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Energy Generation Potential of West African Ocean Current: Peculiarities, Challenges and Perspectives

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Energy Generation Potential of West African Ocean Current: Peculiarities, Challenges and Perspectives Energy Generation Potential of West African Ocean Current: Peculiarities, Challenges and Perspectives 1 2 Agbakwuru, Jasper Ahamefula , Nwaoha, Thaddeus Chidiebere 1,2 Department of Marine Engineering, Faculty of Technology, Federal University of Petroleum Resources, P.M.B. 1221 P.M.B. 1221 Effurun, Nigeria . Abstract A review of the West African ocean current energy generating potential is carried out. The peculiarity of the West African ocean characteristic is discussed and the challenges noted. Based on this review, it is found that ocean current represents an alternative source of renewable energy in West Africa in a streamed regular supply. The ocean weather condition is mild and offers good benefit to marine operations with respect to renewable energy conversion system installations offshore. In the perspective of the authors, it is believed that engineering and scientific investments are necessary in order to harness the ocean current renewable source in West Africa. Suggested techniques include - Application of momentum diffusion technology to the ocean current flow system; Design of ocean current generating system whose efficiency relies more on volume flow rather than fast running fluid velocities; Investigation into reported increased velocities suspected to be due to hydrodynamic influence of discharging upland rivers into the ocean water systems. A success of such confirmation will lead to the use of conventional generating system in such locations.It is largely hoped that aggressive interests in the subject area will open wide opportunities in the ocean current renewable energy source to supplement the intense energy demand of this part of the continent. Keywords- Ocean; current; renewable; energy; momentum-diffusion; upland-rivers; velocity; West Africa. 1.0 Introduction World-wide, there has been a necessary preferred installation for water current trend of energy shift from what it used to be, generation is in the open ocean. to the renewable sources. The costs, Examining developments in water/ocean depletions, environmental and green house current energy generation in West Africa, effects of the hydrocarbon sources are some only minimal effort has been made despite the of the reasons for this shift. On the other hand, opportunities in the continent. Interestingly, the hazard posed by nuclear power plant leak most countries in the continent encourage and in recent time has introduced skeptics in a support financing of renewable forms of nuclear power source. Africa is endowed with power generation in the country. Instances of huge energy from the sun [1]. There has been political and economic supports as described great effort in recent time to harness solar by [5] and the National Renewable Energy energy by corporate companies, non-profit and Energy Efficiency Policy of April- 2015 organization and government. Good success of the Nigerian Ministry of Power in tapping the solar energy source has been demonstrate the need to engage in sustained made due to improved efficiency in solar technology on renewable energy sources system design [2]. In Asia and America, water within our disposal. current generators have received attention The purpose of this paper is to signal the because water current is relatively constant need for more research and development in compared to solar source [3] and [4]. Due to water current energy generation in West space requirement and ecological reasons, the Africa in order to meet the energy challenge of the continent and also further reduce the West African Journal of Industrial & Academic Research Vol.15 No.1 December 2015 12 over dependence on hydrocarbon energy the Guinea Current was higher offshore than source with its associated green house effect onshore. Thus, [15] suggested that the that is today threatening the existence of our presence of a westward current at the surface global world. near the coast could be due to the surfacing of the Ivoirian Undercurrent and the seaward 1.1 West African ocean characteristic displacement of the Guinea Current, not due and its peculiarities to the reversal of the Guinea Current. Another West African ocean condition is mild in explanation, proposed by [12] is that the nature. Reference [6] discussed the apparent reversals are actually caused by continental shelf of the West African region cyclonic eddies between the current and the between 5o N and 15o S. It is noted that the coast. Reference [12] points out that "the data extreme wave condition in the West African on which the concept of current reversals is area is quite uncommon because tropical based are either point observations or isolated cyclones do not occur in the South Atlantic sections perpendicular to the coastline," which Ocean. Reference [7] discusses that the do not clearly depict current reversals in the environment of Offshore West Africa lacks alongshore direction.” locally generated storms, therefore the storm The overall implication is that the West surge is minimal and tidal current dominate African Offshore condition is peculiar. water level variations. A Statoil report on Though suitable site of high velocity flow of Offshore Nigeria points that approximately current near shore is not presently identified 95% of the swells come from sector, 165o to by literatures for ocean current renewable 225o [8]. energy generation in West Africa, it is noted Guinea current is the prevalent offshore that [8] and [17] for Offshore Nigeria and current in West Africa. Reference [9] Angola respectively indicate current average described that depending on the season, the speed range of 0.3 ms-1 to 0.4 ms-1 and primary source of waters for the Guinea maximum of 0.8 ms-1 with monsoon and other Current is either the Canary Current or the N. seasonal effects. This excludes the Equatorial Counter Current (NECC). For hydrodynamic influence of discharging example, during the winter, the NECC is very upland river systems into the ocean water weak, while in the summer, the NECC is at its which can alter these values substantially. strongest. As stated by [9], several authors ([10], 1.2 Challenges [11], [12], [13] and [14]) agree that the The challenges of measuring current Guinea Current experiences a minimum ranges from cost elements, measurement during November through February and a duration requirement and unfriendly maximum during May through September. environmental conditions and software issues. As discussed by [13], some authors ([10], It takes some millions of United State Dollar [11]) thought they had detected a reversal in in cost to operate a typical ocean data current direction during the minima. They gathering vessel for a full year data collection. attributed this change to variations in the flow There are also local marine and environmental of the North Equatorial Countercurrent, the variations that are difficult to deal with. Canary Current, and the Benguela Current The interests in the field of ocean current ([10], [12]), and to the weakening of the measurements have been majorly to predict easterly winds ([11], [12]). However, [15] transport of sediment, determine drift of offered an alternative explanation. As the contaminates, transport processes, determine authors were studying the currents on the loadings on marine structures and ocean continental shelf of the Ivory Coast during transports [18]. The interests have minimal December, they observed not only the Guinea focus on power generation and engineering. Current, but also a current below it. This current, named the Ivoirian Undercurrent, 1.3 Prospects and Perspective flowed opposite to the Guinea, to the west. In general terms, the current They also noticed that at times the speed of speed/velocity in West Africa may be West African Journal of Industrial & Academic Research Vol.15 No.1 December 2015 13 considered low with respect to ocean selection often a higher momentum and will diffuse site criteria recently developed by [3] and [19] into the lower momentum in the direction of the consistency and regularity of the current flow. As at today, no literature is found flow is a major benefit that must not be discussing momentum diffusion with respect overlooked. Scientific and engineering to maximizing generated fluid flow forces. methods to effectively harness this energy Exploring this field of science is source should be investigated and applied. necessarily required. A scientific method could be the An engineering method could be a design application of momentum diffusion technique of special blades that would operate optimize to amplify flow velocities. When a streaming volume flow energy of water in a given flow is guided by a smooth straight plate of direction rather than the present turbine minimal cross sectional area, a laminar flow is technology that depend largely on fast optimised within the guided channel. In this running fluid velocities. The result could be open system as we have in an open ocean, slow motion with large torque that can be shear stresses and pressure variations within reconverted to electrical energies. These will the flow will generate momentum change be examined in another paper. within the affected fluid. This momentum is Furthermore, measurements reported by [20] showed some surprises which was not recognized by the authors as a potential for generation of power from the ocean current. Figure 1 shows some of the results of field measurements conducted using RD 300 KHz ADCP deployed at a Benin River at a shallow water depth of 15.8m within the mouth of Escravos and Forcados River as reported by [20]. The measurement between 19th April 2000 and 4th February 2001 at 2.3 meter from sea bottom in a current polar plot indicates a possibility of water current speed of about 3 m/s. It is suggested that the local water fluxes others along the West African ocean coast. It from discharge of Figureupland 1.Rivers High speedinto thewater currentis suspected as reported that by the[20]. increased speed of ocean can contribute to this increased ocean current at this local position is the resultant It is suggested that the local water fluxes from flow speed of the Atlantic current and the in- discharge of upland Rivers into the ocean can fluxing rivers.
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