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1

SWAIN, ASHOK. "Ethiopia, the Sudan, and Egypt: The Nile River Dispute." Journal of Modern African Studies 35, no. 4 (1997): 675–94. http://dx.doi.org/10.1017/s0022278x97002577.

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The Nile flows for 6,700 kilometres through ten countries in north-eastern Africa – Rwanda, Burundi, Zaïre/Congo, Tanzania, Kenya, Uganda, Eritrea, Ethiopia, the Sudan, and Egypt – before reaching the Mediterranean, and is the longest international river system in the world – see Map 1. Its two main tributaries converge at Khartoum: the White Nile, which originates from Burundi and flows through the Equatorial Lakes, provides a small but steady flow that is fed by the eternal snows of the Ruwenzori (the ‘rain giver’) mountains, while the Blue Nile, which suffers from high seasonal fluctuations
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2

Mulat, Asegdew G., and Semu A. Moges. "The impacts of Upper Blue Nile Dams construction on agricultural water availability of Sudan." Water Practice and Technology 15, no. 2 (2020): 437–49. http://dx.doi.org/10.2166/wpt.2020.031.

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Abstract The objective of this research is assessing water resource availability in the Blue Nile River for different development scenarios using Mike Hydro modeling. The long term Blue Nile total irrigation water demand will be more than 46.67 × 109m3, which is nearly similar to the naturalized flow (around 48 × 109m3). In the phase II irrigation, water shortfalls increase to 0.38 × 109m3/year. There is up to 2.172 × 109m3/year irrigation water deficit at the full development level in Ethiopia. Due to flow regulation, there are no shortfalls in irrigation in Sudan in either the medium or the
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3

Treszkai, Ákos. "The River Nile Conflict in the Aspects of Critical Infrastructure Protection." Honvédségi Szemle 148, no. 1 (2020): 41–49. http://dx.doi.org/10.35926/hdr.2020.1.3.

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The aim of this paper is to present the River Nile conflict from the aspects of critical infrastructure protection. It is often stated that the next world war will be fought over water, and there are few regions as tense as the Nile Valley. Egypt and Ethiopia have a severe disagreement, Sudan is in the middle of it, and a big geopolitical shift is being played along the world’s longest river. The Grand Renaissance Dam has been un-der construction on the Blue Nile River in Ethiopia. This dam will be the greatest hydro-electric power plant in Africa. This critical infrastructure has both politic
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4

Li, Peng, Zhen He, Jianwu Cai, et al. "Identify the Impacts of the Grand Ethiopian Renaissance Dam on Watershed Sediment and Water Yields Dynamics." Sustainability 14, no. 13 (2022): 7590. http://dx.doi.org/10.3390/su14137590.

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The construction of large-scale water reservoir facilities in transboundary river basins always arouses intense concern and controversy. The Grand Ethiopian Renaissance Dam (GERD) under construction in Ethiopia is perceived to affect water security in Egypt and Sudan. Therefore, this study investigated the water and sediment balance of the Blue Nile River (BNR) basin and identified the spatio-temporal variation in sediment and water yields along with the construction of GERD using Integrated Valuation of Ecosystem Services and Tradeoffs (InVEST) sediment and water yield models. The BNR basin e
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Goor, Q., C. Halleux, Y. Mohamed, and A. Tilmant. "Optimal operation of a multipurpose multireservoir system in the Eastern Nile River Basin." Hydrology and Earth System Sciences Discussions 7, no. 4 (2010): 4331–69. http://dx.doi.org/10.5194/hessd-7-4331-2010.

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Abstract. The upper Blue Nile River Basin in Ethiopia is a largely untapped resource despite its huge potential for hydropower generation and irrigated agriculture. Controversies exist as to whether the numerous infrastructural development projects that are on the drawing board in Ethiopia will generate positive or negative externalities downstream in Sudan and Egypt. This study attempts at 1) examining the (re-)operation of infrastructures, in particular the proposed reservoirs in Ethiopia and the High Aswan Dam and 2) assessing the economic benefits and costs associated with the storage infr
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Goor, Q., C. Halleux, Y. Mohamed, and A. Tilmant. "Optimal operation of a multipurpose multireservoir system in the Eastern Nile River Basin." Hydrology and Earth System Sciences 14, no. 10 (2010): 1895–908. http://dx.doi.org/10.5194/hess-14-1895-2010.

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Abstract. The upper Blue Nile River Basin in Ethiopia is a largely untapped resource despite its huge potential for hydropower generation and irrigated agriculture. Controversies exist as to whether the numerous infrastructural development projects that are on the drawing board in Ethiopia will generate positive or negative externalities downstream in Sudan and Egypt. This study attempts at (1) examining the (re-)operation of infrastructures, in particular the proposed reservoirs in Ethiopia and the High Aswan Dam and (2) assessing the economic benefits and costs associated with the storage in
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King, Andrew, and Paul Block. "An assessment of reservoir filling policies for the Grand Ethiopian Renaissance Dam." Journal of Water and Climate Change 5, no. 2 (2014): 233–43. http://dx.doi.org/10.2166/wcc.2014.043.

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Africa's largest hydropower facility is currently under construction on the main stem of the Blue Nile River in Ethiopia. The Grand Ethiopian Renaissance Dam (GERD) is poised to facilitate regional development with a 63 billion cubic meter reservoir and 6,000 MW of power generating capacity. To date, however, no reservoir filling rate policy has been established. This policy will have clear implications on the GERD's ability to generate hydropower in the near-term and coincidentally impact people and livelihoods in Sudan and Egypt through reduced streamflow availability. Implications of climat
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8

Kansara, Prakrut, Wenzhao Li, Hesham El-Askary, et al. "An Assessment of the Filling Process of the Grand Ethiopian Renaissance Dam and Its Impact on the Downstream Countries." Remote Sensing 13, no. 4 (2021): 711. http://dx.doi.org/10.3390/rs13040711.

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The Grand Ethiopian Renaissance Dam (GERD), formerly known as the Millennium Dam, has been filling at a fast rate. This project has created issues for the Nile Basin countries of Egypt, Sudan, and Ethiopia. The filling of GERD has an impact on the Nile Basin hydrology and specifically the water storages (lakes/reservoirs) and flow downstream. In this study, through the analysis of multi-source satellite imagery, we study the filling of the GERD reservoir. The time-series generated using Sentinel-1 SAR imagery displays the number of classified water pixels in the dam from early June 2017 to Sep
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9

Betrie, G. D., Y. A. Mohamed, A. van Griensven, and R. Srinivasan. "Sediment management modelling in the Blue Nile Basin using SWAT model." Hydrology and Earth System Sciences 15, no. 3 (2011): 807–18. http://dx.doi.org/10.5194/hess-15-807-2011.

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Abstract. Soil erosion/sedimentation is an immense problem that has threatened water resources development in the Nile river basin, particularly in the Eastern Nile (Ethiopia, Sudan and Egypt). An insight into soil erosion/sedimentation mechanisms and mitigation methods plays an imperative role for the sustainable water resources development in the region. This paper presents daily sediment yield simulations in the Upper Blue Nile under different Best Management Practice (BMP) scenarios. Scenarios applied in this paper are (i) maintaining existing conditions, (ii) introducing filter strips, (i
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10

Tesfaye, Abonesh, and Roy Brouwer. "Exploring the scope for transboundary collaboration in the Blue Nile river basin: downstream willingness to pay for upstream land use changes to improve irrigation water supply." Environment and Development Economics 21, no. 2 (2015): 180–204. http://dx.doi.org/10.1017/s1355770x15000182.

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AbstractIn this study we model the preferences and willingness to pay (WTP) of downstream farmers in one of the largest irrigation schemes worldwide in Sudan for improved irrigation water supply through transboundary collaboration with farmers upstream in Ethiopia. In a choice experiment, Sudanese farmers are asked to pay an increase in existing irrigation fees to secure future irrigation water availability by either enhancing the removal of sediments in their local irrigation channels or compensating farmers in the Ethiopian highlands for taking soil conservation measures to prevent land degr
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11

Omer, A. Y. A., Y. S. A. Ali, J. A. Roelvink, A. Dastgheib, P. Paron, and A. Crosato. "Modelling of sedimentation processes inside Roseires Reservoir (Sudan)." Earth Surface Dynamics Discussions 2, no. 1 (2014): 153–79. http://dx.doi.org/10.5194/esurfd-2-153-2014.

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Abstract. Roseires Reservoir, located on the Blue Nile River, in Sudan, is the first trap to the sediments coming from the upper catchment in Ethiopia, which suffers from high erosion and desertification problems. The reservoir lost already more than one third of its storage capacity due to sedimentation in the last four decades. Appropriate management of the eroded area in the upper basin could mitigate this problem. In order to do that, the areas providing the highest sediment volumes to the river have to be identified, since they should have priority with respect to the application of erosi
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12

Omer, A. Y. A., Y. S. A. Ali, J. A. Roelvink, A. Dastgheib, P. Paron, and A. Crosato. "Modelling of sedimentation processes inside Roseires Reservoir (Sudan)." Earth Surface Dynamics 3, no. 2 (2015): 223–38. http://dx.doi.org/10.5194/esurf-3-223-2015.

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Abstract. Roseires Reservoir, located on the Blue Nile River in Sudan, is the first trap to the sediments coming from the vast upper river catchment in Ethiopia, which suffers from high erosion and desertification problems. The reservoir has already lost more than one-third of its storage capacity due to sedimentation in the last four decades. Appropriate management of the eroded soils in the upper basin could mitigate this problem. In order to do that, the areas providing the highest sediment volumes to the river have to be identified, since they should have priority with respect to the appli
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13

El Baradei, Sherine Ahmed, Ahmed Abodonya, Nahla Hazem, et al. "Ethiopian Dam Optimum Hydraulic Operating Conditions to Reduce Unfavorable Impacts on Downstream Countries." Civil Engineering Journal 8, no. 9 (2022): 1906–19. http://dx.doi.org/10.28991/cej-2022-08-09-011.

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As noted by several researchers, the Grand Ethiopian Renaissance Dam (GERD) on the Blue Nile River is expected to have unfavorable consequences for downstream countries like Egypt and Sudan. To limit GERD's negative effects on downstream countries, its operation should be secure, and its upstream water level should be ideal. However, none of the studies carried out the ideal operating scenarios from the perspective of controlling the number of gate openings. Accordingly, this study evaluates the optimal operating scenarios of the GERD and its impact on downstream countries by adopting a mathem
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14

Eldardiry, Hisham, and Faisal Hossain. "Understanding Reservoir Operating Rules in the Transboundary Nile River Basin Using Macroscale Hydrologic Modeling with Satellite Measurements." Journal of Hydrometeorology 20, no. 11 (2019): 2253–69. http://dx.doi.org/10.1175/jhm-d-19-0058.1.

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Abstract Challenges to manage and secure a sustainable water supply are expected to become more acute in Egypt as the lowermost riparian country of the Nile basin with the construction of new transboundary water infrastructures in Ethiopia and Sudan. To understand the impact of such transboundary water projects on Egypt, it is first necessary to develop a modeling tool that can simulate potential flow and reservoir scenarios inside Egypt without requiring in situ hydrologic or transboundary dam data that are typically unavailable. This study presents the water management value of a modeling fr
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15

Lorenz, Christof, Tanja C. Portele, Patrick Laux, and Harald Kunstmann. "Bias-corrected and spatially disaggregated seasonal forecasts: a long-term reference forecast product for the water sector in semi-arid regions." Earth System Science Data 13, no. 6 (2021): 2701–22. http://dx.doi.org/10.5194/essd-13-2701-2021.

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Abstract. Seasonal forecasts have the potential to substantially improve water management particularly in water-scarce regions. However, global seasonal forecasts are usually not directly applicable as they are provided at coarse spatial resolutions of at best 36 km and suffer from model biases and drifts. In this study, we therefore apply a bias-correction and spatial-disaggregation (BCSD) approach to seasonal precipitation, temperature and radiation forecasts of the latest long-range seasonal forecasting system SEAS5 of the European Centre for Medium-Range Weather Forecasts (ECMWF). As refer
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16

Baratti, E., A. Montanari, A. Castellarin, J. L. Salinas, A. Viglione, and A. Bezzi. "Estimating the flood frequency distribution at seasonal and annual time scales." Hydrology and Earth System Sciences 16, no. 12 (2012): 4651–60. http://dx.doi.org/10.5194/hess-16-4651-2012.

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Abstract. We propose an original approach to infer the flood frequency distribution at seasonal and annual time scale. Our purpose is to estimate the peak flow that is expected for an assigned return period T, independently of the season in which it occurs (i.e. annual flood frequency regime), as well as in different selected sub-yearly periods (i.e. seasonal flood frequency regime). While a huge literature exists on annual flood frequency analysis, few studies have focused on the estimation of seasonal flood frequencies despite the relevance of the issue, for instance when scheduling along th
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Baratti, E., A. Montanari, A. Castellarin, J. L. Salinas, A. Viglione, and A. Bezzi. "Estimating the flood frequency distribution at seasonal and annual time scale." Hydrology and Earth System Sciences Discussions 9, no. 6 (2012): 7947–67. http://dx.doi.org/10.5194/hessd-9-7947-2012.

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Abstract. We propose an original approach to infer the flood frequency distribution at seasonal and annual time scale. Our purpose is to estimate the peak flow that is expected for an assigned return period T, independently of the season in which it occurs (i.e. annual flood frequency regime), as well as in different selected sub-yearly periods (i.e. seasonal flood frequency regime). While a huge literature exists on annual flood frequency analysis, few studies have focused on the estimation of seasonal flood frequencies despite the relevance of the issue, for instance when scheduling along th
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18

Saad Omer, T. Z., S. E. Ahmed, and A. Karimi. "OPTIMAL OPERATION OF MULTIPURPOSE RESERVOIRS IN SERIES: ROSEIRES AND SENNAR CASE STUDY." Міжвідомчий тематичний науковий збірник "Меліорація і водне господарство", no. 2 (December 23, 2021): 5–23. http://dx.doi.org/10.31073/mivg202102-310.

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The Roseires-Sennar Dams System (RSDS) at lower part of Blue Nile River play a vital role in water supply to the irrigation schemes in Sudan. The existing rule curves for this system belong to 1925 and 1966 for Sennar and Roseires reservoirs, respectively. Introduction of new irrigation schemes, approved climate change impacts on Blue Nile River flow and upstream developments in Ethiopia as well as the heightening of the Roseires Dam from elevation 480 to 490 m.a.s.l have shown the RSDS is losing its efficiency in terms of fully supplying the water demands. The literature addresses the simulat
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19

Hassaballah, Khalid, Yasir Mohamed, Stefan Uhlenbrook, and Khalid Biro. "Analysis of streamflow response to land use and land cover changes using satellite data and hydrological modelling: case study of Dinder and Rahad tributaries of the Blue Nile (Ethiopia–Sudan)." Hydrology and Earth System Sciences 21, no. 10 (2017): 5217–42. http://dx.doi.org/10.5194/hess-21-5217-2017.

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Abstract. Understanding the land use and land cover changes (LULCCs) and their implication on surface hydrology of the Dinder and Rahad basins (D&R, approximately 77 504 km2) is vital for the management and utilization of water resources in the basins. Although there are many studies on LULCC in the Blue Nile Basin, specific studies on LULCC in the D&R are still missing. Hence, its impact on streamflow is unknown. The objective of this paper is to understand the LULCC in the Dinder and Rahad and its implications on streamflow response using satellite data and hydrological model
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E.H., Osman, Gumaa Y.S.A., and Elhag A.M.H. "Land Cover/Land Use Trends along the Blue Nile River Blue Nile State – Sudan." IRA-International Journal of Applied Sciences (ISSN 2455-4499) 13, no. 1 (2019): 1. http://dx.doi.org/10.21013/jas.v13.n1.p1.

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<p>The study focused on quantifying the extent and sources of the deterioration of the vegetation cover of the study area at the Sudanese Blue Nile watershed in relation to agriculture extension policy, inefficient management and Lack of governmental policy. </p><p>The Research was based on forest and vegetation inventory and soil analysis to determine the current situation using ground survey, forest inventory and remote sensing data as well as secondary information from other sources to cover historical records from 1990 to 2015.</p><p>The results showed a signi
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Herrer Fernández, Sara. "Water conflict analysis: The Nile River dispute." Análisis Jurídico - Político 4, no. 8 (2022): 83–112. http://dx.doi.org/10.22490/26655489.5877.

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The Nile River Basin is the source of life of Egypt, Ethiopia, Sudan, and Upstream countries, principally as water for agriculture and hydropower. The resource is the focus of much contested development between downstream and upstream countries. In recent years, largely due to climate change and rapid population growth, there has been an increasing level of conflict related to water scarcity and the consequent aggravation of food insecurity. Additionally, transboundary masses of water have an even more complex water management, becoming one of the main geopolitical issues of today. This confli
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Negasa Gelana Debisa. "The Utilization of Nile Water among the Riparian States: Tensions and Controversies on the Filling and Annual Operation of the GERD." PanAfrican Journal of Governance and Development (PJGD) 2, no. 1 (2021): 31–54. http://dx.doi.org/10.46404/panjogov.v2i1.2909.

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Despite the fear entertained by the downstream countries of the Nile basin, little attention was paid to the right of Ethiopia to utilize the Blue Nile waters. The purpose of this study is to explain the tension between upper riparian Ethiopia and downstream Sudan and Egypt on the Grand Ethiopian Renaissance Dam (GERD) filling and controversies on its annual operation. A descriptive qualitative research method was employed to describe the tension concerning the filling and controversies on the annual operation of the GERD. The investigation relied on secondary sources of data obtained from You
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Abu Sabah, Rasha Babiker Gurashi, Abubaker Haroun Mohamed Adam, and Dawoud Mohamed Ali. "Assessment of Water Quality of Blue Nile River in Sudan." Journal of Agronomy Research 1, no. 3 (2018): 1–14. http://dx.doi.org/10.14302/issn.2639-3166.jar-18-2457.

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The objectives of this study were to quantify the fresh water quality of Blue Nile River before processing, identify the pollutants, and to determine the most polluted areas, and their impacts on living organisms as well as the surrounding environment. Thus, random water samples were collected and analyzed at the laboratory of the Ministry of Irrigation and Water Resources, Ground water and Wadis Directorates - Khartoum. The outcomes were compared with the World Health Organization standardization. The results revealed variations in the concentration of the studied elements taken from the diff
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Johnson, Peggy A., and P. Douglas Curtis. "Water Balance of Blue Nile River Basin in Ethiopia." Journal of Irrigation and Drainage Engineering 120, no. 3 (1994): 573–90. http://dx.doi.org/10.1061/(asce)0733-9437(1994)120:3(573).

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Gelete, Gebre, Huseyin Gokcekus, and Tagesse Gichamo. "Impact of climate change on the hydrology of Blue Nile basin, Ethiopia: a review." Journal of Water and Climate Change 11, no. 4 (2019): 1539–50. http://dx.doi.org/10.2166/wcc.2019.014.

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Abstract Climate change alters the spacial and temporal availability of water resources by affecting the hydrologic cycle. The main objective of this paper is to review the climate change effect on the water resources of the Blue Nile River, Ethiopia. The impact of climate change on water resources is highly significant as all natural ecosystems and humans are heavily dependent on water. It alters precipitation, temperature, and streamflow of the Blue Nile river basin which is threatening the lives and livelihoods of people and life-supporting systems. Rainfall within the Blue Nile river basin
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YIMER, Nigusu Adem. "ETHIOPIA: THE CHANGING ASPECTS OF THE ETHIO-EGIPT WATER DIPLOMACY – KEY DRIVES, CHALLENGES AND PROSPECTS." Conflict Studies Quarterly, no. 41 (October 5, 2022): 78–96. http://dx.doi.org/10.24193/csq.41.5.

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Starting the inception of the 2010s, Ethiopia’s relations with Egypt have been experiencing one of the deepest crises in the relationship of the two countries’ history. Ethiopia, one of the upper riparian states of the Nile River not only theoretically challenged the exclusive veto power of Egypt over the Nile River but also practically start constructing one of Africa’s largest hydropower dams on the Blue Nile since 2011. The challenging behavior of Ethiopia over the Nile River worried the long-standing regional hegemon, Egypt. Against this background, this paper aims to forward a new insight
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Russo, Antonio, Getaneh Assefa, and Balemwal Atnafu. "Sedimentary evolution of the Abay River (Blue Nile) Basin, Ethiopia." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 1994, no. 5 (1994): 291–308. http://dx.doi.org/10.1127/njgpm/1994/1994/291.

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Mohieldeen, Yasir Elginiad. "More water flows from Western Sudan as virtual water than the flow of the River Nile in former Sudan." Water Policy 18, no. 3 (2015): 533–44. http://dx.doi.org/10.2166/wp.2015.130.

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This study argues that by mobilising ‘social resources’, communities in water-scarce, semi-arid areas can not only successfully sustain a livelihood, but they can also play an important role in the water budget of their semi-arid regions. The pastoralist communities in the Darfur region of west Sudan utilise the limited volumes of green – root-zone – water in the soil to rear livestock. They have for centuries developed and adopted a very adaptive management system that has enabled them to utilise the green water of the Nile Basin. The embedded green water in livestock totals more than Sudan's
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Garzanti, Eduardo, Sergio Andò, Giovanni Vezzoli, Ada Ali Abdel Megid, and Ahmed El Kammar. "Petrology of Nile River sands (Ethiopia and Sudan): Sediment budgets and erosion patterns." Earth and Planetary Science Letters 252, no. 3-4 (2006): 327–41. http://dx.doi.org/10.1016/j.epsl.2006.10.001.

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Muluneh, T., and W. Mamo. "Morphometric Analysis of Didessa River Catchment in Blue Nile Basin, Western Ethiopia." Science, Technology and Arts Research Journal 3, no. 3 (2014): 191. http://dx.doi.org/10.4314/star.v3i3.31.

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Saad, Magdi H. "The Distribution of the Heavy Metals in Soil Sample Along Blue Nile During overflow Season." Applied Physics Research 10, no. 1 (2017): 19. http://dx.doi.org/10.5539/apr.v10n1p19.

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The research cared out to calculate the heavy metals deposition for the soil of the Blue Nile along the edges of two sides, starting from the Sudan Ethiopia border end to the Khartoum state in Tuti Island. The samples were analyzed by inductively coupled plasma mass spectrometry (ICP-MS) technique. The results show that there is a significant difference for most of the concentration of the elements deposition on two sides of the Blue Nile outside of Nile channel for that area which covered by water after the overflow. Heavy metals Cr, Fe, Co, Cu, and Zn concentration deposition are increased i
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Mehari, Abrehet Kahsay, Shewit Gebremedhin, and Belayneh Ayele. "Effects of Bahir Dar Textile Factory Effluents on the Water Quality of the Head Waters of Blue Nile River, Ethiopia." International Journal of Analytical Chemistry 2015 (2015): 1–7. http://dx.doi.org/10.1155/2015/905247.

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The study was conducted in 2013/14 with the objective of determining the effects of Bahir Dar textile factory effluents on the head of Blue Nile River water quality. Dissolve oxygen was higher at the upstream site of the river, whereas BOD5, TDS, and total alkalinity values were higher at wastewater outlet of the factory site. The mean values of dissolved oxygen, BOD5, and total alkalinity were above maximum permissible limits set by WHO for drinking water at head of Blue Nile River. The mean value of BOD5 was above permissible limit of IFC for textile effluents to be discharged to surface wat
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Kwesi Kyirewiah, Francis. "Water Diplomacy: And the Share of the Nile River between Egypt, Ethiopia and Sudan." Mediterranean Journal of Social Sciences 13, no. 1 (2022): 32. http://dx.doi.org/10.36941/mjss-2022-0004.

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Water diplomacy across international borders can be a useful tool in solving problems related to the shared water resources of the political entities involved, especially when the interests of the countries are diverse. Water disputes can likely lead to potential conflicts if not properly address in a holistic manner to satisfy all parties concerned. Many discussions about water resources that cut across international borders have focused on their potential for either conflict or cooperation. Africa as a continent with shared resources is not isolated from these enormous challenges concerning
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Yimere, Abay, and Engdawork Assefa. "Assessment of the Water-Energy Nexus under Future Climate Change in the Nile River Basin." Climate 9, no. 5 (2021): 84. http://dx.doi.org/10.3390/cli9050084.

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This study investigated the Water-Energy relationship in the Nile River Basin under changing climate conditions using an energy and water model. Climate change will likely affect both water and energy resources, which will create challenges for future planning and decision making, particularly considering the uncertainty surrounding the direction and magnitude of such effects. According to the assessment model, when countries depend heavily on hydropower for energy, power generation is determined by climate variability. For example, Ethiopia, Egypt, and Sudan are more hydropower-dependent than
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Mekkonen Bekele, Teferi. "A Decade of Regional Confrontation over the Nile Waters." Archiv orientální 84, no. 1 (2016): 23–50. http://dx.doi.org/10.47979/aror.j.84.1.23-50.

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This article examines how unilateral actions hindered the imperative for cooperation between Ethiopia, Egypt and the Sudan over the use of the waters of the Nile River. It focuses on the remarkable strategic shift away from the idea of comprehensive Basinwide hydraulic projects – that would have benefited all the states and hence would have brought about cooperation in the Nile Valley – to Egypt’s unilateral decision to erect the High Dam at Aswan in the early 1950s. It examines in detail Ethiopia’s counter response to the Aswan High Dam Project and the subsequent Egypt-Sudanese bilateral nego
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Tesfaye, Gizaw. "Soil Erosion and Sedimentation Rate in the Blue Nile River Basin of Ethiopia." American Journal of Environmental Protection 11, no. 1 (2022): 1. http://dx.doi.org/10.11648/j.ajep.20221101.11.

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Elzeiny, Radwa, Mossad Khadr, Shreen Zahran, and Ebrahim Rashwan. "Homogeneity Analysis of Rainfall Series in the Upper Blue Nile River Basin, Ethiopia." Journal of Engineering Research 3, no. 9 (2019): 46–53. http://dx.doi.org/10.21608/erjeng.2019.125704.

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Bokke, Andualem Shigute, Meron Teferi Taye, Patrick Willems, and Shimelis Asefu Siyoum. "Validation of General Climate Models (GCMs) over Upper Blue Nile River Basin, Ethiopia." Atmospheric and Climate Sciences 07, no. 01 (2017): 65–75. http://dx.doi.org/10.4236/acs.2017.71006.

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Tegegne, Getachew, Assefa M. Melesse, Dereje H. Asfaw, and Abeyou W. Worqlul. "Flood Frequency Analyses over Different Basin Scales in the Blue Nile River Basin, Ethiopia." Hydrology 7, no. 3 (2020): 44. http://dx.doi.org/10.3390/hydrology7030044.

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The frequency and intensity of flood quantiles and its attendant damage in agricultural establishments have generated a lot of issues in Ethiopia. Moreover, precise estimates of flood quantiles are needed for efficient design of hydraulic structures; however, quantification of these quantiles in data-scarce regions has been a continuing challenge in hydrologic design. Flood frequency analysis is thus essential to reduce possible flood damage by investigating the most suitable flood prediction model. The annual maximum discharges from six representative stations in the Upper Blue Nile River Bas
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Betrie, G. D., Y. A. Mohamed, A. van Griensven, R. Srinivasan, and A. Mynett. "Sediment management modelling in Blue Nile Basin using SWAT model." Hydrology and Earth System Sciences Discussions 7, no. 4 (2010): 5497–524. http://dx.doi.org/10.5194/hessd-7-5497-2010.

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Abstract. Soil erosion/sedimentation is a colossal problem that has menaced water resources development in the Nile, particularly in Eastern Nile (Ethiopia, Sudan and Egypt). An insight into soil erosion/sedimentation mechanism and mitigation methods plays an indispensable role for the sustainable water resources development in the region. This paper presents a daily sediment yield simulation in the Upper Blue Nile under different Best Management Practices (BMPs) scenarios. The scenarios were baseline (existing condition), Buffer strips, stone bund (parallel terrace), and reforestation. The So
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Williams, Martin A. J. "A river flowing through a desert: late Quaternary environments in the Nile basin – current understanding and unresolved questions." Journal of Palaeosciences 70, no. (1-2) (2021): 267–88. http://dx.doi.org/10.54991/jop.2021.22.

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Late Quaternary environments in the Nile Basin reflect the influence of the African summer monsoon upon plant cover, sediment yield and flood discharge in the Ethiopian and Ugandan headwaters of the Nile. Intervals of prolonged and very high Nile flow coincide with times of stronger summer monsoon and have been dated using a combination of 14C, OSL and 10Be methods. Periods of high Nile flow into the eastern Mediterranean coincide with the formation of highly organic sedimentary layers termed sapropels. Ages obtained so far for these times of sustained middle to late Pleistocene high flow in t
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Eldaw, Elsiddig, Tao Huang, Adam Khalifa Mohammed, and Yahaya Muhama. "Stochastic Time series analysis of Runoff data of the Blue Nile at Eldeim, Sudan." E3S Web of Conferences 81 (2019): 01005. http://dx.doi.org/10.1051/e3sconf/20198101005.

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To improve the management of operation system for the Roseires reservoir it is necessary to know the hydrological system of the Blue Nile river, which is the main water source of the reservoir. In this work, a Modified Thomas Fiering model for generating and forecasting monthly flow is used. The methodological procedure is applied on the data obtained at the gauging station of Eldeim in Blue Nile, Sudan. The study uses the monthly flows data for years 1965 to 2009. After estimation the model parameters, the synthetic time series of monthly flows are simulated. The results revealed that the mod
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Bombelli, Giovanni, Stefano Tomiet, Alberto Bianchi, and Daniele Bocchiola. "Impact of Prospective Climate Change Scenarios upon Hydropower Potential of Ethiopia in GERD and GIBE Dams." Water 13, no. 5 (2021): 716. http://dx.doi.org/10.3390/w13050716.

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Ethiopia is growing fast, and the country has a dire need of energy. To avoid environmental damages, however, Ethiopia is looking for green energy polices, including hydropower exploitation, with large water availability (i.e., the Blue Nile, the greatest tributary of Nile river). Besides other dams on the Omo river, the GIBE family, Ethiopia is now building the largest hydropower plant of Africa, the GERD (Grand Ethiopian Renaissance Dam), on the Blue Nile river, leading to tensions between Ethiopia, and Egypt, due to potentially conflictive water management. In addition, present and prospect
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Abate, Mengiste, Jan Nyssen, Tammo S. Steenhuis, et al. "Morphological changes of Gumara River channel over 50 years, upper Blue Nile basin, Ethiopia." Journal of Hydrology 525 (June 2015): 152–64. http://dx.doi.org/10.1016/j.jhydrol.2015.03.044.

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Yoon, Sungsuk, and Goytom Afera Gebrekiros. "Tripartite Conflicts Between Egypt, Sudan, and Ethiopia over the Nile River: A Search for Political Avenue." Journal of Humanities and Social sciences 21 12, no. 1 (2021): 675–90. http://dx.doi.org/10.22143/hss21.12.1.47.

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A.M.H., Elhag, Gumaa Y.S.A., and Osman E.H. "Monitoring, Predicting and Quantifying Soil Alkalinity, Sodicity and Salinity in Blue Nile State, Sudan, Using Soil Techniques, Remote Sensing and GIS Analysis; Case Study: Blue Nile River." IRA-International Journal of Applied Sciences (ISSN 2455-4499) 11, no. 3 (2018): 37. http://dx.doi.org/10.21013/jas.v11.n3.p2.

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<p>This study focused on the assessment of land degradation on a transect of 20 km along the Blue Nile River (10 km at each side of the river) within the Blue Nile state, Blue Nile State, Sudan. Through mapping and monitoring the changes that occurred in the soil properties, due to Water Erosion, Vegetations degradation, mismanagement in addition to the Human activities and Climatic change The study attempted also to update some information in the study area such as chemical properties using different methods of data transformation and analysis such as: Soil analysis technique, GIS and r
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Hassaballah, Khalid, Yasir A. Mohamed, and Stefan Uhlenbrook. "The long-term trends in hydro-climatology of the Dinder and Rahad basins, Blue Nile, Ethiopia/Sudan." International Journal of Hydrology Science and Technology 9, no. 6 (2019): 690. http://dx.doi.org/10.1504/ijhst.2019.10025127.

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Hassaballah, Khalid, Yasir A. Mohamed, and Stefan Uhlenbrook. "The long-term trends in hydro-climatology of the Dinder and Rahad basins, Blue Nile, Ethiopia/Sudan." International Journal of Hydrology Science and Technology 9, no. 6 (2019): 690. http://dx.doi.org/10.1504/ijhst.2019.103447.

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Haile, A. T., T. H. M. Rientjes, E. Habib, V. Jetten, and M. Gebremichael. "Rain event properties at the source of the Blue Nile River." Hydrology and Earth System Sciences 15, no. 3 (2011): 1023–34. http://dx.doi.org/10.5194/hess-15-1023-2011.

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Abstract. In the present study, spatial and temporal patterns of rain event properties are analysed. These event properties are rain event depth, event duration, mean event rain rate, peak rain rate and the time span between two consecutive rain events which is referred to as inter-event time (IET). In addition, we assessed how rain event properties change when the period over which rainfall data is aggregated changes from 1 to 6 min and when the minimum inter-event time (MIT) changes from 30 min to 8 h. Rainfall data is obtained from a field campaign in two wet seasons of June–August (JJA) of
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Haile, Mesfin Mamo. "Bivariate Flood Frequency Analysis: A case study of Rib River, Upper Blue Nile Basin, Ethiopia." ARRUS Journal of Engineering and Technology 2, no. 2 (2022): 46–64. http://dx.doi.org/10.35877/jetech489.

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Hydrological design, planning and design of flood mitigation structures require detailed knowledge of the characteristics of the flood event, i.e. peaks, volumes, occurrence times and duration. In addition to the uncertainty associated with the occurrence in both space and time, these events may often have a correlation of varying strengths. The literature study interestingly reveals that the majority of studies are based on a univariate approach rather than a more realistic approach that recognizes the multivariate nature of the underlying phenomenology. Therefore, the main objective of this
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