 Namibia Institute for Democracy. No part of this publication may be reproduced in any form or by any means electronical or mechanical including photocopying, recording, or by any information storage and retrieval system, without the permission of the publisher. DESIGN AND LAYOUT: K22 Communications/Afterschool PRINTED BY : John Meinert Printing ISBN: 978-99916-865-5-4 PHYSICAL ADDRESS House of Democracy 70-72 Dr. Frans Indongo Street Windhoek West P.O. Box 11956, Klein Windhoek Windhoek, Namibia EMAIL: [email protected] WEBSITE: www.nid.org.na You may forward the completed questionnaire at the end of this guide to NID or contact NID for inclusion in possible future editions of this guide Foreword A vibrant civil society is the cornerstone of educated, safe, clean, involved and spiritually each community and of our Democracy. uplifted. Namibia’s constitution gives us, the citizens and inhabitants, the freedom and mandate CSOs spearheaded Namibia’s Independence to get involved in our governing process. process. As watchdogs we hold our elected The 3rd Edition of the Guide to Civil Society representatives accountable. -
Go Wild – Boxed2go Track Namibia’S Awesome Wildlife
Go Wild – Boxed2Go Track Namibia’s awesome wildlife. 12 Day Namibian Self-Drive Safari. Experience the wild side of Namibia on this twelve-day trip through the northern regions of the country. Join the Gondwana Collection and Namibia2Go for a special Namibian journey. This carefully planned safari includes stopovers at all the popular wildlife sites. Beginning in Windhoek, the route leads northwards to the famous Etosha National Park, where two nights are enjoyed at the unique and quirky Etosha Safari Camp. The third day is spent travelling into the heart of Etosha for superb wildlife viewing, exiting in the late afternoon at the northern gate. Overnight at the stylish Etosha King Nehale on the Andoni Plains before travelling further north to the peaceful oasis of Hakusembe Lodge on the glittering Okavango River. Arrive in time to raise your glass and watch the sun sink into the horizon from the deck of the lodge. As you journey eastwards into the Zambezi Region and toward the Kwando River, a wilder Africa calls. A sanctuary for wildlife, Bwabwata National Park and surrounds provide countless photographic opportunities. Tune in to the sounds of the river and fall asleep to the chortling of hippos at Namushasha River Lodge. A highlight of a stay is a trip into Bwabwata, by boat and game-viewing vehicle. The safari continues further east on the floodplains of the Chobe River, adjacent to Chobe National Park, where it’s possible to spot elephant, buffalo and water-adapted antelope like sitatunga at different times of the year. After savouring the delights of Chobe, you enter into the enchanted world of the mighty Zambezi River, where the life-affirming calls of fish eagles resound through the day. -
Angolan Giraffe (Giraffa Camelopardalis Ssp
Angolan Giraffe (Giraffa camelopardalis ssp. angolensis) Appendix 1: Historical and recent geographic range and population of Angolan Giraffe G. c. angolensis Geographic Range ANGOLA Historical range in Angola Giraffe formerly occurred in the mopane and acacia savannas of southern Angola (East 1999). According to Crawford-Cabral and Verissimo (2005), the historic distribution of the species presented a discontinuous range with two, reputedly separated, populations. The western-most population extended from the upper course of the Curoca River through Otchinjau to the banks of the Kunene (synonymous Cunene) River, and through Cuamato and the Mupa area further north (Crawford-Cabral and Verissimo 2005, Dagg 1962). The intention of protecting this western population of G. c. angolensis, led to the proclamation of Mupa National Park (Crawford-Cabral and Verissimo 2005, P. Vaz Pinto pers. comm.). The eastern population occurred between the Cuito and Cuando Rivers, with larger numbers of records from the southeast corner of the former Mucusso Game Reserve (Crawford-Cabral and Verissimo 2005, Dagg 1962). By the late 1990s Giraffe were assumed to be extinct in Angola (East 1999). According to Kuedikuenda and Xavier (2009), a small population of Angolan Giraffe may still occur in Mupa National Park; however, no census data exist to substantiate this claim. As the Park was ravaged by poachers and refugees, it was generally accepted that Giraffe were locally extinct until recent re-introductions into southern Angola from Namibia (Kissama Foundation 2015, East 1999, P. Vaz Pinto pers. comm.). BOTSWANA Current range in Botswana Recent genetic analyses have revealed that the population of Giraffe in the Central Kalahari and Khutse Game Reserves in central Botswana is from the subspecies G. -
Mozambique Zambia South Africa Zimbabwe Tanzania
UNITED NATIONS MOZAMBIQUE Geospatial 30°E 35°E 40°E L a k UNITED REPUBLIC OF 10°S e 10°S Chinsali M a l a w TANZANIA Palma i Mocimboa da Praia R ovuma Mueda ^! Lua Mecula pu la ZAMBIA L a Quissanga k e NIASSA N Metangula y CABO DELGADO a Chiconono DEM. REP. OF s a Ancuabe Pemba THE CONGO Lichinga Montepuez Marrupa Chipata MALAWI Maúa Lilongwe Namuno Namapa a ^! gw n Mandimba Memba a io u Vila úr L L Mecubúri Nacala Kabwe Gamito Cuamba Vila Ribáué MecontaMonapo Mossuril Fingoè FurancungoCoutinho ^! Nampula 15°S Vila ^! 15°S Lago de NAMPULA TETE Junqueiro ^! Lusaka ZumboCahora Bassa Murrupula Mogincual K Nametil o afu ezi Namarrói Erego e b Mágoè Tete GiléL am i Z Moatize Milange g Angoche Lugela o Z n l a h m a bez e i ZAMBEZIA Vila n azoe Changara da Moma n M a Lake Chemba Morrumbala Maganja Bindura Guro h Kariba Pebane C Namacurra e Chinhoyi Harare Vila Quelimane u ^! Fontes iq Marondera Mopeia Marromeu b am Inhaminga Velha oz P M úngu Chinde Be ni n è SOFALA t of ManicaChimoio o o o o o o o o o o o o o o o gh ZIMBABWE o Bi Mutare Sussundenga Dondo Gweru Masvingo Beira I NDI A N Bulawayo Chibabava 20°S 20°S Espungabera Nova OCE A N Mambone Gwanda MANICA e Sav Inhassôro Vilanculos Chicualacuala Mabote Mapai INHAMBANE Lim Massinga p o p GAZA o Morrumbene Homoíne Massingir Panda ^! National capital SOUTH Inhambane Administrative capital Polokwane Guijá Inharrime Town, village o Chibuto Major airport Magude MaciaManjacazeQuissico International boundary AFRICA Administrative boundary MAPUTO Xai-Xai 25°S Nelspruit Main road 25°S Moamba Manhiça Railway Pretoria MatolaMaputo ^! ^! 0 100 200km Mbabane^!Namaacha Boane 0 50 100mi !\ Bela Johannesburg Lobamba Vista ESWATINI Map No. -
Water Scenarios for the Zambezi River Basin, 2000 - 2050
Water Scenarios for the Zambezi River Basin, 2000 - 2050 Lucas Beck ∗ Thomas Bernauer ∗∗ June 1, 2010 Abstract Consumptive water use in the Zambezi river basin (ZRB), one of the largest fresh- water catchments in Africa and worldwide, is currently around 15-20% of total runoff. This suggests many development possibilities, particularly for irrigated agriculture and hydropower production. Development plans of the riparian countries indicate that con- sumptive water use might increase up to 40% of total runoff already by 2025. We have constructed a rainfall–runoff model for the ZRB that is calibrated on the best available runoff data for the basin. We then feed a wide range of water demand drivers as well as climate change predictions into the model and assess their implications for runoff at key points in the water catchment. The results show that, in the absence of effective international cooperation on water allocation issues, population and economic growth, expansion of irrigated agriculture, and water transfers, combined with climatic changes are likely to have very important transboundary impacts. In particular, such impacts involve drastically reduced runoff in the dry season and changing shares of ZRB coun- tries in runoff and water demand. These results imply that allocation rules should be set up within the next few years before serious international conflicts over sharing the Zambezi’s waters arise. Keywords: Water demand scenarios, Zambezi River Basin, water institutions ∗[email protected] and [email protected], ETH Zurich, Center for Comparative and Interna- tional Studies and Center for Environmental Decisions, Weinbergstrasse 11, 8092 Zurich, Switzerland, Phone: +41 44 632 6466 ∗∗We are very grateful to Tobias Siegfried, Wolfgang Kinzelbach, and Amaury Tilmant for highly useful comments on previous versions of this paper. -
Ecological Changes in the Zambezi River Basin This Book Is a Product of the CODESRIA Comparative Research Network
Ecological Changes in the Zambezi River Basin This book is a product of the CODESRIA Comparative Research Network. Ecological Changes in the Zambezi River Basin Edited by Mzime Ndebele-Murisa Ismael Aaron Kimirei Chipo Plaxedes Mubaya Taurai Bere Council for the Development of Social Science Research in Africa DAKAR © CODESRIA 2020 Council for the Development of Social Science Research in Africa Avenue Cheikh Anta Diop, Angle Canal IV BP 3304 Dakar, 18524, Senegal Website: www.codesria.org ISBN: 978-2-86978-713-1 All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopy, recording or any information storage or retrieval system without prior permission from CODESRIA. Typesetting: CODESRIA Graphics and Cover Design: Masumbuko Semba Distributed in Africa by CODESRIA Distributed elsewhere by African Books Collective, Oxford, UK Website: www.africanbookscollective.com The Council for the Development of Social Science Research in Africa (CODESRIA) is an independent organisation whose principal objectives are to facilitate research, promote research-based publishing and create multiple forums for critical thinking and exchange of views among African researchers. All these are aimed at reducing the fragmentation of research in the continent through the creation of thematic research networks that cut across linguistic and regional boundaries. CODESRIA publishes Africa Development, the longest standing Africa based social science journal; Afrika Zamani, a journal of history; the African Sociological Review; Africa Review of Books and the Journal of Higher Education in Africa. The Council also co- publishes Identity, Culture and Politics: An Afro-Asian Dialogue; and the Afro-Arab Selections for Social Sciences. -
Letter of Concern: Mining in the Lower Zambezi River Water Catchment and Protected Areas
Letter of Concern: Mining in the Lower Zambezi River Water Catchment and Protected Areas INTRODUCTION This petition is submitted to express the growing concern by the traditional residents of the Lower Zambezi Valley, the international conservation community, and local leaseholders in regard to the numerous proposed mining projects currently under development in the area. These projects are likely to impact the area’s irreplaceable eco-system and cause irreversible damage to one of the greatest natural heritage areas in Zambia, and all of Africa. The mining projects are located both within and adjacent to the Lower Zambezi National Park, the recently formed Partnership Park (the first of its kind in Zambia which is a partnership between community and GMA leaseholders), and Mana Pools National Park, a World Heritage Site located directly across the river in neighboring Zimbabwe. The area currently supports many communities in which thousands of local people depend on sustainable industries including agriculture, fisheries and tourism. As per the signatories document attached, you will see many of the communities are represented here. All of these communities and sustainable enterprises are under threat by the potential consequences of the proposed mining, which does not provide long-term economic benefits to Zambian citizens. As a unique and world-renowned ecosystem with immense financial and ecological value to Zambia, this area deserves the highest level of protection. We are very concerned about the profound and long- lasting negative socio-economic and environmental impacts that are likely to occur if the proposed mining operations go forward. The proposed open pit mining projects are located inside the Zambezi River water catchment, in close proximity to tributaries to this invaluable water resource. -
The Zambezi River Basin: Water Resources Management
Department of Physical Geography The Zambezi River Basin: water resources management Energy-Food-Water nexus approach Gabriel Sainz Sanchez Master’s thesis NKA 216 Physical Geography and Quaternary Geology, 45 Credits 2018 Preface This Master’s thesis is Gabriel Sainz Sanchez’s degree project in Physical Geography and Quaternary Geology at the Department of Physical Geography, Stockholm University. The Master’s thesis comprises 45 credits (one and a half term of full-time studies). Supervisors have been Arvid Bring at the Department of Physical Geography, Stockholm University and Louise Croneborg-Jones, The World Bank. Examiner has been Steffen Holzkämper at the Department of Physical Geography, Stockholm University. The author is responsible for the contents of this thesis. Stockholm, 8 June 2018 Lars-Ove Westerberg Vice Director of studies Abstract The energy-food-water nexus is of fundamental significance in the goal towards sustainable development. The Zambezi River Basin, situated in southern Africa, currently offers vast water resources for social and economic development for the eight riparian countries that constitute the watershed. Hydropower generation and agriculture are the main water users in the watershed with great potential of expansion, plus urban water supply materialise the largest consumers of this resource. Climate and social changes are pressuring natural resources availability which might show severe alterations due to enhances in the variability of precipitation patterns. This study thus examines the present water resources in the transboundary basin and executes low and high case future climate change incited scenarios in order to estimate the possible availability of water for the period 2060-2099 by performing water balances. -
The Pungwe, Buzi, and Save (Pubusa)
The Pungwe, Buzi and Save (Pubusa) and Central Zambezi Basins Portfolio Jefter Sakupwanya, Mbali Malekane; June 2014 General Overview of the Basins The current reality in the Basins is one of increasing populations despite the impacts of the HIV/AIDS endemic 1.6 million people in the Pungwe Basin 1.3 million people in the Buzi Basin 3.2 million people in the Save Basin 20 million people in Central Zambezi Poverty is a persistent problem in the Basins with more than half the rural population living below the poverty datum line 60% lack access to safe and reliable drinking water 75% lack access to proper sanitation General Overview of the Basins The water resources are unevenly distributed across the Basins, both spatially and temporally There is generally a lack of coincidence between water resources endowment and human settlement Floods and drought are a major challenge Situation exacerbated by the impact of climate change Water quality problems from improper land use practices CRIDF Interventions Responding to the needs of poor Communities and key Partners Need to protect the resource base Strengthening Institutional Capacity of key Partners through TA support Strengthening Stakeholder structures to enhance mutual trust and confidence Consolidating cooperation in Transboundary Water Resources Management CRIDF Interventions: Project Selection Transparency – stakeholders must have confidence in how projects are selected Fairness and inclusivity – every attempt is made to ensure that all stakeholders are treated fairly and processes around -
Southern Africa • Floods Regional Update # 5 20 April 2010
Southern Africa • Floods Regional Update # 5 20 April 2010 This report was issued by the Regional Office for Southern and Eastern Africa (ROSEA). It covers the period from 09 to 20 April 2010. The next report will be issued within the next two weeks. I. HIGHLIGHTS/KEY PRIORITIES • An assessment mission to the Angolan Province of Cunene found that 23,620 people have been affected by floods; • In Madagascar, access to affected communities remains an issue. II. Regional Situation Overview As the rainy season draws to a close, countries downstream of the Zambezi River - Malawi, Mozambique, Zambia and Zimbabwe – are not experiencing any new incidences of flooding. However, continuing high water levels in the upper Zambezi, Cunene, Cuvelai and Kavango Rivers are still being recorded, affecting Angola and northern Namibia. Furthermore, as the high water levels in the upper Zambezi River move downstream, localized flooding remains a possibility. In the next two weeks, no significant rainfall is expected over the currently flood-affected areas or their surrounding basins. III. Angola A joint assessment mission by Government and the United Nations Country Team (UNCT) was conducted in the flood-affected Cunene Province from 06 to 09 April 2010. The mission found that 23,620 people (3,300 households) have been affected by floods in the province. Of that total, 12,449 people (1,706 households) have been left homeless but have been able to stay with neighbors and family, whilst the remaining 11,171 people (1,549 households) have been relocated to Government-managed camps within the province. There are also reports of damage to schools and infrastructure. -
Mozambique Case Study Example1
Mozambique Case study example1 - Principle 1: The Zambezi River Basin - "dialogue for building a common vision" The Zambezi River Basin encompasses some 1.300 km2 throughout the Southern African Development Community (SADC) region, including a dense network of tributaries and associated wetland systems in eight countries (Angola, Namibia, Botswana, Zimbabwe, Zambia, Malawi, Tanzania, Mozambique). The livelihoods of approximately 26 million people are directly dependent on this basin, deriving benefits from its water, hydro-electric power, irrigation developments, fisheries and great wealth of related natural resources, including grazing areas, wildlife, and tourism. Over the past forty years, however, the communities and ecosystems of the lower Zambezi have been constraint by the management of large upstream dams. The toll is particularly high on Mozambique, as it the last country on the journey of the Zambezi; Mozambicans have to live with the consequences of upriver management. By eliminating natural flooding and greatly increasing dry season flows in the lower Zambezi, Kariba Dam (completed in 1959) and especially Cahora Bassa Dam (completed in 1974) cause great hardship for hundreds of thousands of Mozambican villagers whose livelihoods depend on the ebb and flow of the Zambezi River. Although these hydropower dams generate important revenues and support development however, at the expense of other resource users. Subsistence fishing, farming, and livestock grazing activities have collapsed with the loss of the annual flood. The productivity of the prawn fishery has declined by $10 - 20 million per year -- this in a country that ranks as one of the world’s poorest nations (per capita income in 2000 was USD230). -
Dynamic Evolution of the Zambezi-Limpopo Watershed, Central Zimbabwe
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Online Research @ Cardiff Moore, Blenkinsop and Cotterill Zim watershed_20120408_AEM DYNAMIC EVOLUTION OF THE ZAMBEZI-LIMPOPO WATERSHED, CENTRAL ZIMBABWE Andy Moore1,2, Tom Blenkinsop3 and Fenton (Woody) Cotterill4 1African Queen Mines Ltd., Box 66 Maun, Botswana. 2Dept of Geology, Rhodes University, Grahamstown 6140, South Africa. Email: [email protected] 3School of Earth and Environmental Sciences, James Cook University, Townsville, QLD4811, Australia. Email: [email protected] 4AEON – African Earth Observatory Network, Geoecodynamics Research Hub, University of Stellenbosch, Private Bag X1, Matieland 7602, South Africa. Email: [email protected] ABSTRACT Prospecting carried out to the south of the Zambezi-Limpopo drainage divide in the vicinity of Bulawayo, Zimbabwe, led to the recovery of a suite of ilmenites with a chemical “fingerprint” that can be closely matched with the population found in the early Palaeozoic Colossus kimberlite, which is located to the north of the modern watershed. The ilmenite geochemistry eliminates other Zimbabwe Kimberlites as potential sources of these pathfinder minerals. Geophysical modelling has been used to ascribe the elevation of southern Africa to dynamic topography sustained by a mantle plume; however, the evolution of the modern divide between the Zambezi and Limpopo drainage basins is not readily explained in terms of this model. Rather, it can be interpreted to represent a late Palaeogene continental flexure, which formed in response to crustal shortening, linked to intra-plate transmission of stresses associated with an episode of spreading reorganization at the ocean ridges surrounding southern Africa.