Okavango River Basin Transboundary Diagnostic Analysis May 1998
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Okavango River Basin Groundwater Overview
Okavango River Basin Groundwater Overview Specialist Report prepared by Interconsult Namibia for : PERMANENT OKAVANGO RIVER BASIN COMMISSION Angola Botswana Namibia Ministério da Energia e Águas Ministry of Mineral Resources and Water Affairs Ministry of Agriculture, Water and Rural Development GABHIC Department of Water Affairs Department of Water Affairs Cx. P. 6695 Private Bag 0029 Private Bag 13193 LUANDA GABORONE WINDHOEK Tel: +244 2 393 681 Tel: +267 360 7100 Tel: +264 61 296 9111 Fax: +244 2 393 687 Fax: +267 303508 Fax: +264 61 232 861 PERMANENT OKAVANGO RIVER BASIN COMMISSION (OKACOM) OKAVANGO RIVER BASIN PREPARATORY ASSESSMENT: GROUNDWATER OVERVIEW Report prepared by: Interconsult Namibia (Pty) Ltd P. O. Box 20690 Windhoek With input from Wellfield Consulting Services, and E. Bereslawski March 1999 TABLE OF CONTENTS 1 INTRODUCTION ............................................................................................................... 1 1.1. BACKGROUND.............................................................................................................. 1 1.2. TERMS OF REFERENCE ................................................................................................ 1 2 OVERVIEW OF THE GEOHYDROLOGY OF THE BASIN .............................................. 2 2.1 BASIN GEOLOGY.............................................................................................................. 2 2.2 GEOHYDROLOGY OVERVIEW ........................................................................................... -
Country Profile Republic of Zambia Giraffe Conservation Status Report
Country Profile Republic of Zambia Giraffe Conservation Status Report Sub-region: Southern Africa General statistics Size of country: 752,614 km² Size of protected areas / percentage protected area coverage: 30% (Sub)species Thornicroft’s giraffe (Giraffa camelopardalis thornicrofti) Angolan giraffe (Giraffa camelopardalis angolensis) – possible South African giraffe (Giraffa camelopardalis giraffa) – possible Conservation Status IUCN Red List (IUCN 2012): Giraffa camelopardalis (as a species) – least concern G. c. thornicrofti – not assessed G. c. angolensis – not assessed G. c. giraffa – not assessed In the Republic of Zambia: The Zambia Wildlife Authority (ZAWA) is mandated under the Zambia Wildlife Act No. 12 of 1998 to manage and conserve Zambia’s wildlife and under this same act, the hunting of giraffe in Zambia is illegal (ZAWA 2015). Zambia has the second largest proportion of land under protected status in Southern Africa with approximately 225,000 km2 designated as protected areas. This equates to approximately 30% of the total land cover and of this, approximately 8% as National Parks (NPs) and 22% as Game Management Areas (GMA). The remaining protected land consists of bird sanctuaries, game ranches, forest and botanical reserves, and national heritage sites (Mwanza 2006). The Kavango Zambezi Transfrontier Conservation Area (KAZA TFCA), is potentially the world’s largest conservation area, spanning five southern African countries; Angola, Botswana, Namibia, Zambia and Zimbabwe, centred around the Caprivi-Chobe-Victoria Falls area (KAZA 2015). Parks within Zambia that fall under KAZA are: Liuwa Plain, Kafue, Mosi-oa-Tunya and Sioma Ngwezi (Peace Parks Foundation 2013). GCF is dedicated to securing a future for all giraffe populations and (sub)species in the wild. -
Ramsar Information Sheet
Ramsar Information Sheet Text copy-typed from the original document. 1. Date this sheet was completed: 20.11.1996 2. Country: Botswana 3. Name of wetland: The Okavango Delta System 4. Geographical co-ordinates: The Okavango Delta System lies between Longitudes 21 degrees 45 minutes East and 23 degrees 53 minutes East; and Latitudes 18 degrees 15 minutes South and 20 degrees 45 minutes South. It includes the Okavango River, commonly referred to as the Pan handle; the entire Okavango Delta; Lake Ngami; and parts of the Kwando and Linyanti River systems that fall west of the western boundary of the Chobe National Park. The entire area is as depicted on the attached map. 5. Altitude: Generally between 930 metres and 1000 metres above sea level. 6. Area: Approximately 68 640 km² (6 864 000 hectares) 7. Overview Three main features characterise the region, the Okavango, the Kwando and Linyanti river system connected to the Okavango Delta through the Selinda spillway and the intervening and surrounding dryland areas. These features are located within the Okavango rift, a geological structure subject to tectonis control and infilled with Kahalari Group sediments, principally sand, up to 300 metres thick. The Delta is the most important of the above named features. It is an inland delta in a semi arid region in which inflow fluctuations result in large fluctuations in flooded area (10,000 - 16,000 km²), which is comprised of permanent swamp, seasonal swamp and intermittently flooded areas. Similar flooding takes place in the Kwando/Linyanti river system. This leads to high seasonal concentrations of birdlife and wildlife, giving the area a very high tourism potential. -
Final Report: Southern Africa Regional Environmental Program
SOUTHERN AFRICA REGIONAL ENVIRONMENTAL PROGRAM FINAL REPORT DISCLAIMER The authors’ views expressed in this publication do not necessarily reflect the views of the United States Agency for International Development or the United States government. FINAL REPORT SOUTHERN AFRICA REGIONAL ENVIRONMENTAL PROGRAM Contract No. 674-C-00-10-00030-00 Cover illustration and all one-page illustrations: Credit: Fernando Hugo Fernandes DISCLAIMER The authors’ views expressed in this publication do not necessarily reflect the views of the United States Agency for International Development or the United States government. CONTENTS Acronyms ................................................................................................................ ii Executive Summary ............................................................................................... 1 Project Context ...................................................................................................... 4 Strategic Approach and Program Management .............................................. 10 Strategic Thrust of the Program ...............................................................................................10 Project Implementation and Key Partners .............................................................................12 Major Program Elements: SAREP Highlights and Achievements .................. 14 Summary of Key Technical Results and Achievements .......................................................14 Improving the Cooperative Management of the River -
Check-List of the Butterflies of the Kakamega Forest Nature Reserve in Western Kenya (Lepidoptera: Hesperioidea, Papilionoidea)
Nachr. entomol. Ver. Apollo, N. F. 25 (4): 161–174 (2004) 161 Check-list of the butterflies of the Kakamega Forest Nature Reserve in western Kenya (Lepidoptera: Hesperioidea, Papilionoidea) Lars Kühne, Steve C. Collins and Wanja Kinuthia1 Lars Kühne, Museum für Naturkunde der Humboldt-Universität zu Berlin, Invalidenstraße 43, D-10115 Berlin, Germany; email: [email protected] Steve C. Collins, African Butterfly Research Institute, P.O. Box 14308, Nairobi, Kenya Dr. Wanja Kinuthia, Department of Invertebrate Zoology, National Museums of Kenya, P.O. Box 40658, Nairobi, Kenya Abstract: All species of butterflies recorded from the Kaka- list it was clear that thorough investigation of scientific mega Forest N.R. in western Kenya are listed for the first collections can produce a very sound list of the occur- time. The check-list is based mainly on the collection of ring species in a relatively short time. The information A.B.R.I. (African Butterfly Research Institute, Nairobi). Furthermore records from the collection of the National density is frequently underestimated and collection data Museum of Kenya (Nairobi), the BIOTA-project and from offers a description of species diversity within a local literature were included in this list. In total 491 species or area, in particular with reference to rapid measurement 55 % of approximately 900 Kenyan species could be veri- of biodiversity (Trueman & Cranston 1997, Danks 1998, fied for the area. 31 species were not recorded before from Trojan 2000). Kenyan territory, 9 of them were described as new since the appearance of the book by Larsen (1996). The kind of list being produced here represents an information source for the total species diversity of the Checkliste der Tagfalter des Kakamega-Waldschutzge- Kakamega forest. -
See the Itinerary Here
A pioneering expedition to the Cuito River region in southeastern Angola. This expedition will be the first of its kind into Angola exploring the remote Cuito River system and will essentially open the way for tourism into one of Africa’s last wilderness frontiers. There is no better way to experience a true African Safari Expedition than in the comfort and privacy of your own exclusive mobile safari camp. An exploratory journey through the wilderness with the intimacy and flexibility of your own camp, guide, boats, helicopter and staff compliment. We will move our partner mobile rig (operated by Botswana based Beagle Expeditions) and staff, keeping our high standards of service the same. • 8 night Angolan Expedition • Fully inclusive • Minimum 4 / Maximum 4 persons • Private helicopter use of more than 30 hours • Possibility of collaring three elusive Angolan elephants • Led by specialist guide Simon Byron Day 1 Day 6 • Arrival at the Cuito Cuanavale airport • Fly on to the upper Cuito River base camp. • Morning Battle field tour of Cuito Cuanavale and Lomba batlle Field. • Helicopter flight to the Cuando River in the Bico area. • Afternoon boat cruise. • Exploration of the Luiana. (Luiana fly camp) Day 2 Day 7 • Full day helicopter exploration over the source lakes, with fly • Morning helicopter exploration of the Luiana and Cuando River system camp at Cuanavale Source Lake. and visit to Jamba, Jonas Savimbi’s UNITA base. Afternoon boat cruise Days 3 on the Cuito River • Morning helicopter exploration down the Cuanavale River Day 8 in search of elusive elephant. • Morning helicopter exploration of lower Cuito and vast wilderness area • Afternoon walk. -
The Herpetofauna of the Cubango, Cuito, and Lower Cuando River Catchments of South-Eastern Angola
Official journal website: Amphibian & Reptile Conservation amphibian-reptile-conservation.org 10(2) [Special Section]: 6–36 (e126). The herpetofauna of the Cubango, Cuito, and lower Cuando river catchments of south-eastern Angola 1,2,*Werner Conradie, 2Roger Bills, and 1,3William R. Branch 1Port Elizabeth Museum (Bayworld), P.O. Box 13147, Humewood 6013, SOUTH AFRICA 2South African Institute for Aquatic Bio- diversity, P/Bag 1015, Grahamstown 6140, SOUTH AFRICA 3Research Associate, Department of Zoology, P O Box 77000, Nelson Mandela Metropolitan University, Port Elizabeth 6031, SOUTH AFRICA Abstract.—Angola’s herpetofauna has been neglected for many years, but recent surveys have revealed unknown diversity and a consequent increase in the number of species recorded for the country. Most historical Angola surveys focused on the north-eastern and south-western parts of the country, with the south-east, now comprising the Kuando-Kubango Province, neglected. To address this gap a series of rapid biodiversity surveys of the upper Cubango-Okavango basin were conducted from 2012‒2015. This report presents the results of these surveys, together with a herpetological checklist of current and historical records for the Angolan drainage of the Cubango, Cuito, and Cuando Rivers. In summary 111 species are known from the region, comprising 38 snakes, 32 lizards, five chelonians, a single crocodile and 34 amphibians. The Cubango is the most western catchment and has the greatest herpetofaunal diversity (54 species). This is a reflection of both its easier access, and thus greatest number of historical records, and also the greater habitat and topographical diversity associated with the rocky headwaters. -
Spatiotemporal Patterns and Drivers of Surface Water Quality and Landscape Change in a Semi-Arid, Southern African Savanna
Spatiotemporal Patterns and Drivers of Surface Water Quality and Landscape Change in a Semi-Arid, Southern African Savanna John Tyler Fox Dissertation submitted to the faculty of the Virginia Polytechnic Institute and State University in partial fulfillment of the requirements for the degree of Doctor of Philosophy In Fisheries and Wildlife Kathleen A. Alexander Adil N. Godrej Emmanuel A. Frimpong Stephen P. Prisley May 16, 2016 Blacksburg, VA Keywords: (Escherichia coli, fecal indicator bacteria, water quality modeling, microbial fate, pollution, remote sensing, savanna disturbance ecology, land cover change, climate change, fire frequency, water-borne pathogens, wildlife, erosion, dryland rivers, water quality, Africa, ecosystem services) Copyright © 2016 J. Tyler Fox Spatiotemporal Patterns and Drivers of Surface Water Quality and Landscape Change in a Semi-Arid, Southern African Savanna John Tyler Fox Abstract The savannas of southern Africa are a highly variable and globally-important biome supporting rapidly-expanding human populations, along with one of the greatest concentrations of wildlife on the continent. Savannas occupy a fifth of the earth’s land surface, yet despite their ecological and economic significance, understanding of the complex couplings and feedbacks that drive spatiotemporal patterns of change are lacking. In Chapter 1 of my dissertation, I discuss some of the different theoretical frameworks used to understand complex and dynamic changes in savanna structure and composition. In Chapter 2, I evaluate spatial drivers of water quality declines in the Chobe River using spatiotemporal and geostatistical modeling of time series data collected along a transect spanning a mosaic of protected, urban, and developing urban land use. Chapter 3 explores the complex couplings and feedbacks that drive spatiotemporal patterns of land cover (LC) change across the Chobe District, with a particular focus on climate, fire, herbivory, and anthropogenic disturbance. -
L'exemple Du Bassin De Makgadikgadi-Okavango-Zambezi
Bassins de rift à des stades précoces de leur développement: l’exemple du bassin de Makgadikgadi-Okavango-Zambezi, Botswana et du bassin Sud-Tanganyika (Tanzanie et Zambie). Composition géochimique des sédiments: traçeurs des changements climatiques et tectoniques Philippa Huntsman-Mapila To cite this version: Philippa Huntsman-Mapila. Bassins de rift à des stades précoces de leur développement: l’exemple du bassin de Makgadikgadi-Okavango-Zambezi, Botswana et du bassin Sud-Tanganyika (Tanzanie et Zambie). Composition géochimique des sédiments: traçeurs des changements climatiques et tec- toniques. Géochimie. Université de Bretagne occidentale - Brest, 2006. Français. tel-00161196 HAL Id: tel-00161196 https://tel.archives-ouvertes.fr/tel-00161196 Submitted on 10 Jul 2007 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. 2 Remerciements Je tiens tout d’abord à remercier Jean-Jacques Tiercelin et Christophe Hémond, mes directeurs de thèse. Je leur suis très reconnaissante pour leurs conseils et leur sympathie. Je remercie beaucoup Mathieu Benoit et Jo Cotten pour la patience qu’ils ont montré lors de la mesure d’échantillons au cours de ma thèse et pour avoir accepté de travailler sur mes échantillons de sédiments. -
The Hydrology of the Okavango Delta, Botswana—Processes, Data and Modelling
Regional review: the hydrology of the Okavango Delta, Botswana—processes, data and modelling Christian Milzow & Lesego Kgotlhang & Peter Bauer-Gottwein & Philipp Meier & Wolfgang Kinzelbach Abstract The wetlands of the Okavango Delta accom- Introduction modate a multitude of ecosystems with a large diversity in fauna and flora. They not only provide the traditional The Okavango wetlands, commonly called the Okavango livelihood of the local communities but are also the basis Delta, are spread on top of an alluvial fan located in of a tourism industry that generates substantial revenue for northern Botswana, in the western branch of the East the whole of Botswana. For the global community, the African Rift Valley. Waters forming the Okavango River wetlands retain a tremendous pool of biodiversity. As the originate in the highlands of Angola, flow southwards, upstream states Angola and Namibia are developing, cross the Namibian Caprivi-Strip and eventually spread however, changes in the use of the water of the Okavango into the terminal wetlands on Botswanan territory cover- River and in the ecological status of the wetlands are to be ing the alluvial fan (Fig. 1). Whereas the climate in the expected. To predict these impacts, the hydrology of the headwater region is subtropical and humid with an annual Delta has to be understood. This article reviews scientific precipitation of up to 1,300 mm, it is semi-arid in Botswana work done for that purpose, focussing on the hydrological with precipitation amounting to only 450 mm/year in the modelling of surface water and groundwater. Research Delta area. High potential evapotranspiration rates cause providing input data to hydrological models is also over 95% of the wetland inflow and local precipitation to be presented. -
Altimetry, SAR and GRACE Applied for Modelling of an Ungauged Catchment
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Hydrol. Earth Syst. Sci. Discuss., 7, 9123–9154, 2010 Hydrology and www.hydrol-earth-syst-sci-discuss.net/7/9123/2010/ Earth System HESSD doi:10.5194/hessd-7-9123-2010 Sciences 7, 9123–9154, 2010 © Author(s) 2010. CC Attribution 3.0 License. Discussions Altimetry, SAR and This discussion paper is/has been under review for the journal Hydrology and Earth GRACE applied for System Sciences (HESS). Please refer to the corresponding final paper in HESS modelling of an if available. ungauged catchment Combining satellite radar altimetry, SAR C. Milzow et al. surface soil moisture and GRACE total Title Page storage changes for model calibration Abstract Introduction and validation in a large ungauged Conclusions References catchment Tables Figures 1 2 1 C. Milzow , P. E. Krogh , and P. Bauer-Gottwein J I 1 Department of Environmental Engineering, Technical University of Denmark, J I 2800 Kgs. Lyngby, Denmark 2National Space Institute, Technical University of Denmark, 2100 Copenhagen, Denmark Back Close Received: 12 November 2010 – Accepted: 20 November 2010 Full Screen / Esc – Published: 30 November 2010 Correspondence to: C. Milzow ([email protected]) Printer-friendly Version Published by Copernicus Publications on behalf of the European Geosciences Union. Interactive Discussion 9123 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract HESSD The availability of data is a major challenge for hydrological modelling in large -
The Okavango Delta and Its Place in the Geomorphological Evolution of Southern Africa.Pdf
1-54 McCarthy_105-108 van Dijk copy 2013/09/12 10:53 AM Page 1 1 30th Alex L. du Toit Memorial Lecture THE OKAVANGO DELTA AND ITS PLACE IN THE GEOMORPHOLOGICAL EVOLUTION OF SOUTHERN AFRICA T.S. McCARTHY Island vegetation shows a distinct zonation: the outer fringes are characterized by evergreen trees, followed inwards by deciduous trees, ivory palms, shrubs and grass and finally barren soil. The swamp surrounding the island is densely vegetated with sedges and grasses. SOUTH AFRICAN JOURNAL OF GEOLOGY, 2013, VOLUME 116.1 PAGE 1-54 doi:10.2113/gssajg.116.1.1 1-54 McCarthy_105-108 van Dijk copy 2013/09/12 10:53 AM Page 2 30th Alex L. du Toit Memorial Lecture Alex du Toit in the field with his first wife and only son in the early 1900s. Picture by kind courtesy M.C.J. de Wit, E.O. Köstlin and R.S. Liddle Photo: Gevers SOUTH AFRICAN JOURNAL OF GEOLOGY 1-54 McCarthy_105-108 van Dijk copy 2013/09/12 10:53 AM Page 3 T.S. McCARTHY 3 THE OKAVANGO DELTA AND ITS PLACE IN THE GEOMORPHOLOGICAL EVOLUTION OF SOUTHERN AFRICA T.S. McCARTHY School of Geosciences, University of the Witwatersrand, P.O.Box 3, WITS 2050, Johannesburg, South Africa e-mail: [email protected] © 2013 June Geological Society of South Africa ABSTRACT The Okavango Delta is southern Africa’s largest wetland ecosystem and probably the most pristine large wetland ecosystem in the world. Alex du Toit was the first to recognize the role of faulting in the origin of the Delta, proposing that the Delta lies within a graben structure related to the East African Rift Valley system.