3. Groundwater Needs Assessment – Okavango-Cubango River Basin

Total Page:16

File Type:pdf, Size:1020Kb

3. Groundwater Needs Assessment – Okavango-Cubango River Basin GROUNDWATER NEEDS ASSESSMENT OKAVANGO-CUBANGO RIVER BASIN BY Benjamin Mapani UNIVERSITY OF NAMIBIA AND WATERNET 1 February 2012 Acronyms DWA - Department of Water Affairs DWAF - Department of Water Affairs and Forestry TBA - Transboundary aquifer OBSC - Okavango Basin Steering Commission TDA - Technical Diagnosis Analysis SAP - Strategic Action Plans ITF - Institutional Task Force BTF - Biodiversity Task Force HTF - Hydrology Task Force 2 Table of Contents Acronyms .................................................................................................................................. 2 1. Introduction ...................................................................................................................... 4 2. Objectives .......................................................................................................................... 7 3. The basin and its water management ............................................................................... 8 3.1. Bio-physical conditions .............................................................................................. 8 3.2. Socio-economic conditions ...................................................................................... 12 3.3. Hydro-geological conditions .................................................................................... 15 3.3.1. Transboundary aquifers .................................................................................... 16 3.4. Water governance framework for OKACOM ........................................................... 18 3.4.1. Groundwater governance framework .............................................................. 20 4. Interviews ........................................................................................................................ 20 5. SWOT analysis ..................................................................... Error! Bookmark not defined. 5.1. Strengths .................................................................................................................. 24 5.2. Weaknesses ............................................................................................................. 24 5.3. Opportunities ........................................................................................................... 25 5.4. Threats ..................................................................................................................... 25 6. Conclusions ..................................................................................................................... 26 7. Recommendations .......................................................................................................... 27 8. References ....................................................................................................................... 29 AppendiX 1 Table of basic data for the L/R/ABO AppendiX 2 Transcripts of interviews 3 1. Introduction The Okavango River basin and delta comprises three riparian states of Angola, Botswana and Namibia. The basin consists of rivers that flow from the Angolan highlands into the Okavango delta in Botswana. The delta area was once part of a large lake called Makgadikgadi that dried up in the Holocene times and is now an essentially endoheic basin in common with other sections of the East African Rift (McCarthy and Metcalfe, 1990). The area is mostly inhabited by subsistence farming communities and large scale tourist operators, especially so in Botswana and Namibia. The actual Okavango River Basin area is quite eXtensive, including the Omatako basin in Namibia, which traditionally has not been treated as part of the Okavango basin for economic, social, and administrative reasons. The basin is jointly being managed by the Okavango- Cubango River Basin Commission (OKACOM), which was created when the three riparian states signed an agreement on its creation on 15th September 1994. The relative distribution of area for each riparian state is given in Table 1, below. Table 1 also shows the actual administrative district for each of the riparian states. Table 1. (Source: OKACOM 2010 Annual report, Maun, Botswana) 4 The area of concern for this needs assessment is shown in figure 1, below. Despite the presence of major river systems in this area, several communities live quite far from these water sources, and ground water is their main source of water. These settlements are shown on the map in figure 2a and 2b. This has to do with both cultural and later historical reasons, especially the last civil war in Angola, that necessitated large communities to move neXt to major highways and major settlements where there was security. Figure 1. The map of the Okavango-Cubango River Basin. The stippled area is the inactive part of the basin, which is not covered in this report. Rural water supply has been a major challenge in most African countries. It is estimated that the continent has close to 250 000 hand pumps, and half of them are non-operational (Harvey and Reed, 2006). This goes to show how programmes of rural water supply have become continuous action sectors. In the Okavango-Cubango river basin, this aspect of water supply has been attempted by Angola (1957-1961, Morais, 1997), and in Namibia (1994 up to present). In Namibia, some areas that are close to the “Golden Highway”, the B8 (Figure 2b, in blue) are supplied by tankers. This means of water supply is neither 5 permanent nor reliable, and is testimony to the need of groundwater supply via boreholes that can be community managed. The major industrial activities in the basin are found in the growing towns of Cuangar, Cuando, Kubango, Calai, and Menongue in Angola and Grootfontein and Rundu in Namibia, and Maun in Botswana. In the region between Rundu and Divundu (Figure 2b), the Government of Namibia has introduced irrigation schemes along the Okavango river, where commercial agriculture is currently being practiced. The Okavango River basin has about 600 000 inhabitants, living in an area of 260,379 km2, most of whom live in the rural areas. 54% of the population is in Angola, 36% in Namibia and 10% in Botswana. Figure 2a. The northern part of the Okavango-Cubango basin in Angola, showing major settlements and national parks and reserves. (Map source: Map Studio,2011). 6 Figure 2b. Map showing some of the major settlements and communications in the Botswana-Namibia and southern Angola part of the Okavango Basin (Map source: Map Studio, 2011). 2. Objectives The immediate objective of the needs assessment is to assess the present framework, eXperiences, and capacity for GW management in selected L/RBOs in the Okavango- Cubango River Basin and identify shortcomings for integrated groundwater management as part of integrated and transboundary water resources management (ITWRM). Furthermore, the objective is to develop targeted and prioritized recommendations for enhancing the capacity of L/RBOs for integrated GW management in the basins, based on consultations with the L/RBOs. 7 This work is part of the ongoing efforts by the riparian states and the international community to strengthen the L/RBOs as main actors in national and transboundary water resources management in Africa. The Specific objectives of the study are: (1) to understand how Groundwater water resources are managed in the basin, identify current initiatives that are being undertaken by the River Basin Commission on Groundwater, (2) To document current capacity in groundwater resources management and collaboration being undertaken by the Riparian states, (3) To produce a SWOT analysis for the basin. 3. The basin and its water management 3.1. Bio-physical conditions (a) Geographical, physical and hydrological context The Okavango delta river basin lies within three riparian states, Angola, Botswana and Namibia. The Okavango river has its source in southern Angola, near Huambo, and then flows in south-easterly direction until it reaches the town of Rundu on the Namibia-Angola border (Figure 2c). It then flows easterly for about 200 km, marking the border between Angola and Namibia. Then at Bagani (Divundu) it turns south-easterly again, crossing into Namibia for about 23 km then finally into Botswana where it ends into the inland delta known as the Okavango Delta. The delta has what is known as an active and inactive zones, these are shown in figure 2c below. The active zones of the delta are perennially filled with water, whereas the inactive parts only get flooded during the wet season. The Okavango river rises in Angola as the Cubango, then on the Namibia-Angola border it becomes the Okavango. The main tributaries of the Cubango-Okavango River are the Cutchi 8 and Culela in Angola; as the Okavango, the Cuito and the Omatako become the most important tributaries (Figures 2a and 2b). Other smaller ephemeral streams are the Ncamasere, Xaudum and the Eiseb. Relief As shown in figure 3 below, the relief of the Okavango basin varies greatly, from high relief in Angola (from near the source in Huambo to the Namibian border, near Rundu (circa 1000 km of river length)) and then flattens out in a meander river system from Rundu to near Maun in Botswana (660 km of river length). The implication is that most of the groundwater flow direction would be towards the Namibia border from Angola. Although this pattern is not eXactly followed, but it holds true for the high relief part of Angola (Bereslawski, 1997). Climate and implications for recharge The climate in the Okavango basin is tropical and the
Recommended publications
  • 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.
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • 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
    [Show full text]
  • Estimating Rainfall and Water Balance Over the Okavango River Baprovidedsin Byfor South Easthydrological Academic Libraries System (SEALS) Applications
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE Estimating rainfall and water balance over the Okavango River Baprovidedsin byfor South Easthydrological Academic Libraries System (SEALS) applications Julie Wilk, Dominic Kniveton, Lotta Andersson, Russell Layberry, Martin C. Todd, Denis Hughes, Susan Ringrose and Cornelis Vanderpost Department of Water and Environmental Studies, Linköping University, S-581 83 Linköping, Sweden Department of Physics Chemistry and Environmental Science, University of Sussex, Falmer, Brighton, UK Swedish Meteorological and Hydrological Institute, 601 76 Norrköping, Sweden University College of London, 26 Bedford Way, WC1H 0AP, London, UK Institute of Water Research, Rhodes University, Grahamstown, South Africa Harry Oppenheimer Okavango Research Centre, Private Bag 285, Maun, Botswana Abstract A historical database for use in rainfall-runoff modeling of the Okavango River Basin in Southwest Africa is presented. The work has relevance for similar data-sparse regions. The parameters of main concern are rainfall and catchment water balance, which are key variables for subsequent studies of the hydrological impacts of development and climate change. Rainfall estimates are based on a combination of in situ gauges and satellite sources. Rain gauge measurements are most extensive from 1955 to 1972, after which they are drastically reduced due to the Angolan civil war. The sensitivity of the rainfall fields to spatial interpolation techniques and the density of gauges were evaluated. Satellite based rainfall estimates for the basin are developed for the period from 1991 onwards, based on the Tropical Rainfall Measuring Mission (TRMM) and Special Sensor Microwave Imager (SSM/I) datasets. The consistency between the gauges and satellite estimates was considered.
    [Show full text]
  • The Okavango; a River Supporting Its People, Environment and Economic Development
    The Okavango; a river supporting its people, environment and economic development Article (Accepted Version) Kgathi, D L, Kniveton, D, Ringrose, S, Turton, A R, Vanderpost, C H M, Lundqvist, J and Seely, M (2006) The Okavango; a river supporting its people, environment and economic development. Journal of Hydrology, 331 (1-2). pp. 3-17. ISSN 0022-1694 This version is available from Sussex Research Online: http://sro.sussex.ac.uk/id/eprint/1690/ This document is made available in accordance with publisher policies and may differ from the published version or from the version of record. If you wish to cite this item you are advised to consult the publisher’s version. Please see the URL above for details on accessing the published version. Copyright and reuse: Sussex Research Online is a digital repository of the research output of the University. Copyright and all moral rights to the version of the paper presented here belong to the individual author(s) and/or other copyright owners. To the extent reasonable and practicable, the material made available in SRO has been checked for eligibility before being made available. Copies of full text items generally can be reproduced, displayed or performed and given to third parties in any format or medium for personal research or study, educational, or not-for-profit purposes without prior permission or charge, provided that the authors, title and full bibliographic details are credited, a hyperlink and/or URL is given for the original metadata page and the content is not changed in any way. http://sro.sussex.ac.uk Special Issue Journal of Hydrology The Hydrology of the Okavango Basin and Delta in a development perspective Guest editors: Dominic Kniveton, and Martin Todd Paper 1.
    [Show full text]
  • Overview of the Cubango Okavango
    Transboundary Cooperation for Protecting the Cubango- Okavango River Basin and Improving the Integrity of the Okavango Delta World Heritage Property Overview of the Cubango-Okavango River Basin in Angola: Challenges and Perspectives Maun, 3-4 June 2019 Botswana National Development Plan (2018-2022) The National Development Plan 6 Axis provides framework for the development of infrastructure, 25 Policies environmental sustainability and land and territorial planning. 83 Programs Cubango-Okavango River Basin Key Challenges To develop better conditions for the economic development of the region. To foster sustainable development considering technical, socio- economic and environmental aspects. To combat poverty and increase the opportunities of equitable socioeconomic benefits. Key Considerations 1. Inventory of the water needs and uses. 2. Assessment of the water balance between needs and availability. 3. Water quality. 4. Risk management and valorization of the water resources. Some of the Main Needs Water Institutional Monitoring Capacity Network Decision- Participatory making Management Supporting Systems Adequate Funding Master Plans for Cubango Zambezi and Basins Cubango/ Approved in 6 main Up to 2030 Okavango 2016 programs Final Draft 9 main Zambezi Up to 2035 2018 programs Cubango/Okavango Basin Master Plan Main Programs Rehabilitation of degraded areas. Maintaining the natural connectivity between rivers and river corridors. Implementing water monitoring network. Managing the fishery activity and water use. Biodiversity conservation. Capacity building and governance. Zambezi Basin Master Plan Main Programs Water supply for communities and economic activities. Sewage and water pollution control. Economic and social valorisation of water resources. Protection of ecosystems. Risk management. Economic sustainability of the water resources. Institutional and legal framework.
    [Show full text]
  • Okavango River Basin Transboundary Diagnostic Analysis May 1998
    Table of Contents SECTION A 1. INTRODUCTION 2. AVAILABILITY OF INFORMATION AND DATA 3. STAKEHOLDER CONSULTATION AND PARTICIPATION 3.1 Introduction/General 3.2 Namibia and Botswana 3.2.1 The Stakeholders 3.2.2 Work carried Out 3.2.3 Feedback 3.3 Angola 3.2.1 General 4. DESCRIPTION AND HISTORY OF THE AREA 4.1 History 4.2 Geology, Soils, Topography, Geomorphology and Vegetation 4.2.1 Introduction 4.2.2 Data Available 4.2.2.1 General 4.2.2.2 Catchment Topography Topographic Maps and aerial photography Satellite Imagery 4.2.2.3 Catchment Geomorphology Soils (Data available 4.2.2.4 Vegetation 4.2.3 Overview/Analysis 4.2.3.1 Catchment Topography 4.2.3.2 Catchment Geomorphology Soils Geological Setting 4.2.3.3 Catchment Vegetation 4.3 Climate 4.3.1 Introduction 4.3.2 Data available 4.3.2.1 Rainfall 4.3.2.2 Temperature 4.3.2.3 Other Climatic paramaters 4.3.3 Overview 4.3.3.1 General 4.3.3.2 Precipitation 4.3.3.3 Temperature 4.2.3.4 Evaporation 4.4 Human Links with the Basin 4.4.1 Introduction 4.4.2 Data Available 1 4.4.3 Previous Studies and Research 4.4.4 Overview 5. HYDROLOGY, HYDRAULICS AND GEOHYDROLOGY OF THE OKAVANGO RIVER 5.1 Introduction 5.2 River Morphology 5.2.1 Data Available 5.2.2 Overview/Analysis 5.3 Water levels and Runoff 5.3.1 Introduction 5.3.2 Data Availability 5.3.2.1 Gauging Network 5.3.2.2 Completeness and Quality of Data 5.3.3 Overview/Analysis 5.3.3.1 General 5.3.3.2 Cubango River and Tributaries (take down through Angola and include Rundu) 5.3.3.3 Cuito River and Tributaries 5.3.3.4 Okavango River 5.3.3.5 Inflow: Okavango at Mohembo 5.3.3.6 Outflow Rivers 5.3.3.7 Conclusions 5.4 Erosion, Sediment Loads and Sedimentation 5.5 Groundwater 6.
    [Show full text]
  • Estimating Rainfall and Water Balance Over the Okavango River Basin for Hydrological Applications
    Estimating rainfall and water balance over the Okavango River Basin for hydrological applications Article (Accepted Version) Wilk, Julie, Kniveton, Dominic, Andersson, Lotta, Layberry, Russell, Todd, Martin C, Hughes, Denis, Ringrose, Susan and Vanderpost, Cornelis (2006) Estimating rainfall and water balance over the Okavango River Basin for hydrological applications. Journal of Hydrology, 331 (1-2). pp. 18-29. ISSN 0022-1694 This version is available from Sussex Research Online: http://sro.sussex.ac.uk/id/eprint/1696/ This document is made available in accordance with publisher policies and may differ from the published version or from the version of record. If you wish to cite this item you are advised to consult the publisher’s version. Please see the URL above for details on accessing the published version. Copyright and reuse: Sussex Research Online is a digital repository of the research output of the University. Copyright and all moral rights to the version of the paper presented here belong to the individual author(s) and/or other copyright owners. To the extent reasonable and practicable, the material made available in SRO has been checked for eligibility before being made available. Copies of full text items generally can be reproduced, displayed or performed and given to third parties in any format or medium for personal research or study, educational, or not-for-profit purposes without prior permission or charge, provided that the authors, title and full bibliographic details are credited, a hyperlink and/or URL is given for the original metadata page and the content is not changed in any way. http://sro.sussex.ac.uk Estimating rainfall and water balance over the Okavango River Basin for hydrological applications Julie Wilk*a, Dominic Kniveton b Lotta Andersson c, Russell Layberry b, Martin C.
    [Show full text]
  • 1 Southern Africa Regional Flood Update
    Southern Africa Regional Flood Update 20 January 2011 Highlights • In Mozambique, a number of river basins have registered alert levels, and water levels are increasing; • River levels in the upper Zambezi and the Okavango rivers are very high for this early in the rainfall season; • Two spillway gates of Lake Kariba will be opened on 22 January 2011, which could in time lead to flooding downstream; • In South Africa, 40 people have died and 6,000 displaced due to flooding. A National State of Disaster will be declared in 28 municipalities in 7 provinces. • A map of the region is found on Page 7 in this Bulletin Rainfall forecast According to the regional rainfall forecast, all countries in contiguous southern Africa are expected to receive normal to above-normal rainfall between January and March 2011, specifically the regions of northern Zimbabwe, central Zambia, southern Malawi, central Mozambique and most of Madagascar, which are expected to receive above-normal rainfall. In the case of Mozambique and Madagascar, this rainfall could come in the form of tropical cyclones, which affect these countries every season. Likely scenarios Flooding along the major rivers of the region is an annual occurrence, and regularly affected communities, who depend on the floodplains for food production, usually move to higher ground well in advance of the floodwaters. Meteorological and hydrological authorities are monitoring the situation and regular warnings are being issued. It should be noted that exchange of information between countries that share major rivers have improved significantly. All countries have contingency plans prepared with scenarios of what could happen and interventions needed.
    [Show full text]
  • A Seasonal Survey of the Fish of the Kavango River Floodplain Along The
    A Decade of Namibian Fisheries Science Payne, A. I. L., Pillar, S. C. and R. J. M. Crawford (Eds). S. Afr. J. mar. Sci. 23: 449–464 2001 449 FISH RESPONSE TO THE ANNUAL FLOODING REGIME IN THE KAVANGO RIVER ALONG THE ANGOLA/NAMIBIA BORDER C. H. HOCUTT* and P. N. JOHNSON† The results of the first seasonal survey of the fish of the Kavango River floodplain along the Angola/Namibia border are reported. The river experiences peak flooding from February through June, with the 375-km long flood- plain extending up to 5 km across. The floodplain was sampled five times in 1992 by seine, fish traps and rotenone. The data indicated a pronounced structural and functional response of the fish community in relation to the alternating flood and drought conditions in the river. Catch per unit effort and diversity were highest during months of peak flooding (May and June), and lowest during the month of least flow (November). The reproductive strategies of K-selected piscivorous cichlids and tigerfish were in advance of flooding. Many r-selected invertivores, especially cyprinids, were in relative synchrony with flooding and the stimulation of littoral zone plant growth, while other invertivores lagged the cyprinids. Herbivores had lowest relative abundance during peak flooding; this seemingly inverse relationship with the invertivores should not be interpreted as replacement, but rather the swamping of the system with young-of-the-year r-selected invertivores. The data support the Flood Pulse Concept, which hypothesizes that flooding is the major “driver” of productivity in lowland or floodplain rivers. Key words: behaviour, floodplain fishery, migration, Okavango Delta, r-/K-selection, subsistence fishery A seasonal survey of the fish of the Kavango River long-term shifts in the structural and functional com- floodplain along the Angola/Namibia border was ponents of the fish community.
    [Show full text]
  • The Okavango River Basin in Southern Africa: a Case Study of Transboundary Resource Management Issues
    University of Colorado Law School Colorado Law Scholarly Commons Allocating and Managing Water for a Sustainable Future: Lessons from Around the 2002 World (Summer Conference, June 11-14) 6-14-2002 The Okavango River Basin in Southern Africa: A Case Study of Transboundary Resource Management Issues Robert K. Hitchcock Follow this and additional works at: https://scholar.law.colorado.edu/allocating-and-managing-water-for- sustainable-future Part of the Environmental Policy Commons, Natural Resources and Conservation Commons, Natural Resources Management and Policy Commons, Sustainability Commons, Transnational Law Commons, Water Law Commons, and the Water Resource Management Commons Citation Information Hitchcock, Robert K., "The Okavango River Basin in Southern Africa: A Case Study of Transboundary Resource Management Issues" (2002). Allocating and Managing Water for a Sustainable Future: Lessons from Around the World (Summer Conference, June 11-14). https://scholar.law.colorado.edu/allocating-and-managing-water-for-sustainable-future/71 Reproduced with permission of the Getches-Wilkinson Center for Natural Resources, Energy, and the Environment (formerly the Natural Resources Law Center) at the University of Colorado Law School. Robert K. Hitchcock, The Okavango River Basin in Southern Africa: A Case Study of Transboundary Resource Management Issues, in ALLOCATING AND MANAGING WATER FOR A SUSTAINABLE FUTURE: LESSONS FROM AROUND THE WORLD (Natural Res. Law Ctr., Univ. of Colo. Sch. of Law 2002). Reproduced with permission of the Getches-Wilkinson Center for Natural Resources, Energy, and the Environment (formerly the Natural Resources Law Center) at the University of Colorado Law School. The Okavango River Basin in Southern Africa: A Case Study of Transboundary Resource Management Issues Robert K.
    [Show full text]