Relevant bibliographies by topics / Rivers – Namibia

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Rivers – Namibia'

Author: Grafiati
Published: 4 June 2021
Last updated: 8 February 2022

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Journal articles on the topic "Rivers – Namibia"

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Paillou, Philippe, Sylvia Lopez, Eugene Marais, and Klaus Scipal. "Mapping Paleohydrology of the Ephemeral Kuiseb River, Namibia, from Radar Remote Sensing." Water 12, no. 5 (2020): 1441. http://dx.doi.org/10.3390/w12051441.

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The Kuiseb River is one of the major ephemeral rivers of Western Namibia, setting the northern limit of the Namib Sand Sea and outflowing in the Atlantic Ocean at Walvis Bay. Such ephemeral rivers are of the highest importance for the country since they are related both to recent past climatic conditions and to potential water resources. Using high-resolution radar images from the Japanese ALOS-2 satellite, we mapped for the first time the numerous channels hidden under the surface aeolian sediments: while the non-permanent tributaries of the Kuiseb River appear north of its present-day bed, a
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Miller, R. McG, C. Krapf, T. Hoey, et al. "A sedimentological record of fluvial-aeolian interactions and climate variability in the hyperarid northern Namib Desert, Namibia." South African Journal of Geology 124, no. 3 (2021): 575–610. http://dx.doi.org/10.25131/sajg.124.0008.

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Abstract The aeolian regime of the 100 km wide, hyperarid Namib Desert has been sporadically punctuated by the deposition of fluvial sediments generated during periods of higher humidity either further inland or well within the desert from Late Oligocene to Late Holocene. Four new Late Cenozoic formations are described from the northern Skeleton Coast and compared with formations further south: the Klein Nadas, Nadas (gravels, sands), Vulture’s Nest (silts) and Uniab Boulder Formations. The Klein Nadas Formation is a trimodal mass-flow fan consisting of thousands of huge, remobilised, end-Carb
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Setti, M., A. Lόpez-Galindo, M. Padoan, and E. Garzanti. "Clay mineralogy in southern Africa river muds." Clay Minerals 49, no. 5 (2014): 717–33. http://dx.doi.org/10.1180/claymin.2014.049.5.08.

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AbstractThe composition, morphology and crystal order of clay minerals in silt-sized sediments carried in suspensions from 25 major rivers across tropical southern Africa have been studied by X-ray diffractometry and scanning and transmission electron microscopy. Our goal was to determine the spatial variability of clay-mineral associations in diverse geological settings, and in climatic conditions ranging from humid Angola and Zambia to hyperarid Namibia and the Kalahari. Specific attention was paid to the micromorphology and chemical composition of smectite particles. The relative abundance
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Botes, A., J. Henderson, T. Nakale, K. Nantanga, K. Schachtschneider, and M. Seely. "Ephemeral rivers and their development: testing an approach to basin management committees on the Kuiseb River, Namibia." Physics and Chemistry of the Earth, Parts A/B/C 28, no. 20-27 (2003): 853–58. http://dx.doi.org/10.1016/j.pce.2003.08.028.

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Ringrose, Susan, Wilma Matheson, Mary Seely, Lin Cassidy, Stephan Coetzee, and Thebe Kemosidile. "Aspects of floodplain deposition in semi-arid ephemeral rivers, examples from the Kuiseb river valley, central Namibia." Transactions of the Royal Society of South Africa 69, no. 3 (2014): 187–93. http://dx.doi.org/10.1080/0035919x.2014.953623.

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Douglas, Caitlin M. S., Mark Mulligan, Xavier A. Harrison, Joh R. Henschel, Nathalie Pettorelli, and Guy Cowlishaw. "Widespread dieback of riparian trees on a dammed ephemeral river and evidence of local mitigation by tributary flows." PeerJ 4 (October 27, 2016): e2622. http://dx.doi.org/10.7717/peerj.2622.

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Ephemeral rivers act as linear oases in drylands providing key resources to people and wildlife. However, not much is known about these rivers’ sensitivities to human activities. We investigated the landscape-level determinants of riparian tree dieback along the Swakop River, a dammed ephemeral river in Namibia, focusing on the native ana tree (Faidherbia albida) and the invasive mesquite (Prosopisspp.). We surveyed over 1,900 individual trees distributed across 24 sites along a 250 km stretch of the river. General linear mixed models were used to test five hypotheses relating to three anthrop
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Moser-Nørgaard, P. M., and M. Denich. "Influence of livestock on the regeneration of fodder trees along ephemeral rivers of Namibia." Journal of Arid Environments 75, no. 4 (2011): 371–76. http://dx.doi.org/10.1016/j.jaridenv.2010.11.009.

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Meissner, Richard, and Jeroen Warner. "Indigenous paradiplomacy and the Orokawe hydroelectric dam on the Kunene River." Regions and Cohesion 11, no. 1 (2021): 21–48. http://dx.doi.org/10.3167/reco.2021.110103.

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English Abstract: What role can non-diplomats play in managing and altering power relations in transboundary river basins? We answer this by investigating the lobbying efforts of indigenous peoples to stop the construction of the planned Orokawe (Baynes) dam on the Kunene River. The Kunene River forms part of the border between Angola and Namibia with several concluded treaties in place. These treaties set the context of bilateral state diplomacy concerning the allocation and management of a transboundary water resource. The theoretical foundation of our investigation are ideational power conc
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Zimmermann, M. "Water resources management in central northern Namibia using empirically grounded modelling." Journal of Water, Sanitation and Hygiene for Development 2, no. 2 (2012): 112–23. http://dx.doi.org/10.2166/washdev.2012.090.

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In this paper, a new methodology for the analysis and assessment of water supply regimes is presented. The problems of water supply management in developing countries are multidimensional and interdependent. Conventional methods, which only deal with separated and isolated issues, are not appropriate to deal with these problems. The method presented here, however, can comprehend the whole system. Therefore, using this method, conclusions for the management of adapted institutional and technological transformations can be drawn. In this study, relevant system variables of a problem context are
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Dollar, Evan S. J. "Palaeofluvial geomorphology in southern Africa: a review." Progress in Physical Geography: Earth and Environment 22, no. 3 (1998): 325–49. http://dx.doi.org/10.1177/030913339802200302.

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This article presents an overview of palaeofluvial geomorphology research in southern Africa. For the purposes of this article this includes South Africa, Zimbabwe, Namibia, Lesotho, Swaziland and Botswana. Although interest in fluvial systems has a long history in southern Africa, the scientific study of rivers was initiated by the discovery of the first alluvial diamond along the banks of the Orange River in 1867. Since then, significant progress has been made in unravelling the fluvial history of southern Africa from the early Archaean Ventersdorp Contact Reef River to modern channel proces
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Dissertations / Theses on the topic "Rivers – Namibia"

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Sarma, Diganta. "Assessment of sustainable groundwater utilization with case studies from semi-arid Namibia." University of the Western Cape, 2016. http://hdl.handle.net/11394/5649.

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Philosophiae Doctor - PhD<br>The thesis addresses sustainability of groundwater utilization in arid and semiarid regions of Namibia. Recharge in this hydrogeological setting occurs as discrete events to aquifers that are bounded in extent. Case studies involving fractured hardrock and alluvial aquifers with aquifer-ephemeral river interaction were considered. The nature of recharge to arid region bounded aquifers was explored. In arid region aquifers, roundwater storage is depleted during extended dry periods due to pumping and natural discharge. Steady state conditions are rarely achieved. W
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De, Almeida Louise. "The effect of sewage effluent from De Beers marine diamond mining operations on the expression of cytochrome P450 (CYP1A) and vitellogenin (vtg)." Thesis, Rhodes University, 2013. http://hdl.handle.net/10962/d1009440.

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Sewage effluents disposed into the marine environment from De Beers Marine Namibia diamond mining vessels have the potential to cause endocrine disruptive effects in marine organisms. Endocrine disruption refers to the alteration of the normal functioning of the endocrine system and various chemicals have the ability to mimic hormones, effecting endogenous hormone synthesis, transport, receptor interaction and intracellular signaling. The potential endocrine disruptive effects, caused by the release of different types of sewage effluents into the ocean, on fish species is a concern due to the
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Krapf, Carmen. "Ephemeral river systems at the Skeleton Coast, NW-Namibia sedimentological and geomorphological studies on the braided river dominated Koigab Fan, the cenozoic succession in the Uniabmond area and comparative studies on fluvio-aeolian interaction between ephemeral rivers and the Skeleton Coast erg /." Doctoral thesis, [S.l. : s.n.], 2003. http://deposit.ddb.de/cgi-bin/dokserv?idn=968609740.

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Matengu, Brian Munihango. "Groundwater assessment and sustainable management of the coastal alluvial aquifers in Namib Desert, Namibia: Omdel Aquifer as case study." University of Western Cape, 2020. http://hdl.handle.net/11394/7852.

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Philosophiae Doctor - PhD<br>The study addressed the groundwater assessment and sustainable management of the coastal alluvial aquifers in Namib Desert, the Omaruru River Delta Aquifer (Omdel Aquifer) was used as a case study. Sustainable utilization of groundwater in parts of hyper-arid Sub-Saharan Africa, like the Namib Desert, is always a challenge due to lack of resources and data. Understanding of hydrogeological characteristics of the Omaruru Delta Aquifer System is a pre-requisite for the management of groundwater supply in the Central Namib area (Namib Desert). For the Omdel Aquifer in
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Jobst, Petra. "Investigating water problems of F. albida along the Kuiseb river, Namibia." Thesis, University of Cape Town, 1996. http://hdl.handle.net/11427/25898.

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Spaggiari, Renato Igino. "Sedimentology of plio-pleistocene gravel barrier deposits in the palaeo-Orange River mouth, Namibia : depositional history and diamond mineralisation." Thesis, Rhodes University, 2011. http://hdl.handle.net/10962/d1004636.

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The largest known marine diamond placer, the Namibian mega-placer, lies along the Atlantic coast of south-western Africa from the Orange River mouth 1,000 km northwards to the Namibian-Angolan border. The most economically viable portion of the Namibian mega-placer (>75 million carats recovered at >95% gem quality) comprises onshore and offshore marine deposits that are developed within ∼100km of the Orange River outfall. For much of the Cainozoic, this long-lived fluvial system has been the main conduit transporting diamonds from kimberlitic and secondary sources in the cratonic hinterland of
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Nakashole, Albertina Ndahafifwa. "Heavy minerals in the palaeo and modern Orange River and offshore southern Namibia." Thesis, University of Leeds, 2017. http://etheses.whiterose.ac.uk/20057/.

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Linking the erosional record of drainage basins with the depositional record of sedimentary basins is a major challenge in geosciences. Thick diamondiferous gravel terrace deposits along the lower Orange River and their coeval downstream offshore deposits provide a rare opportunity for understating source-to-sink relationships. Two distinct gravel terrace deposits are recognised, based on clast and heavy mineral assemblage analysis at Boom, Lorelei, Sendelingsdrif, Daberas, Auchas Major, Auchas Lower and Arrisdrif, referred to as the Proto and Meso Orange River deposits. These are compared to
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Kamwi, Innocent Silibelo. "Fitting extreme value distributions to the Zambezi river flood water levels recorded at Katima Mulilo in Namibia." Thesis, University of the Western Cape, 2005. http://etd.uwc.ac.za/index.php?module=etd&amp.

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The aim of this research project was to estimate parameters for the distribution of annual maximum flood levels for the Zambezi River at Katima Mulilo. The estimation of parameters was done by using the maximum likelihood method. The study aimed to explore data of the Zambezi's annual maximum flood heights at Katima Mulilo by means of fitting the Gumbel, Weibull and the generalized extreme value distributions and evaluated their goodness of fit.
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Van, der Merwe Schalk. "Is commercial livestock farming environmentally viable within the Orange and Fish River catchment area (OFCA) of Southern Namibia?" Master's thesis, University of Cape Town, 2001. http://hdl.handle.net/11427/4811.

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Includes bibliographical references.<br>There are neither historical nor current baseline information relating to the productivity of the OFCA veld and a definite link between the current crisis and the possibly that it is suffering from the effects of having farmed the OFCA veld into a state of durable suboptimal productivity remains to be conclusively established. This current study has been undertaken in order to investigate such a possible link, and to reach a more definite conclusion with regards to the contribution of negative environmental feedback which may have arisen from commercial
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Jacobson, Peter James. "An ephemeral perspective of fluvial ecosystems: Viewing ephemeral rivers in the context of current lotic ecology." Diss., Virginia Tech, 1997. http://hdl.handle.net/10919/30582.

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Hydrologic and material dynamics of ephemeral rivers were investigated in the Namib Desert to assess how hydrologic regimes shape the physical habitat template of these river ecosystems. An analysis of long-term hydrologic records revealed that the variation in mean annual runoff and peak discharge were nearly four times higher than the global average, rendering the rivers among the most variable fluvial systems yet described. Further, a pronounced downstream hydrologic decay characterized all of the rivers. The high spatio-temporal variability in flow was reflected in patterns of material tra
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Books on the topic "Rivers – Namibia"

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Jacobson, Peter J. Ephemeral rivers and their catchments: Sustaining people and development in western Namibia. Desert Research Foundation of Namibia, 1995.

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Julian, Fennessy, Schneider Stephanie, Desert Research Foundation of Namibia., and Gobabeb Training and Research Centre., eds. Hoanib River catchment study, northwestern Namibia: Water. Desert Research Foundation of Namibia, 2001.

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Julian, Fennessy, Schneider Stephanie, Desert Research Foundation of Namibia., and Gobabeb Training and Research Centre., eds. Hoanib River catchment study, northwestern Namibia: Fauna. Desert Research Foundation of Namibia, 2001.

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Julian, Fennessy, Schneider Stephanie, Desert Research Foundation of Namibia., and Gobabeb Training and Research Centre., eds. Hoanib River catchment study, northwestern Namibia: Soil. Desert Research Foundation of Namibia, 2001.

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Julian, Fennessy, Schneider Stephanie, Desert Research Foundation of Namibia., and Gobabeb Training and Research Centre., eds. Hoanib River catchment study, northwestern Namibia: Vegetation. Desert Research Foundation of Namibia, 2001.

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Ward, J. D., Ph. D. The Cenozoic succession in the Kuiseb Valley, central Namib Desert. Geological Survey of South West Africa/Namibia, 1987.

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J, Abbott. The 2002 joint frame survey of fisheries on the Upper Zambezi River (Namibia/Zambia). Directorate of Environmental Affairs, Ministry of Environment and Tourism, 2003.

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New approaches to the study of surface palaeolithic artefacts: A pilot project at Zebra River, Western Namibia. Archaeopress, 2011.

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Fisch, Maria. Die Kavangojäger im Nordosten Namibias: Jagdmethoden, religiös-magische Praktiken, Lieder und Preisgedichte. Namibia Wissenschaftliche Gesellschaft, 1994.

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Image, Cool. Epupa Waterfall with Rainbow on Kunene River Angola/Namibia Border Journal: 150 page lined notebook/diary. CreateSpace Independent Publishing Platform, 2016.

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Book chapters on the topic "Rivers – Namibia"

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Crerar, S., R. G. Fry, P. M. Slater, G. Langenhove, and D. Wheeler. "An Unexpected Factor Affecting Recharge from Ephemeral River Flows in SWA/Namibia." In Estimation of Natural Groundwater Recharge. Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-015-7780-9_2.

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Amutenya, Jacobine Taukondjele, and Gerald (Augusto) Corzo Perez. "Infrastructures for Data in the Context of Flow Forecasting Using Artificial Neural Network Model for Okavango River in Namibia." In Advances in Environmental Engineering and Green Technologies. IGI Global, 2019. http://dx.doi.org/10.4018/978-1-7998-0163-4.ch007.

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A number of evolutions on data collection and sharing have been published. Countries have collected data, but lack of access and complexity to implement these technologies has limitations. HydroServer Lite, a web-based server for sharing water data, helps to address the need of data sharing and storing in a standard format. Namibia Hydrological Services has no common online system for storing and sharing of water data. This study extends the research on HSL features as data system linked to online ANN forecasting model. This is done by implementing a Namibian HSL using real-time connection to the database to operate in real-time tools developed to visualize and fill in missing data. Lastly, a model was build using Waikato Environment for Knowledge Analysis. Results of the best model obtained are coded in hypertext preprocessor with near real-time data to provide continuous forecast. Linking data system for water resource management in a standard format is practical and promising.
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Mbukusa, Nchindo Richardson. "Understanding indigenous coping strategies of the Basubiya on the flooded plains of the Zambezi River." In Indigenous Knowledge of Namibia. University of Namibia Press, 2015. http://dx.doi.org/10.2307/j.ctvgc619h.17.

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Unganai, Leonard S. "Monitoring Agricultural Drought in Southern Africa." In Monitoring and Predicting Agricultural Drought. Oxford University Press, 2005. http://dx.doi.org/10.1093/oso/9780195162349.003.0030.

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Southern Africa lies between 0°S to 35°S latitude and 10°E to 41°E longitude. In this region, annual rainfall ranges from below 20 mm along the western coastal areas of Namibia to as high as 3000 mm in some highland areas of Malawi. Rainfall generally increases from south to north in response to topography and the main rain-bearing systems affecting the subregion. In the southwest sections of the sub-region, annual rainfall averages below 400 mm, whereas the high-altitude areas receive up to 3000 mm due to orographic enhancement. Two important features that control the climate of southern Africa are the semipermanent subtropical high-pressure cells centered in the southeast Atlantic and the southwest Indian Ocean. These subtropical high pressure cells are associated with widespread and persistent subsidence (Lockwood, 1979). Part of southern Africa is under the downward leg of the Hadley Cell, superposed on the zonal Walker cell. The complex interaction of these cells, particularly during warm El Niño/Southern Oscillation (ENSO) episodes, is usually associated with drier than normal austral summers over much of southern Africa. Much of southern Africa is therefore semiarid and prone to recurrent droughts. In South Africa, for operational purposes, a drought is broadly defined as occurring when the seasonal rainfall is 70% or less of the long-term average (Bruwer, 1990; Du Pisani, 1990). It becomes a disaster or severe drought when two or more consecutive rainfall seasons experience drought. Drought affects some part of southern Africa virtually every year. Southern Africa has suffered recurrent droughts since record keeping began (Nicholson, 1989; Unganai, 1993). Severe drought periods included 1800– 30, 1840–50, 1870–90, 1910–15, 1921–25, 1930–50, 1965–75, and 1980–95. During some of these drought periods, rivers, swamps, and wells dried up and well-watered plains turned into barren lands. For Zimbabwe, the worst drought years were 1911–12, 1923–24, 1946–47, 1972–73, 1981–82, 1982–83, 1986–87, and 1991–92 (Zimbabwe Department of Meteorological Services, personal communication, 2002). During the severe and recurrent droughts of the 1980s and 1990s, the impact on vulnerable communities and the environment was catastrophic.
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Mfundisi, Kelebogile B., Alex M. Mudabeti, and Anastacia Makati. "Integrating Geoinformatics and Remote Sensing Data to Assess Impacts of Flooding on Land Productivity in the Zambezi River Floodplains, Namibia." In Advances in Geospatial Technologies. IGI Global, 2018. http://dx.doi.org/10.4018/978-1-5225-3440-2.ch013.

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Exposure to flood waters poses a risk to land productivity and livelihoods of communities in the Zambezi River Basin who are engaged in arable agricultural activities along its floodplains. This is exacerbated by occurrence of frequent flooding events in the area since 2008 due to climate variability. The objective of this research is to assess the extent of exposure to flooding on floodplain land used for maize production along the Zambezi River in Namibia. Existing survey information on geospatial locations of farms is used as baseline data. Field survey maps are then overlaid into flood maps developed using 2013 Landsat satellite data taken during peak flood event, and DEM. Weighted sum overlay results show that 14.5% of croplands were inundated with floods by March 2013. Integration of inundation results into a DEM show areas at low, medium and high risk to flooding. This provides useful geospatial information for flood mitigation.
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"The strengthening and widening of the Okavango River Bridge in Northern Namibia." In Research and Applications in Structural Engineering, Mechanics and Computation. CRC Press, 2013. http://dx.doi.org/10.1201/b15963-437.

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Mitchell, Graham. "The Scientific Age." In How Giraffes Work. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780197571194.003.0003.

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Scientific study of giraffes depended on the scientists of Europe being able to study specimens. The first of those specimens was sent to Europe not long after the establishment of a settlement at the Cape of Good Hope in South Africa in 1652. Obtaining the specimens was difficult because the nearest giraffes were to be found along the Gariep (Orange) River on the northern border of South Africa with Namibia, about 1,000 km from the Cape, across arid and inhospitable terrain. The first specimens were collected by Robert Jacob Gordon and William Paterson and were sent to Holland and England, respectively. Their arrival attracted zoologists and others to southern Africa, and further specimens became available for study. In the early 1800s establishment of zoos in Europe meant that living giraffes could be studied, and the first of these were taken to France and England. Among the prominent scientists who studied giraffes were Etienne Geoffroy St.-Hilaire in Paris and Richard Owen in London. Their studies established the scientific basis for the study of giraffes.
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Amakali, Maria, and Larry A. Swatuk. "Different Approaches to Local Level Participation in River Basin Management in Namibia: A Comparison Between the Kuiseb and Cuvelai Basins." In Transboundary Water Governance in Southern Africa. Nomos Verlagsgesellschaft mbH & Co KG, 2009. http://dx.doi.org/10.5771/9783845212890-111.

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Conference papers on the topic "Rivers – Namibia"

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Nicoll, Kathleen. "SOURCING RIVER ROCK AND MIDDLE STONE AGE ARTEFACTS DISCOVERED ALONG THE CUNENE RIVER, ANGOLA-NAMIBIA BORDER, SOUTHERN AFRICA." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-300521.

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Maus, Stefan, K. P. Sengpiel, and E. A. W. Tordiffe. "Variogram analysis of magnetic data to identify paleochannels of the Omaruru River in Namibia." In SEG Technical Program Expanded Abstracts 1996. Society of Exploration Geophysicists, 1996. http://dx.doi.org/10.1190/1.1826365.

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Enzel, Yehouda, Tamir Grodek, Efrat Morin, et al. "STAGE, DURATION, AND TRANSMISSION LOSSES OF KUISEB RIVER FLOODS ACROSS THE NAMIB AND VEGETATION DYNAMICS AND DISTRIBUTION ACROSS FLOODPLAIN AND RARELY-FLOODED DOWNSTREAM REACHES." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-282206.

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