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Journal articles on the topic 'The Niger river basin'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

Okoli, Chucks. "The Hydrometeorology of Niger River Basin." Advanced Materials Research 824 (September 2013): 613–29. http://dx.doi.org/10.4028/www.scientific.net/amr.824.613.

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This paper examines the mean annual cycle of rainfall and general circulation features over the Niger River Basin consisting of mainly West Africa and Central Africa regions. Rainfall is examined using a 1400-station archive compiled by earlier workers. Other circulation features are examined using the NCEPNCAR reanalysis dataset. Important features of the reanalysis zonal wind field are shown to compare well with the seasonal evolution described by the radiosonde observations. In addition to the well-known African easterly jet (AEJ) of the Northern Hemisphere, the seasonal evolution of its So

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2

Sorí, Rogert, Raquel Nieto, Anita Drumond, and Luis Gimeno. "The Niger River Basin Moisture Sources: A Lagrangian Analysis." Atmosphere 8, no. 12 (2017): 38. http://dx.doi.org/10.3390/atmos8020038.

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3

Ogilvie, Andrew, Gil Mahé, John Ward, et al. "Water, agriculture and poverty in the Niger River basin." Water International 35, no. 5 (2010): 594–622. http://dx.doi.org/10.1080/02508060.2010.515545.

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4

Andersson, Jafet C. M., Abdou Ali, Berit Arheimer, David Gustafsson, and Bernard Minoungou. "Providing peak river flow statistics and forecasting in the Niger River basin." Physics and Chemistry of the Earth, Parts A/B/C 100 (August 2017): 3–12. http://dx.doi.org/10.1016/j.pce.2017.02.010.

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5

Akana, Tombra, and Olubunmi Adeigbe. "Channel characteristics and planform dynamics of the lower Niger River, Niger Delta Basin (1985–2015)." Geology, Geophysics and Environment 45, no. 4 (2020): 291. http://dx.doi.org/10.7494/geol.2019.45.4.291.

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This study used repeat satellite imagery and Geographic Information System analysis to assess the plan-form dynamics along the length of the lower Niger River Valley from Onitsha city to the coast between 1985 and 2015. The aim is to understand the altered dynamics and its plausible causes in this data-poor region. Analyses revealed that the Niger River has undergone change corresponding to enhanced instability in terms of an increased rate of erosion. In the study area, a change was observed from 3.7% of deposition in the first 10 years (1985–1995) to 3.9% of erosion in the next 10 years (199

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6

Aich, Valentin, Bakary Koné, Fred Hattermann, and Eva Paton. "Time Series Analysis of Floods across the Niger River Basin." Water 8, no. 4 (2016): 165. http://dx.doi.org/10.3390/w8040165.

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7

Landis, Steven T., Babak Rezaeedaryakenari, Yifan Zhang, Cameron G. Thies, and Ross Maciejewski. "Fording differences? Conditions mitigating water insecurity in the Niger River Basin." Political Geography 56 (January 2017): 77–90. http://dx.doi.org/10.1016/j.polgeo.2016.10.002.

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8

Werth, S., D. White, and D. W. Bliss. "GRACE Detected Rise of Groundwater in the Sahelian Niger River Basin." Journal of Geophysical Research: Solid Earth 122, no. 12 (2017): 10,459–10,477. http://dx.doi.org/10.1002/2017jb014845.

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9

Sorí, Rogert, Raquel Nieto, Anita Drumond, Milica Stojanovic, and Luis Gimeno. "On the Connection between Atmospheric Moisture Transport and Dry Conditions in Rainfall Climatological Zones of the Niger River Basin." Water 11, no. 3 (2019): 622. http://dx.doi.org/10.3390/w11030622.

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The hydroclimatology of the Niger River basin, located in West Africa, is very complex. It has been widely studied because of its importance to the socioeconomic activities of the countries that share its natural resources. In this study, to better understand the causes and mechanisms that modulate the rainfall over the Niger River basin, we identified the most relevant moisture sources for precipitation within the basin. The Lagrangian model FLEXPART was utilised to track backward trajectories of air parcels initially losing humidity over climatological rainfall zones of the basin. Along 10-d

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10

Eme, L. C., J. A. Ulasi, A. I. Alade Tunde, and A. C. Odunze. "Hydrokinetic turbines for power generation in Nigerian river basins." Water Practice and Technology 14, no. 1 (2019): 71–80. http://dx.doi.org/10.2166/wpt.2019.001.

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Abstract This work presents a design for Hydrokinetic Renewable Energy (HRE), for off grid power generation for remote riverine regions in developing nations. The uniqueness of this technique for power generation using streams and other marine currents to generate electric energy is detailed. The problem of the impact of greenhouse gas emissions on the environment, rapid increase in human population, industries, modernization and our lifestyle put immense pressure on most power generation plants and infrastructures. Thus, global warming and carbon footprints of using fossil fuels to generate e

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11

Massazza, Giovanni, Maurizio Bacci, Luc Descroix, et al. "Recent Changes in Hydroclimatic Patterns over Medium Niger River Basins at the Origin of the 2020 Flood in Niamey (Niger)." Water 13, no. 12 (2021): 1659. http://dx.doi.org/10.3390/w13121659.

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Niamey, the capital of Niger, is particularly prone to floods, since it is on the banks of the Niger River, which in its middle basin has two flood peaks: one in summer (the red flood) and one in winter (the black flood). In 2020, the Niger River in Niamey reached its all-time highest levels following an abundant rainy season. On the other hand, the floods in Niamey have been particularly frequent in the last decade, a symptom of a change in hydroclimatic behaviour already observed since the end of the great droughts of the 1970s and 1980s and which is identified with the name of Sahelian Para

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12

Bâ, Khalidou, Luis Balcázar, Vitali Diaz, Febe Ortiz, Miguel Gómez-Albores, and Carlos Díaz-Delgado. "Hydrological Evaluation of PERSIANN-CDR Rainfall over Upper Senegal River and Bani River Basins." Remote Sensing 10, no. 12 (2018): 1884. http://dx.doi.org/10.3390/rs10121884.

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This study highlights the advantage of satellite-derived rainfall products for hydrological modeling in regions of insufficient ground observations such as West African basins. Rainfall is the main input for hydrological models; however, gauge data are scarce or difficult to obtain. Fortunately, several precipitation products are available. In this study, Precipitation Estimation from Remotely Sensed Information using Artificial Neural Networks–Climate Data Record (PERSIANN-CDR) was analyzed. Daily discharges of three rivers of the Upper Senegal basin and one of the Upper Niger basin, as well

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13

Ologhadien, Itolima. "Developments in river bank protection schemes in the lower Niger delta basin." MOJ Civil Engineering 5, no. 2 (2019): 58–67. http://dx.doi.org/10.15406/mojce.2019.05.00150.

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14

Babatolu, Joseph Sunday, and Rufus Temidayo Akinnubi. "Surface Temperature Anomalies in the River Niger Basin Development Authority Areas, Nigeria." Atmospheric and Climate Sciences 03, no. 04 (2013): 532–37. http://dx.doi.org/10.4236/acs.2013.34056.

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15

Akumaga, Uvirkaa, and Aondover Tarhule. "Projected Changes in Intra-Season Rainfall Characteristics in the Niger River Basin, West Africa." Atmosphere 9, no. 12 (2018): 497. http://dx.doi.org/10.3390/atmos9120497.

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The magnitude and timing of seasonal rainfall is vitally important to the health and vitality of key agro-ecological and social-economic systems of the Niger River Basin. Given this unique context, knowledge concerning how climate change is likely to impact future rainfall characteristics and patterns is critically needed for adaptation and mitigation planning. Using nine ensemble bias-corrected climate model projection results under RCP4.5 and RCP8.5 (RCP—Representative Concentration Pathway) emissions scenarios at the mid-future time period, 2021/2025-2050 from the Coordinated Regional Clima

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16

Pedinotti, V., A. Boone, B. Decharme, et al. "Characterization of the hydrological functioning of the Niger basin using the ISBA-TRIP model." Hydrology and Earth System Sciences Discussions 8, no. 5 (2011): 9173–227. http://dx.doi.org/10.5194/hessd-8-9173-2011.

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Abstract. During the 70s and 80s, West Africa has faced extreme climate variations with extended extreme drought conditions. Of particular importance is the Niger basin, since it traverses a large part of the Sahel and is thus a critical source of water in this semi arid region. However, the understanding of the hydrological processes over this basin is currently limited by the lack of spatially distributed surface water and discharge measurements. The purpose of this study is to use the ISBA-TRIP continental hydrologic system to explore key processes related to the hydrological cycle of the N

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17

Uzoegbu, M. U. "Evidence of terrestrial organic carbon inputs on Niger Delta Sea Shelf." Scientia Africana 19, no. 3 (2021): 83–100. http://dx.doi.org/10.4314/sa.v19i3.7.

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The objective of this research is to determine the actual source of organic matter in the Niger Delta Sea Shelf (NDSS). Organic carbon (OC) and n-alkanes were investigated in the suspended matter (SM) and surfcial sediments of the Niger and Imo Rivers and the opposite Niger Delta Sea Shelf. Organic nitrogen and carbon isotope (δ13C) values were determined as additional parameters in the sediments. OC and n-alkane concentrations were highly variable. This variability was interpreted as the result of sources of materials from the inland basins and a complex sedimentation pattern involving the di

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18

Pandey, R., and G. Amarnath. "The potential of satellite radar altimetry in flood forecasting: concept and implementation for the Niger-Benue river basin." Proceedings of the International Association of Hydrological Sciences 370 (June 11, 2015): 223–27. http://dx.doi.org/10.5194/piahs-370-223-2015.

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Abstract. Flood forecasting in the downstream part of any hydrological basin is extremely difficult due to the lack of basin-wide hydrological information in near real-time and the absence of a data-sharing treaty among the transboundary nations. The accuracy of forecasts emerging from a hydrological model could be compromised without prior knowledge of the day-to-day flow regulation at different locations upstream of the Niger and Benue rivers. Only satellite altimeter monitoring allows us to identify the actual river levels upstream that reflect the human intervention at that location. This

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19

B, Alhou, Issiaka Boukari, and Darchambeau F. "Apports En Carbone Et Azote Dans Le Fleuve Niger À Tondibia (Niamey) : Résultats De Deux (2) Ans D’observations." European Scientific Journal, ESJ 12, no. 21 (2016): 167. http://dx.doi.org/10.19044/esj.2016.v12n21p167.

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The Niger River is the third more important river in Africa and drains a surface of about 2,120,000 km². It includes six hydrographic regions representing West African ecosystems. Despite the importance of this river at the regional and continental scale, little information has been collected on its biogeochemical characteristics and particularly on its role in the transportation and the transformation of matter (carbon, nitrogen and phosphorus). This study present the results of two years investigation, April 2011 to March 2013 in the middle Niger, upstream Niamey (Niger) city [2.01° E, 13.57

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20

Vetter, T., S. Huang, V. Aich, et al. "Multi-model climate impact assessment and intercomparison for three large-scale river basins on three continents." Earth System Dynamics Discussions 5, no. 2 (2014): 849–900. http://dx.doi.org/10.5194/esdd-5-849-2014.

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Abstract. Climate change impacts on hydrological processes should be simulated for river basins using validated models and multiple climate scenarios in order to provide reliable results for stakeholders. In the last 10–15 years climate impact assessment was performed for many river basins worldwide using different climate scenarios and models. Nevertheless, the results are hardly comparable and do not allow to create a full picture of impacts and uncertainties. Therefore, a systematic intercomparison of impacts is suggested, which should be done for representative regions using state-of-the-a

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21

Andersson, Jafet C. M., Berit Arheimer, Farid Traoré, David Gustafsson, and Abdou Ali. "Process refinements improve a hydrological model concept applied to the Niger River basin." Hydrological Processes 31, no. 25 (2017): 4540–54. http://dx.doi.org/10.1002/hyp.11376.

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22

Munier, S., A. Polebistki, C. Brown, G. Belaud, and D. P. Lettenmaier. "SWOT data assimilation for operational reservoir management on the upper Niger River Basin." Water Resources Research 51, no. 1 (2015): 554–75. http://dx.doi.org/10.1002/2014wr016157.

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23

Oguntunde, Philip G., and Babatunde J. Abiodun. "The impact of climate change on the Niger River Basin hydroclimatology, West Africa." Climate Dynamics 40, no. 1-2 (2012): 81–94. http://dx.doi.org/10.1007/s00382-012-1498-6.

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24

Béné, Christophe, Louisa Evans, David Mills, et al. "Testing resilience thinking in a poverty context: Experience from the Niger River basin." Global Environmental Change 21, no. 4 (2011): 1173–84. http://dx.doi.org/10.1016/j.gloenvcha.2011.07.002.

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25

Ghile, Y. B., M. Ü. Taner, C. Brown, J. G. Grijsen, and Amal Talbi. "Bottom-up climate risk assessment of infrastructure investment in the Niger River Basin." Climatic Change 122, no. 1-2 (2013): 97–110. http://dx.doi.org/10.1007/s10584-013-1008-9.

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26

Picouet, Cécile, Benoît Hingray, and Jean Claude Olivry. "Modelling the suspended sediment dynamics of a large tropical river: the Upper Niger river basin at Banankoro." Hydrological Processes 23, no. 22 (2009): 3193–200. http://dx.doi.org/10.1002/hyp.7398.

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27

Salami, Adebayo Wahab, Oseni Taiwo Amoo, Joshiah Adetayo Adeyemo, Abdulrasaq Apalando Mohammed, and Adeniyi Ganiyu Adeogun. "Morphometrical Analysis and Peak Runoff Estimation for the Sub-Lower Niger River Basin, Nigeria." Slovak Journal of Civil Engineering 24, no. 1 (2016): 6–16. http://dx.doi.org/10.1515/sjce-2016-0002.

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AbstractThis study utilized Spatial Information Technology (SIT) such as Remote Sensing (RS), a Geographical Information System (GIS), the Global Positioning System (GPS) and a high-resolution Digital Elevation Model (DEM) for a morphometrical analysis of five sub-basins within the Lower Niger River Basin, Nigeria. Morpho-metrical parameters, such as the total relief, relative relief, relief ratio, ruggedness number, texture ratio, elongation ratio, circularity ratio, form factor ratio, drainage density, stream frequency, sinuosity factor and bifurcation ratio, have been computed and analyzed.

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28

Scarcelli, Nora, Philippe Cubry, Roland Akakpo, et al. "Yam genomics supports West Africa as a major cradle of crop domestication." Science Advances 5, no. 5 (2019): eaaw1947. http://dx.doi.org/10.1126/sciadv.aaw1947.

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While there has been progress in our understanding of the origin and history of agriculture in sub-Saharan Africa, a unified perspective is still lacking on where and how major crops were domesticated in the region. Here, we investigated the domestication of African yam (Dioscorea rotundata), a key crop in early African agriculture. Using whole-genome resequencing and statistical models, we show that cultivated yam was domesticated from a forest species. We infer that the expansion of African yam agriculture started in the Niger River basin. This result, alongside with the origins of African r

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29

Vetter, T., S. Huang, V. Aich, et al. "Multi-model climate impact assessment and intercomparison for three large-scale river basins on three continents." Earth System Dynamics 6, no. 1 (2015): 17–43. http://dx.doi.org/10.5194/esd-6-17-2015.

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Abstract. Climate change impacts on hydrological processes should be simulated for river basins using validated models and multiple climate scenarios in order to provide reliable results for stakeholders. In the last 10–15 years, climate impact assessment has been performed for many river basins worldwide using different climate scenarios and models. However, their results are hardly comparable, and do not allow one to create a full picture of impacts and uncertainties. Therefore, a systematic intercomparison of impacts is suggested, which should be done for representative regions using state-

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30

Modu, B., and B. Herbert. "Spatial analysis from remotely sensed observations of Congo basin of East African high Land to drain water using gravity for sustainable management of low laying Chad basin of Central Africa." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XL-1 (November 7, 2014): 279–86. http://dx.doi.org/10.5194/isprsarchives-xl-1-279-2014.

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The Chad basin which covers an area of about 2.4 million kilometer square is one of the largest drainage basins in Africa in the centre of Lake Chad .This basin was formed as a result of rifting and drifting episode, as such it has no outlet to the oceans or seas. It contains large area of desert from the north to the west. The basin covers in part seven countries such as Chad, Nigeria, Central African Republic, Cameroun, Niger, Sudan and Algeria. It is named Chad basin because 43.9% falls in Chad republic. Since its formation, the basin continues to experienced water shortage due to the activ

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31

Oyerinde, Ganiyu Titilope, Agnide E. Lawin, and Oluwafemi E. Adeyeri. "Multi-variate infilling of missing daily discharge data on the Niger basin." Water Practice and Technology 16, no. 3 (2021): 961–79. http://dx.doi.org/10.2166/wpt.2021.048.

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Abstract The Niger basin has experienced historical drought episodes and floods in recent times. Reliable hydrological modelling has been hampered by missing values in daily river discharge data. We assessed the potential of using the Multivariate Imputation by Chained Equations (MICE) to estimate both continuous and discontinuous daily missing data across different spatial scales in the Niger basin. The study was conducted on 22 discharge stations that have missing data ranging from 2% to 70%. Four efficiency metrics were used to determine the effectiveness of MICE. The flow duration curves (

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32

Bader, Jean-Claude, Honoré Dacosta, and Jean-Christophe Pouget. "Seasonal Variations of the Depletion Factor during Recession Periods in the Senegal, Gambia and Niger Watersheds." Water 12, no. 9 (2020): 2520. http://dx.doi.org/10.3390/w12092520.

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The daily depletion factor K describes the discharge decrease of rivers only fed by groundwater in the absence of rainfall. In the Senegal, Gambia and Niger river basins in West Africa, the flow recession can exceed 6 months and the precise knowledge of K thus allows discharge forecasts to be made over several months, and is hence potentially interesting for hydraulic structure managers. Seasonal flow recession observed at 54 gauging stations in these basins from 1950 to 2016 is represented by empirical and usual conceptual models that express K. Compared to conventional conceptual models, an

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33

Abdoulaye, Abdoulaye Oumarou, Haishen Lu, Yonghua Zhu, and Yousef Alhaj Hamoud. "Future Irrigation Water Requirements of the Main Crops Cultivated in the Niger River Basin." Atmosphere 12, no. 4 (2021): 439. http://dx.doi.org/10.3390/atmos12040439.

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Precise agricultural predictions of climate change effects on crop water productivity are essential to ensure food security and alleviate water scarcity. In this regard, the present study provides an overview of the future impacts of climate change on the irrigation of agricultural products such as rice, millet, maize, cassava, sorghum, and sugar cane. These crops are some of the most-consumed foodstuffs in countries of the Niger River basin. This study is realized throughout 2020 to 2080, and three Global Climate Models (GCMs) (CSIRO, MIROC5, and ECHAM. MPI-ESM-LR) have been used. The GCMs da

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34

Moruff, Adelakun Kehinde, Mu’azu Mohammed Mu’azu, Amali Rosemary Patric, and Omotayo Olabode Lawrence. "Diversity of Phytoplankton Communities in a Tropical River Basin, Nigeria." Hydro Nepal: Journal of Water, Energy and Environment 19 (July 26, 2016): 52–56. http://dx.doi.org/10.3126/hn.v19i0.15353.

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Biological assessment is a useful alternative for understanding the ecological quality of aquatic ecosystems because biological communities integrate the environmental effects of water. This work investigates the diversity and abundance of phytoplankton in the Upper Jebba Basin of the Niger River in Nigeria. We sampled phytoplanktons by dragging plankton nets at three stations from March to May 2015 for qualitative and quantitative samples. Qualitative plankton samples were collected by towing 55μm mesh hydrobios plankton nets just below the water surface for five minutes at each sampling stat

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35

Oguntunde, Philip G., Babatunde J. Abiodun, and Gunnar Lischeid. "A numerical modelling study of the hydroclimatology of the Niger River Basin, West Africa." Hydrological Sciences Journal 61, no. 1 (2015): 94–106. http://dx.doi.org/10.1080/02626667.2014.980260.

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36

Aich, Valentin, Stefan Liersch, Tobias Vetter, et al. "Flood projections within the Niger River Basin under future land use and climate change." Science of The Total Environment 562 (August 2016): 666–77. http://dx.doi.org/10.1016/j.scitotenv.2016.04.021.

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37

Stohl, Andreas, and Paul James. "A Lagrangian Analysis of the Atmospheric Branch of the Global Water Cycle. Part II: Moisture Transports between Earth’s Ocean Basins and River Catchments." Journal of Hydrometeorology 6, no. 6 (2005): 961–84. http://dx.doi.org/10.1175/jhm470.1.

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Abstract A diagnostic Lagrangian method to trace the budgets of freshwater fluxes, first described in Part I of this article, is used here to establish source–sink relationships of moisture between earth’s ocean basins and river catchments. Using the Lagrangian particle dispersion model FLEXPART, driven with meteorological analyses, 1.1 million particles, representing the mass of the atmosphere, were tracked over a period of 4 yr. Via diagnosis of the changes of specific humidity along the trajectories, budgets of evaporation minus precipitation (E − P) were determined. For validation purposes

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38

Ladokun, LL, KR Ajao, and BF Sule. "Regional Scale Assessment of the Gross Hydrokinetic Energy Potentials of Some Rivers in Lower Niger River Basin, Nigeria." Nigerian Journal of Technology 34, no. 2 (2015): 421. http://dx.doi.org/10.4314/njt.v34i2.29.

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39

Abiodun, Ajiboye, A. O. Adekunmi, and O. A. Adeleke A. O. Awoyemi. "Impact of Land Right Arrangements on the use of Irrigation Resources in the Lower Niger River Basin Development Authority of Nigeria." International Journal of Trend in Scientific Research and Development Volume-3, Issue-3 (2019): 637–41. http://dx.doi.org/10.31142/ijtsrd22927.

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40

Morrison, Brian P., and Daniel J. Moore. "First Occurrence of a Juvenile Chain Pickerel (Esox niger) in Ontario Waters of Lake Ontario." Canadian Field-Naturalist 131, no. 4 (2018): 331–34. http://dx.doi.org/10.22621/cfn.v131i4.1946.

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This paper documents the first juvenile Chain Pickerel (Esox niger) captured in Ontario waters of Lake Ontario. It was found during August 2016 monitoring activities at Port of Newcastle. Its occurrence represents a significant westward range expansion from recently documented adults in the eastern basin of Lake Ontario/Bay of Quinte/St. Lawrence River, likely colonizing from United States waters of Lake Ontario.

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41

Silva, AMO, M. Tavares-Dias, GT Jerônimo, and ML Martins. "Parasite diversity in Oxydoras niger (Osteichthyes: Doradidae) from the basin of Solimões River, Amazonas state, Brazil, and the relationship between monogenoidean and condition factor." Brazilian Journal of Biology 71, no. 3 (2011): 791–96. http://dx.doi.org/10.1590/s1519-69842011000400026.

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This study describes the parasitic fauna of Oxydoras niger from the Coari Lake, tributary of the medium Solimões River, State of Amazonas, Brazil, and the relationship between the number of Monogenoidea and the condition factor. From a total of 27 examined fish, 70.3% were parasitised by at least one parasite species as follows: Ichthyophthirius multifiliis (Protozoa), Chilodonella sp. (Protozoa), Cosmetocleithrum gussevi, C. confusus, C. parvum and Cosmetocleithrum sp. (Monogenoidea), Paracavisona impudica (Acanthocephala), Cucullanus grandistomis (Nematoda), Proteocephalus kuyukuyu (Cestoda)

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42

Vivian Anyiam, Ifeoma, and Thomas Ohwofasa Ikpesu. "Microbiological quality and biochemical composition of water snail (Pachymelania byronensis) of lower Niger River basin." Emergent Life Sciences Research 4, no. 2 (2018): 1–10. http://dx.doi.org/10.31783/elsr.2018.420110.

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43

Oluwasegun, Adebayo H. "Flood risk and vulnerability mapping of settlements within upper and lower Niger river basin, Nigeria." Ethiopian Journal of Environmental Studies and Management 9, no. 1 (2017): 815. http://dx.doi.org/10.4314/ejesm.v9i1.2s.

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44

Oguntunde, Philip G., Babatunde J. Abiodun, Gunnar Lischeid, and Christoph Merz. "Modelling the impacts of reforestation on the projected hydroclimatology of Niger River Basin, West Africa." Ecohydrology 7, no. 1 (2012): 163–76. http://dx.doi.org/10.1002/eco.1343.

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45

Ward, John, and David Kaczan. "Challenging Hydrological Panaceas: Water poverty governance accounting for spatial scale in the Niger River Basin." Journal of Hydrology 519 (November 2014): 2501–14. http://dx.doi.org/10.1016/j.jhydrol.2014.05.068.

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46

Okpara, D. A., and M. B. Offiong. "Morphodynamics of river and coastal transport of sediments in mega delta basin, Niger Delta Nigeria." IOP Conference Series: Earth and Environmental Science 424 (January 27, 2020): 012010. http://dx.doi.org/10.1088/1755-1315/424/1/012010.

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47

Badou, Djigbo Félicien, Bernd Diekkrüger, Evison Kapangaziwiri, et al. "Modelling blue and green water availability under climate change in the Beninese Basin of the Niger River Basin, West Africa." Hydrological Processes 32, no. 16 (2018): 2526–42. http://dx.doi.org/10.1002/hyp.13153.

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48

López, Oliver, Rasmus Houborg, and Matthew Francis McCabe. "Evaluating the hydrological consistency of evaporation products using satellite-based gravity and rainfall data." Hydrology and Earth System Sciences 21, no. 1 (2017): 323–43. http://dx.doi.org/10.5194/hess-21-323-2017.

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Abstract. Advances in space-based observations have provided the capacity to develop regional- to global-scale estimates of evaporation, offering insights into this key component of the hydrological cycle. However, the evaluation of large-scale evaporation retrievals is not a straightforward task. While a number of studies have intercompared a range of these evaporation products by examining the variance amongst them, or by comparison of pixel-scale retrievals against ground-based observations, there is a need to explore more appropriate techniques to comprehensively evaluate remote-sensing-ba

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Ekeu-wei, Iguniwari, George Blackburn, and Philip Pedruco. "Infilling Missing Data in Hydrology: Solutions Using Satellite Radar Altimetry and Multiple Imputation for Data-Sparse Regions." Water 10, no. 10 (2018): 1483. http://dx.doi.org/10.3390/w10101483.

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In developing regions missing data are prevalent in historical hydrological datasets, owing to financial, institutional, operational and technical challenges. If not tackled, these data shortfalls result in uncertainty in flood frequency estimates and consequently flawed catchment management interventions that could exacerbate the impacts of floods. This study presents a comparative analysis of two approaches for infilling missing data in historical annual peak river discharge timeseries required for flood frequency estimation: (i) satellite radar altimetry (RA) and (ii) multiple imputation (M

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Picouet, C., B. Hingray, and J. C. Olivry. "Empirical and conceptual modelling of the suspended sediment dynamics in a large tropical African river: the Upper Niger river basin." Journal of Hydrology 250, no. 1-4 (2001): 19–39. http://dx.doi.org/10.1016/s0022-1694(01)00407-3.

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