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ghana climate change vulnerability and adaptation assessment

ghana climate change vulnerability and adaptation assessment

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effect. In the drier scenario, the waterlevel of lake is low <strong>and</strong> most often below the level atwhichhydropower productionis impossible. The wetter scenarios pushh lake levels tonear maximal operatingcapacities. In the reference (or no <strong>change</strong>) scenariotarget releases were met but storage was close toinadequate. Similar sensitivity to <strong>climate</strong> variability was indicatedd in another hydrological simulation(Leemhuiset al., 2009) <strong>and</strong> <strong>assessment</strong>s focused onthe Black Volta basin (i.e., Bui dam project, Laube et al.,2008) predict reduced water availability from reduced seasonal rainfall <strong>and</strong> river flows which will beexacerbated by higher temperatures <strong>and</strong> evapotranspiration. These factors, apparently not accounted forindam planning <strong>and</strong> design, could negatively affect the hydropower operations at Bui dam (Biney, 2010).Interestingly, in another20-year modeling scenario, small upstream reservoirss with a steadystate annualincrease of 10 percent were projectedto reduce Lake Volta inflows by about 3 percent at the end of 20 years.This is a small impact on power production relative to present variability in storage volumeor to possible<strong>change</strong>s caused by <strong>climate</strong> <strong>change</strong> (Lemoalle <strong>and</strong> Condappa, 2009) but is nevertheless a reduction in powergeneratingg capacity. A question remains of whether the 10 percent annual increase in upstream reservoirrcapacity isan under-or over-estimateof water development in northern Ghana <strong>and</strong> ripariancountries in thenext 20 years.Source: Condappa et al. 2009, Lemoalle <strong>and</strong>Condappa 2009Figure 10.4 Simulation of water storage in Lake Volta undera reference conditionn(No <strong>change</strong>from 1980-2000) <strong>and</strong> three scenarios of <strong>climate</strong> <strong>change</strong>. The black line labeled “Top of inactive (70 km 3 )” indicatesthe storage level at which hydropower generation is impossible at Akosombo dam <strong>and</strong> thee one labeled “Storage capacity (148km 3 )” is thecapacity of Lake Volta at full pool)Clearly theissue of future hydropower production from Akosombo (<strong>and</strong> Kpong) dams is complex, notsimplistically related to potential <strong>climate</strong> <strong>change</strong>, <strong>and</strong> is replete with transboundary implications. First, thewater development focus between the two major countries in the Volta Riverr Basin is fundamentallydifferent. Burkina Faso has <strong>and</strong> is concentrating effort in the Basin on improved use <strong>and</strong> increased retentionof water for agriculture with dem<strong>and</strong>s in that country (as well ass northern Ghana) expectedto increaseGHANA CLIMATE CHANGE VULNERABILITY ANDADAPTATIONASSESSMENT169

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