Relevant bibliographies by topics / The Warta River Basin

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Academic literature on the topic 'The Warta River Basin'

Author: Grafiati
Published: 4 June 2021
Last updated: 18 February 2022

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Journal articles on the topic "The Warta River Basin"

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Ilnicki, Piotr, Ryszard Farat, Krzysztof Górecki, and Piotr Lewandowski. "Long-term air temperature and precipitation variability in the Warta River catchment area." Journal of Water and Land Development 27, no. 1 (December 1, 2015): 3–13. http://dx.doi.org/10.1515/jwld-2015-0019.

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Abstract The variability of the mean annual air temperature and precipitation totals in three periods: 1848–2010, 1951–2010 and 1981–2010 was investigated in the large Warta River basin, being the area with lowest rainfall in Poland. For the purposes of research, nine meteorological stations with the longest measurement series were selected. Air temperature increase in this river basin was similar than in neighbouring countries. In the last 30 years this trend kept increasing. The precipitation in the whole studied period was slightly increasing in the northern part of the Warta River basin, but decreasing in the southern part. The mean annual precipitation totals in the catchment area did not change visible. In the period 1981–2010, the precipitation totals show a small increase in the winter and spring and a decrease in summer. A negative influence of this climate change was not visible in the Warta River discharge. The main objectives of this study were the collection long-term records of air temperature and precipitation in the Warta River basin, and the statistical analysis of climate variability.
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Weckwerth, Piotr. "Palaeoslopes of Weichselian sand-bed braided rivers in the Toruń Basin (Poland): results of a palaeohydraulic analysis." Geologos 17, no. 4 (December 1, 2011): 227–38. http://dx.doi.org/10.2478/v10118-011-0013-6.

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Palaeoslopes of Weichselian sand-bed braided rivers in the Toruń Basin (Poland): results of a palaeohydraulic analysis Palaeoslopes of Weichselian sand-bed braided rivers have been reconstructed for two stages of fluvial development in the Toruń Basin. (1) The palaeoslope of the ‘fossil’ fluvial succession (buried under Weichselian tills) was calculated on the basis of the median grain size and the Shields parameter. The hydraulic gradient thus found is comparable with the hydraulic gradient of the present-day river. (2) The second developmental stage of the Toruń Basin (as a apart of the Noteć-Warta ice-marginal valley) took place after deglaciation. The slopes of river terraces are a few times lower than those calculated on the basis of the Shields parameter. The palaeoslope of the then river was estimated on the basis of a constant interdependency between the braidplain width, the channel geometry and the grain size. The river gradient that was thus calculated is similar to the measured terrace slope. Palaeoslope estimates in valleys similar to those in the Toruń Basin should consider the width of the braidplain.
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WIETESKA, Zbigniew, and Anna DOBKOWSKA. "ASSESSMENT OF THE INFLUENCE OF DISCREPANCY OF THE LOCATION OF GROUNDWATER AND SURFACE WATERSHEDS ON THE QUANTITY OF CALCULATED RENEWABLE RESOURCES, EXEMPLIFIED BY THE P-IX BALANCE REGION IN THE WARTA WATER REGION." Biuletyn Państwowego Instytutu Geologicznego 471 (October 1, 2018): 185–92. http://dx.doi.org/10.5604/01.3001.0012.5055.

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The article presents the results of research on the renewal of a hydrogeological system that is characterized by a significant discrepancy of the location of groundwater and surface watersheds. The area of the hydrological and hydrogeological studies is part of the P-IX balance region (Warta River from the Prosna to the Mosiński Canal) located south of the Warta River. The evaluation of groundwater renewability has been made using a hydrological method and mathematical modelling. When using the hydrological method, which is a commonly used control method for water balance calculations, it is assumed that the surface and groundwater watersheds are identical. Comparison of the results of water balance calculations obtained with both methods required the assessment of the compatibility of the groundwater catchment and morphological boundaries. This was done by calculating the difference between the quantities of renewable resources determined by two variants of the hydrological method. In the first (standard) variant, renewable resources were determined based on data from water-gauge and hydrometric profiles closing the catchments of the Warta tributaries draining the analyzed water-management regions. In the second (extended) method, they were determined based on data from water gauges controlling the Warta sub-basin. Enlargement of the balanced unit as far as the boundaries of the Warta basin was consistent with the principle that the reliability of calculations of groundwater resources increases proportionally to the analyzed catchment area and the significance of its drainage zone in the regional groundwater circulation (Toth, 1963). The quantity of renewable resources determined by the standard and extended variants of the hydrological method amounted to 107,100 m3/day and 184,000 m3/day, respectively. The difference is 72% of the value determined using the standard method. The article also provides an analysis of the spatial and temporal variability of the nature of the hydraulic relationship between surface water and groundwater, and the influence of this variability on the reliability of water balance calculations, based on stationary observations of surface water flow.
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Pietruczuk, Karol, Krzysztof Dajewski, Anna Garbarczyk, and Krzysztof Szoszkiewicz. "Hydromorphological variability of a large lowland river based on the Hydromorphological Index for Rivers (HIR) basing on the Warta River." Inżynieria Ekologiczna 21, no. 2 (June 1, 2020): 15–25. http://dx.doi.org/10.12912/23920629/122656.

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Żelazna-Wieczorek, Joanna, and Monika Mamińska. "Algoflora and vascular flora of a limestone spring in the Warta river valley." Acta Societatis Botanicorum Poloniae 75, no. 2 (2011): 131–43. http://dx.doi.org/10.5586/asbp.2006.016.

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Qualitative analysis of algae, including microhabitats and vascular vegetation in a spring niche, together with basic physical and chemical characteristics is presented. 175 diatom taxa as well as taxa of macroalgae and vascular plants were determined in the spring niche, and the community types were defined. Seasonal variability of diatom communities was observed. The influence of a flood as a catastrophe on the community of diatoms and macroalgae was noticed.
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Linnerooth-Bayer, Joanne, Anna Dubel, Jan Sendzimir, and Stefan Hochrainer-Stigler. "Challenges for mainstreaming climate change into EU flood and drought policy: Water retention measures in the Warta River Basin, Poland." Regional Environmental Change 15, no. 6 (September 19, 2014): 1011–23. http://dx.doi.org/10.1007/s10113-014-0643-7.

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Wilk, Paweł, Paulina Orlińska-Woźniak, and Joanna Gębala. "The river absorption capacity determination as a tool to evaluate state of surface water." Hydrology and Earth System Sciences 22, no. 2 (February 7, 2018): 1033–50. http://dx.doi.org/10.5194/hess-22-1033-2018.

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Abstract. In order to complete a thorough and systematic assessment of water quality, it is useful to measure the absorption capacity of a river. Absorption capacity is understood as a pollution load introduced into river water that will not cause permanent and irreversible changes in the aquatic ecosystem and will not cause a change in the classification of water quality in the river profile. In order to implement the method, the Macromodel DNS/SWAT basin for the Middle Warta pilot (central Poland) was used to simulate nutrient loads. This enabled detailed analysis of water quality in each water body and the assessment of the size of the absorption capacity parameter, which allows the determination of how much pollution can be added to the river without compromising its quality class. Positive values of the calculated absorption capacity parameter mean that it is assumed that the ecosystem is adjusted in such a way that it can eliminate pollution loads through a number of self-purification processes. Negative values indicate that the load limit has been exceeded, and too much pollution has been introduced into the ecosystem for it to be able to deal with through the processes of self-purification. Absorption capacity thus enables the connection of environmental standards of water quality and water quality management plans in order to meet these standards.
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Graf, Renata, and Pouya Aghelpour. "Daily River Water Temperature Prediction: A Comparison between Neural Network and Stochastic Techniques." Atmosphere 12, no. 9 (September 7, 2021): 1154. http://dx.doi.org/10.3390/atmos12091154.

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The temperature of river water (TRW) is an important factor in river ecosystem predictions. This study aims to compare two different types of numerical model for predicting daily TRW in the Warta River basin in Poland. The implemented models were of the stochastic type—Autoregressive (AR), Moving Average (MA), Autoregressive Moving Average (ARMA) and Autoregressive Integrated Moving Average (ARIMA)—and the artificial intelligence (AI) type—Adaptive Neuro Fuzzy Inference System (ANFIS), Radial Basis Function (RBF) and Group Method of Data Handling (GMDH). The ANFIS and RBF models had the most fitted outputs and the AR, ARMA and ARIMA patterns were the most accurate ones. The results showed that both of the model types can significantly present suitable predictions. The stochastic models have somewhat less error with respect to both the highest and lowest TRW deciles than the AIs and were found to be better for prediction studies, with the GMDH complex model in some cases reaching Root Mean Square Error (RMSE) = 0.619 °C and Nash-Sutcliff coefficient (NS) = 0.992, while the AR(2) simple linear model with just two inputs was partially able to achieve better results (RMSE = 0.606 °C and NS = 0.994). Due to these promising outcomes, it is suggested that this work be extended to other catchment areas to extend and generalize the results.
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Susware, Nilesh K., Jagdish B. Sapkale, Vinaya N. Susware, and Shubham K. Gavhane. "Linkages Between Sinuosity Index and Flood Sustainability: A Study of Morna River (Maharashtra), India." Current World Environment 16, no. 2 (August 30, 2021): 649–61. http://dx.doi.org/10.12944/cwe.16.2.28.

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The morphological changes in the river channel over periods that occur due to the flood events, affected the sinuosity index of the river channel. The river characteristic like sinuosity also determines the intensity of flood in a channel. Recent flood losses have increased as a result of variability in rainfall; simultaneously such problems are coming up with sustainable development. The attempted research study has been carried out to evaluate and understand the river channel changes and bank stability of the Morna river in Maharashtra. The research work also identified the pattern/planform of the river. Morna river meets Warna river near the Mangle village. Most of the streams in the upper basin area are non-perennial. The occurrence of floods takes place due to seasonal rainfall. An index of Sinuosity was used to analyze variation in river courses, as well as identify stability and instability. Therefore, this may facilitate predicting probable riverbank erosion sites and also support sustainable flood management planning for these sites during forthcoming flood events. The sinuosity index of the Morna river ranges from 1.09 to 1.44. The sinuosity indexes for the Morna river and tributaries of its sub-basins/watersheds have been calculated using geospatial techniques. The disparities in sinuosity indexes of the Morna basin and sub-watersheds having a good correlation with slope of the river , fluvial processes, water discharge and hydraulic aspects of the river channel. Seasonal potential flood risk for the agricultural land may be found at the confluence of the Warna river and its tributary Morna river when it receives heavy rainfall in upstream.
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Krąpiec, Marek, Danuta J. Michczyńska, Adam Michczyński, Natalia Piotrowska, Tomasz Goslar, and Elżbieta Szychowska-Krąpiec. "Late Glacial Atmospheric Radiocarbon Variations Recorded in Scots Pine (Pinus sylvestris L.) Wood from KwiatkÓw, Central Poland." Radiocarbon 60, no. 4 (August 2018): 1029–40. http://dx.doi.org/10.1017/rdc.2018.71.

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ABSTRACTOur project aimed to construct a Scots Pine (Pinus sylvestris L.) chronology for part of the Late Glacial and reconstruct changes in the 14C concentrations during this period. Kwiatków (Kolska Basin, central Poland) proved to be very prospective site, in which wood from the end of Allerød was recognized. A level of organic deposits with so-called fossil forest was encountered within the late-Vistulian terrace of the low valley of the Warta river. Dendrochronological analysis of over 267 samples complying to the requirements of the method allowed, at the present stage of the research, to construct a chronology spanning 265 yr. Fifty-two samples (5 consecutive rings each) were subjected to α-cellulose extraction and 14C measurements. Ninety-six results and the wiggle-matching technique anchor the chronology to the period 13,821–13,561 cal BP (Acomb=141.6%) according to the D_Sequence procedure and the IntCal13 calibration curve or to 13,800–13,540 cal BP according to the wiggle-matching technique using the χ2 test and raw data, i.e. the Heidelberg tree-ring sequence.
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Dissertations / Theses on the topic "The Warta River Basin"

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Dorozynska, Dorota. "En studie av retentionen i floden Oder och dess avrinningsområden, Polen." Thesis, Linköping University, Linköping University, 2004. http://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-2597.

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Nutrient enrichment is the main cause of the increasing eutrophication process in the Baltic Sea during last century. A prerequisite counteract this process the load of nutrients to the Sea must be investigated. The large contribution of nutrients to the Sea is caused by emission from the rivers within the drainage basin. For the total emission of nutrient into the Sea the retention process in the rivers has big influence. This process in the river system has been assumed as a not important part of the nutrient cycle. However some investigators have pointed out that the retention process occurs in the river and be an important part of the nutrient dynamics in the river. For the object of investigation the Odra River Basin was chosen, as an example of a large river basin in the Baltic Sea Drainage Basin. The Odra River is mainly localized in Poland and contributes substantially to the eutrophication of the Baltic Proper. The Odra River is one of the least dammed major rivers of the Baltic Proper and as such of especial interest in retention studies. The phosphorus was chosen as an example of nutrient in the eutrophication process. The purpose of the investigation is to determine the phosphorus retention within the river. Two different models were used to calculate the retention process in the river. The"Multiple Regression Model"turned out to be insignificant, therefore the results were computed by using a “similarity model”, based on similarities between load from monitored tributary basins and the rest of the sub-basin. The retention in the Odra River in the amounted to -4608 t yr-1, which is 43% of the total phosphorus emission to the Odra River. There is also stated that in the Notec and the Warta rivers the retention process occur in the amount of -1940 t yr-1 and -3007 t yr-1 respectively.

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O'Donnell, Thomas Kevin. "River restoration in the upper Mississippi River Basin." Diss., Columbia, Mo. : University of Missouri-Columbia, 2006. http://hdl.handle.net/10355/4532.

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Thesis (M.S.) University of Missouri-Columbia, 2006.
The entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file (viewed on August 27, 2007) Includes bibliographical references.
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Adayi, Daniel. "River basin organisation in Nigeria : the case of the lower benue river basin development authority." Doctoral thesis, Instituto Superior de Economia e Gestão, 2019. http://hdl.handle.net/10400.5/19091.

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Doutoramento em Estudos de Desenvolvimento
A gestão de bacias hidrográficas tem uma dimensão inerentemente política uma vez que envolve tomar decisões que são limitadas pelos contextos institucionais, caracterizados por escassez de recursos e conflitos entre múltiplos atores, políticas e estruturas institucionais. No caso de nações em desenvolvimento que padecem de instabilidades políticas, a gestão de bacias hidrográficas torna-se um teatro político em que os principais objetivos de produção alimentar e gestão ambiental ficam fragilizados perante complexos interesses políticos que envolvem o controlo de recursos, a governação de organizações e a política partidária. Enquanto medida de recuperação no pós-guerra e com o apoio das Nações Unidas, a Nigéria adotou uma abordagem integrada para a gestão das bacias hidrográficas. Esta gestão cabe às Autoridades para o Desenvolvimento das Bacias Hidrográficas (ADBH) que estão sob a alçada do governo federal. A sua evolução reflete a instabilidade que caracteriza o federalismo nigeriano. Envolvidas numa política faccionária, com recorrentes intervenções militares e várias reformas no setor da água, as ADBH têm tido um desempenho abaixo do esperado. Este estudo visa explorar a economia política das ADBH na Nigéria, mais concretamente, a trajetória de desenvolvimento das ADBH enquanto reflexo do instável federalismo nigeriano. O documento está organizado em seis capítulos autónomos mas interligados que, no conjunto, encerram uma análise de nível macro e outra de nível micro. O primeiro capítulo descreve a forma como diferentes líderes nigerianos deixaram a sua marca no desenvolvimento das ADBH, desde a sua fundação até à presente administração de Muhammadu Buhari. De uma forma ou de outra, todos os grandiosos planos para aumentar a produção alimentar terminaram em nobres ambições. O capítulo inicia-se com a identificação dos motivos que desencadearam a reorganização da rede hidrográfica na Nigéria. O rescaldo da Guerra Civil, as secas na região do Sahel e a pressão da publicação do relatório das Nações Unidas em 1969 encontram-se entre os principais motivos. Depois de um fraco desempenho inicial em que vários princípios da gestão integrada das bacias hidrográficas foram ignorados, seguiu-se um conjunto de contributos de chefes de estado e presidentes. Infelizmente, nenhuma das promessas feitas surtiu os resultados esperados. O segundo capítulo analisa as ADBH à luz da turbulência que caracterizou o federalismo nigeriano, utilizando o paralelismo como estilo. Este capítulo inicia-se com a discussão do conceito de Federalismo enquanto sistema político e prossegue com a conclusão de que o federalismo existente na Nigéria é peculiar. No início do processo de independência nigeriano, os grupos étnicos não negociaram os termos deste federalismo e a governação militar continuada erodiu os já frágeis pilares criados pelos fundadores da nação. O sistema militar criou os estados e as áreas de governo locais por fragmentação, bem como os mecanismos federais, como são exemplo as três Constituições pós-independência e o Princípio do Carácter Federativo (PCF). O capítulo aborda igualmente vários fatores que influenciaram este paralelismo entre as trajetórias do federalismo nigeriano e das ADBH, nomeadamente, a delicada e volátil questão das minorias, o papel dos militares, o boom petrolífero da década de 70 e o PCF enquanto mecanismo de consociativismo e as recorrentes descontinuidades das políticas públicas e de governação. O paralelismo estabelecido mostra-nos que as ADBH tem uma trajetória que espelha a turbulência do federalismo nigeriano. O terceiro capítulo conclui a primeira parte da tese. Este capítulo foca-se nas reformas introduzidas por diferentes administrações das ADBH e na forma como a organização foi afetada por essas reformas. Os desafios colocados às ADBH começaram com a administração de Shagari, na década de 80, apesar da primeira tentativa para reposicionar as bacias hidrográficas ter ocorrido apenas no final dessa década, com o Programa de Ajustamento Estrutural de Babangida (PAE). Neste capítulo são detalhados o quadro de comercialização parcial criado e alguns dos seus conceitos centrais, as várias fases de preparação das ADBH para o seu novo estatuto, o seu processo de recapitalização e o cronograma da organização até se tornar financeiramente autossuficiente. Todo este processo foi condicionado pela cedência de Babangida à pressão pública e sua consequente demissão. Depois desta tentativa de comercialização das ADBH, várias outras se seguiram mas nenhuma foi bem-sucedida. No capítulo quatro inicia-se a segunda parte da tese, que corresponde a uma abordagem de nível micro à Autoridade para o Desenvolvimento da Bacia Hidrográfica do rio Lower Benue (ADBHLB), uma das doze autoridades existentes no país. Foi dado enfoque a como é que as dinâmicas observadas na primeira parte da tese ocorrem no contexto de apenas uma Autoridade. Este quarto capítulo documenta as observações conseguidas em projetos de irrigação da ADBHLB. As evidencias apresentadas provêm de dezasseis instalações da organização, incluindo a sua sede. Na conclusão do capítulo, são discutidos os traços característicos dos projetos de irrigação. Todos os projetos tem recursos naturais abundantes tais como vastos terrenos, acesso a água e localização em planícies férteis. No entanto, são disfuncionais e tornaram-se dívida pública. A constante mudança política deixou uma longa cadeia de construções inacabadas (e.g. a barragem inacabada de Guma, os terrenos abandonados em Tede ou sistemas de irrigação inacabados em Doma e Guma) e gestores de projeto desesperados. O capítulo cinco trata os impactos da fragmentação do federalismo ao nível de análise micro e detalha como é que o conflito de interesses se transformou à medida que o numero de partes interessadas na ADBHLB aumentou. Este capítulo dá-nos a conhecer como é que a ADBHLB reflete a instabilidade do federalismo nigeriano através de ilustrações da fragmentação estrutural da bacia hidrográfica da ADBHLB, que passou de dois estados fundadores (Benue e Plateau) para quatro (Benue, Plateau, Kogi e Nasarawa), após a fragmentação dos estados fundadores. O capítulo apresenta igualmente casos em que a ADBHLB se tornou uma plataforma política na medida em que os seus executivos de topo utilizam as instalações governamentais para alcançar os seus objetivos políticos. Neste capítulo, é possível concluir que os reveses descritos são um efeito em cascata da fraca negociação do federalismo na Nigéria. O sexto e último capítulo da tese dedica-se a como a ADBHLB respondeu à política de comercialização parcial de Babangida, o esforço renovado de Obasanjo e administrações seguintes. O capítulo inicia-se com a análise do quadro para a comercialização criado pelo governo federal e o plano articulado pela ADBHLB como resposta. O plano estratégico da organização traçou a forma como a ADBHLB se deveria impor no mercado competitivo mas não foi feita qualquer implementação. O capítulo finaliza com a conclusão de que o plano estratégico da ADBHLB foi mal sucedido, com base numa análise aprofundada dos relatórios do trabalho de campo realizado. Esta investigação foi afetada pela limitação do acesso a documentação oficial, tanto ao nível federal como ao nível da ADBHLB. Além disso, a falta de segurança vivida no país não permitiu a cobertura de todas as instalações da ADBHLB. Contudo, o estudo mostra claramente que o fraco desempenho das ADBH reflete a instabilidade do federalismo fragmentado nigeriano. A busca pela revitalização, reposição e comercialização parcial das ADBH deve ter em consideração as suas motivações. O documento termina com um conjunto de sugestões de pesquisa futura. Entre elas, inclui-se uma análise das políticas que estão a conduzir ao crescimento do número de ADBH e, em particular, ao argumento de que não há correlação entre a dimensão das ADBH e a dotação orçamental recebida do governo federal.
The management of river basin organisations is inherently political, due to its unalienable constraints and institutional structures. Characterised by resources limitedness, conflicts of multiple actors, policies, and evolving institutional structures, river basin organisation often becomes the centre of political intrigue and power-play. In developing nations struggling with political instabilities, river basin management is the theatre of complicated politics, and its yield is often minimal since the primary goal of agriculture becomes emasculated by other interests. This study explores the political economy of the River Basin Development Authorities (RBDAs) as a mirror phenomenon of Nigeria’s peculiar and challenge-laden federalism. The mission of the RBDAs become an instrument in the politics of fissiparous fragmentations, recurrent military interventions, and a series of reforms in the water sector. In six separate but interrelated chapters, set out as macro-level and micro-level analyses, this study explores the development trajectory of the RBDAs as a reflection of the turmoil that characterises Nigerian federalism. The macro-analyses focus on the federal actors, while the micro-analyses examine the case of the Lower Benue River Basin Development Authority (LBRBDA). The literature review and the field trips confirm, at both levels of analysis, the claim that river basin organisation is intrinsically political. The study also found that the social life or the politics of the RBDAs derive its push from the general politics of its ambient environment, and bears a likeness to it, as exemplified by the case study. The quest to reposition Nigeria’s ailing RBDAs must further explore the role that politics plays in the creation and management of the RBDAs. The insights from the study will prove valuable to the stakeholders and policymakers. Considering the findings and limitations, the conclusion also highlights some areas for further research.
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Nakamura, Takehiro. "Ecosystem-based river basin management : its conceptual development and policy application in the Yangtze River basin." 京都大学 (Kyoto University), 2007. http://hdl.handle.net/2433/137095.

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Refsgaard, Jens Christian. "Hydrological modelling and river basin management." København : GEUS, 2007. http://www.geus.dk/program-areas/water/denmark/rapporter/geus_special_rap_1_2007.pdf.

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Watson, Thomas J. "Wind River Basin, Wyoming streamflow reconstructions." Laramie, Wyo. : University of Wyoming, 2007. http://proquest.umi.com/pqdweb?did=1400958981&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.

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Norreys, Richard. "Water quality river impact model (RIM) for river basin management." Thesis, University of Salford, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.305863.

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Shimizu, Daigo. "People's Water and River Perceptions in the Selangor River Basin, Malaysia." Kyoto University, 2020. http://hdl.handle.net/2433/253262.

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N'Diaye, Abdoulaye. "Streamflow generation for the Senegal River basin." Thesis, The University of Arizona, 1985. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_e9791_1985_157_sip1_w.pdf&type=application/pdf.

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Jenkins, William Owen. "Decision support systems in river basin management." Thesis, Imperial College London, 1988. http://hdl.handle.net/10044/1/47123.

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Books on the topic "The Warta River Basin"

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Blomquist, William A. Institutional and policy analysis of river basin management: The Warta River Basin, Poland. [Washington, D.C: World Bank, 2005.

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Massachusetts. Division of Water Resources. Charles River Basin. [Boston]: Massachusetts Water Resources Commission, 1988.

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Massachusetts. Division of Water Resources. Hudson River Basin. [Boston]: Massachusetts Water Resources Commission, 1989.

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Deng, Xiangzheng, and John Gibson, eds. River Basin Management. Singapore: Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-10-0841-2.

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Melesse, Assefa M., Wossenu Abtew, and Shimelis G. Setegn, eds. Nile River Basin. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-02720-3.

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Melesse, Assefa M., ed. Nile River Basin. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-0689-7.

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International Conference on River Basin Management (5th 2009 Mellieha, Malta). River basin management V. Edited by Brebbia C. A. Southampton]: WIT, 2009.

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Eisel, Leo. Platte River Basin study. [Washington, D.C.?]: The Commission, 1997.

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Mira, Petrovic, and SpringerLink (Online service), eds. The Ebro River Basin. Berlin, Heidelberg: Springer-Verlag Berlin Heidelberg, 2011.

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International, Conference on River Basin Management (2001 ). (2nd 2003 Las Palmas Canary Islands). River basin management II. Southampton: WIT Press, 2003.

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Book chapters on the topic "The Warta River Basin"

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Das, Anirban, and Meet Panchal. "Krishna River Basin." In Springer Hydrogeology, 339–51. Singapore: Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-10-2984-4_27.

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Willems, Daphne, and Esther Blom. "Rhine River Basin." In The Wetland Book, 1–9. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6173-5_187-1.

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Meynell, Peter-John. "Mekong River Basin." In The Wetland Book, 1–22. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6173-5_244-1.

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Wittmann, Florian, and Wolfgang J. Junk. "Amazon River Basin." In The Wetland Book, 1–20. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6173-5_83-2.

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Csagoly, P., G. Magnin, and O. Hulea. "Danube River Basin." In The Wetland Book, 1–12. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6173-5_87-1.

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McCartney, Matthew, and Lisa-Maria Rebelo. "Nile River Basin." In The Wetland Book, 1–9. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6173-5_89-1.

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McCartney, Matthew, Richard Beilfuss, and Lisa-Maria Rebelo. "Zambezi River Basin." In The Wetland Book, 1–17. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6173-5_91-1.

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Harrison, Ian J., Randall Brummett, and Melanie L. J. Stiassny. "Congo River Basin." In The Wetland Book, 1–18. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6173-5_92-2.

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Willems, Daphne, and Esther Blom. "Rhine River Basin." In The Wetland Book, 923–31. Dordrecht: Springer Netherlands, 2018. http://dx.doi.org/10.1007/978-94-007-4001-3_187.

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Wittmann, Florian, and Wolfgang J. Junk. "Amazon River Basin." In The Wetland Book, 727–46. Dordrecht: Springer Netherlands, 2018. http://dx.doi.org/10.1007/978-94-007-4001-3_83.

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Conference papers on the topic "The Warta River Basin"

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MOSIEJ, Józef, and Teresa SUCHECKA. "THE ROLE OF IRRIGATION IN RIVER VALLEYS TO DEVELOP WATER QUALITY, PRODUCTION OF BIOMASS AND SUSTAINABLE RURAL DEVELOPMENT - CASE STUDY." In RURAL DEVELOPMENT. Aleksandras Stulginskis University, 2018. http://dx.doi.org/10.15544/rd.2017.076.

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Abstract:
Ner river and its valley for over 170 years has been receiver for sewages from the city of Łódź. The natural system of this region (on the border of the watershed location, limitations of water supplies sources, lack of bigger natural rivers) in connection to city growth, lead to forming of specific system involving an agglomeration and water supplies system as well as wastewaters utilization system. The Ner river valley has the great potential to be effective in production biomass for energy purposes. Irrigation with polluted Ner river water cover fast growing plants high water and nutritional requirements. This would also work for the improvement of Ner river water quality. The achievement of good quality of water is not possible without irrigation of agricultural land in river valley. An amount of sewage discharged to Ner (193,017 m³ per day) several times higher then its natural flow in river. This is a result of strategy of water supply that is supported by transfer of water from Pilica river and underground water uptake for agglomeration. Relatively high runoff coefficient in years 1952 – 2011 was equal to 0.325 for Ner, in comparison to 0.17 for other rivers in Warta watershed. Despite the low natural flow Ner river discharges annually relatively high contaminants’ load to Warta river. In the analysed period (1995-2003) the annual average flow of Ner river amounted 10 % of annual average Warta river flow below its estuary. The share of analysed indicators of contaminants’ load approximated 27 % for total nitrogen, 37 % for phosphorus, 39 % for BOD5 and 28% for suspended solids. In the period 2004-2011 the annual average flow of Ner river amounted 13.8 % of annual average Warta river flow. The share of investigated pollutants loads consists 27.9 % for total nitrogen, 42.6 % for phosphorus, 19.8 % for BOD5 and 19.6 % for suspended solids.
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GOTOH, HIROSHI, OSAMU HANADA, TADAYUKI YAMAMOTO, SHOZO TOMAKI, MINORU TANAKA, OSAMU ISHIKAWA, and MITSUO TAKEZAWA. "COUNTERMEASURES FOR THE RIVER MOUTH CLOSING OF ISHIKARI RIVER, JAPAN." In RIVER BASIN MANAGEMENT 2017. Southampton UK: WIT Press, 2017. http://dx.doi.org/10.2495/rbm170041.

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Schodro, A. E. "River bed deformations near banks and hydraulic structures due to river flow." In RIVER BASIN MANAGEMENT 2007. Southampton, UK: WIT Press, 2007. http://dx.doi.org/10.2495/rm070361.

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Santos, J. F., M. M. Portela, M. Naghettini, J. P. Matos, and A. T. Silva. "Precipitation thresholds for drought recognition: a further use of the standardized precipitation index, SPI." In RIVER BASIN MANAGEMENT 2013. Southampton, UK: WIT Press, 2013. http://dx.doi.org/10.2495/rbm130011.

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Martínez-Nájera, J. D. "On the coupling of water cycle components." In RIVER BASIN MANAGEMENT 2013. Southampton, UK: WIT Press, 2013. http://dx.doi.org/10.2495/rbm130021.

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Natakusumah, D. K., D. Harlan, and W. Hatmoko. "A new synthetic unit hydrograph computation method based on the mass conservation principle." In RIVER BASIN MANAGEMENT 2013. Southampton, UK: WIT Press, 2013. http://dx.doi.org/10.2495/rbm130031.

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Agunbiade, O. A., and O. D. Jimoh. "Flood modelling of upper Gurara watershed using remote sensing data and the geospatial streamflow model." In RIVER BASIN MANAGEMENT 2013. Southampton, UK: WIT Press, 2013. http://dx.doi.org/10.2495/rbm130041.

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Colombo, L., P. Gattinoni, S. Rizzo, and L. Scesi. "Flow modelling of dual permeability systems: the case of the Vigolana Massif (Trento, Northern Italy)." In RIVER BASIN MANAGEMENT 2013. Southampton, UK: WIT Press, 2013. http://dx.doi.org/10.2495/rbm130051.

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Morbidelli, R., C. Corradini, C. Saltalippi, A. Flammini, and R. S. Govindaraju. "The role of slope on the overland flow production." In RIVER BASIN MANAGEMENT 2013. Southampton, UK: WIT Press, 2013. http://dx.doi.org/10.2495/rbm130061.

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Moharana, S., K. K. Khatua, and M. Sahu. "Friction factor of a meandering open channel flow." In RIVER BASIN MANAGEMENT 2013. Southampton, UK: WIT Press, 2013. http://dx.doi.org/10.2495/rbm130071.

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Reports on the topic "The Warta River Basin"

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Novichkova, Tatiana. The Indus River. Basin of the river. Edited by Nikolay Komedchikov. Entsiklopediya, January 2012. http://dx.doi.org/10.15356/dm2015-12-29-3.

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Novichkova, Tatiana. The Red River. Basin of the river. Edited by Nikolay Komedchikov. Entsiklopediya, January 2012. http://dx.doi.org/10.15356/dm2016-01-11-5.

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Skone, Timothy J. Powder River Basin Coal, Extraction. Office of Scientific and Technical Information (OSTI), September 2011. http://dx.doi.org/10.2172/1509320.

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Halliwell, D. R., S. Vanderburgh, B. D. Ricketts, and L. E. Jackson. Unconfined aquifers, Fraser River Basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/184136.

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Wagner, John, Nicole Van Helden, and Nick Miller. Sheboygan River Basin Conservation Mapping Tool. The Nature Conservancy, May 2009. http://dx.doi.org/10.3411/col.08251456.

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Kukushkina, Nataliya. The Kuban. Basin of the river. Edited by Nikolay Komedchikov. Entsiklopediya, January 2012. http://dx.doi.org/10.15356/dm2015-12-08--2.

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Kukushkina, Nataliya. The Lena. Basin of the river. Edited by Nikolay Komedchikov. Entsiklopediya, January 2012. http://dx.doi.org/10.15356/dm2015-12-09-1.

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Kukushkina, Nataliya. The Mackenzie. Basin of the river. Edited by Nikolay Komedchikov. Entsiklopediya, January 2012. http://dx.doi.org/10.15356/dm2015-12-09-2.

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Kukushkina, Nataliya. The Mekong. Basin of the river. Edited by Nikolay Komedchikov. Entsiklopediya, January 2012. http://dx.doi.org/10.15356/dm2015-12-09-3.

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Kukushkina, Nataliya. The Murray. Basin of the river. Edited by Nikolay Komedchikov. Entsiklopediya, January 2012. http://dx.doi.org/10.15356/dm2015-12-10-1.

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