2019
DOI: 10.1088/1748-9326/ab055a
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Regional climate projections for impact assessment studies in East Africa

Abstract: In order to overcome limitations of climate projections from Global Climate Models (GCMs), such as coarse spatial resolution and biases, in this study, the Statistical Down-Scaling Model (SDSM) is used to downscale daily precipitation and maximum and minimum temperature (T-max and T-min) required by impact assessment models. We focus on East Africa, a region known to be highly vulnerable to climate change and at the same time facing challenges concerning availability and accessibility of climate data.

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Cited by 80 publications
(54 citation statements)
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“…The impacts of climate change such as rising temperatures and unpredictable precipitation intensity and patterns have become undeniably unequivocal in East Africa [1][2][3], impacting the fragile ecosystems such as wetlands in the region. In addition, human and environmental stressors such as land use changes associated with rapid urbanization and uncoordinated expansion of intensive agricultural production in these wetlands negatively impair their water availability, quality and other ecosystem services and functioning [2,4,5]. The negative impacts associated with climate and land use change are also compounded by other factors, notably exacerbating poverty and high population pressure, which is anticipated to increase demand for food and water in the future [6,7].…”
Section: Introductionmentioning
confidence: 99%
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“…The impacts of climate change such as rising temperatures and unpredictable precipitation intensity and patterns have become undeniably unequivocal in East Africa [1][2][3], impacting the fragile ecosystems such as wetlands in the region. In addition, human and environmental stressors such as land use changes associated with rapid urbanization and uncoordinated expansion of intensive agricultural production in these wetlands negatively impair their water availability, quality and other ecosystem services and functioning [2,4,5]. The negative impacts associated with climate and land use change are also compounded by other factors, notably exacerbating poverty and high population pressure, which is anticipated to increase demand for food and water in the future [6,7].…”
Section: Introductionmentioning
confidence: 99%
“…Most parts of eastern Africa have experienced frequent droughts and a decline in total rainfall during the long rains [26,27], although GCM projections show wetter conditions in the future [27], a contradiction which has been referred to as the East African paradox by Rowell et al [26]. In fact, the Intergovernmental Panel on Climate Change (IPCC) Fifth Assessment Report (AR5) reports large levels of uncertainty in the temporal and spatial variability of precipitation over East Africa in the future [5]. According to Endris et al [25], the GCM and RCM data project a decrease in seasonal rainfall over most parts of East Africa during the June to September (JJAS) and March to May (MAM) seasons.…”
Section: Introductionmentioning
confidence: 99%
“…In studies like the one performed by Nakaegawa [40] or Ospina [41], river discharge in the north of Colombia was analyzed using direct output from a GCM as a hydrometeorological input of the model, and similar studies could be performed in the four selected water districts at the east of Colombia considering the results of the current study in order to use the historical records from these areas to develop a regional climate downscaling or water budget analysis. The spatial and temporal data resolutions show acceptable characteristics for the purpose of performing reliable posterior analysis such as some developed through statistical regional downscaling on other areas with similar characteristics [31,32,[42][43][44], or water budget analysis [45][46][47][48][49]. The use of a dynamical downscaling method could also provide more accurate results, but this approach demands much more intensive computational resources and require large volumes of data which are not available for the studied regions, thus, using a statistical downscaling technique is recommended as a first approach.…”
Section: Discussionmentioning
confidence: 99%
“…Downscaling using stochastic and transfer function methods is performed by modifying parameters using weather generators and developing a statistical relationship between predictands and predictors, respectively. The input data for the SD model must be carefully analyzed since the statistical relationship between the predictors and predictands is the more important aspect in statistical models [31].…”
Section: Regional Downscalingmentioning
confidence: 99%
“…High performance of CHIRPS has been proven in areas where station data are not included [13,86]. In addition, the product has been used in many evaluation studies [87,88] and recommended to support hydrological forecasts and trends analysis, for instance, as proved in an Ethiopian case study [89,90] and other studies that use CHIRPS as input in hydro climate modeling [58,90]. Table 10 below shows the results of CHIRPS performance in several previous studies.…”
Section: Statistical Estimatorsmentioning
confidence: 99%