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Groundwater availability for irrigation in Sub-Saharan Africa

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Presented by IWMI's Karen G. Villholth (Principal Researcher and sub-Theme Leader) at the 2016 Water for Food Global Conference at Nebraska Innovation Campus in Lincoln, Nebraska, USA, held on April 24-26 , 2016.

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Groundwater availability for irrigation in Sub-Saharan Africa

  1. 1. Groundwater availability for irrigation in Sub-Saharan Africa Karen G. Villholth Principal Researcher and sub-Theme Leader IWMI, International Water Management Institute Pretoria, South Africa 2016 Water for Food Global Conference Nebraska Innovation Campus, Lincoln, Nebraska, USA, 24-26 April, 2016
  2. 2. Outline • How can groundwater be part of a solution of enhancing irrigation, food security, resilience, and livelihoods of smallholder farmers in Sub- Saharan Africa (SSA?) • What is the potential?
  3. 3. GW irrigated/cultivated land Africa ~1 % Asia ~14 %Siebert et al., 2010 GW irrigation intensity Percentage of 5 arc min grid cell area equipped for irrigation with groundwater
  4. 4. Photo:DavidBrazier/IWMIPhoto:TomvanCakenberghe/IWMI  Based on a water balance calculation done annually over a 41 year period (1960 – 2000) at a resolution of 50 km x 50 km  Some assumptions in computations  GW is the only water source for irrigation (no conjunctive use with SW)  GW is usable and accessible (no quality, yield, or socio-economic constraints)  GW is locally available 𝑮𝑾𝑰𝑷 (m2) = 𝐺𝑊 𝐴𝑣𝑎𝑖𝑙𝑎𝑏𝑙𝑒 (m3 year−1) 𝐼𝑟𝑟𝑖𝑔. 𝑊𝑎𝑡𝑒𝑟 𝐷𝑒𝑚𝑎𝑛𝑑 (𝑚 year−1) (calculated annually) 𝑰𝒓𝒓𝒊𝒈. 𝑾𝒂𝒕𝒆𝒓 𝑫𝒆𝒎𝒂𝒏𝒅 = {σ 𝑖=1 𝑛 σ 𝑗=1 𝑚 𝐶𝑟𝑜𝑝 𝑊𝑎𝑡𝑒𝑟 𝐷𝑒𝑚𝑎𝑛𝑑−𝐺𝑟𝑒𝑒𝑛 𝑊𝑎𝑡𝑒𝑟 𝑗 × % 𝑜𝑓 𝐴𝑟𝑒𝑎 𝑖 } 𝐼𝑟𝑟𝑖𝑔. 𝐸𝑓𝑓𝑖𝑐𝑖𝑒𝑛𝑐𝑦 = 𝑁𝑒𝑡 𝐼𝑟𝑟𝑔. 𝑊𝑎𝑡𝑒𝑟 𝐷𝑒𝑚𝑎𝑛𝑑 𝐼𝑟𝑟𝑖𝑔. 𝐸𝑓𝑓𝑖𝑐𝑖𝑒𝑛𝑐𝑦 (n= crop) (Calculated monthly then summed on an annual value) 𝑮𝑾 𝑨𝒗𝒂𝒊𝒍𝒂𝒃𝒍𝒆 = 𝐺𝑊 𝑅𝑒𝑐ℎ𝑎𝑟𝑔𝑒 – 𝐻𝑢𝑚𝑎𝑛 𝐺𝑊 𝐷𝑒𝑚𝑎𝑛𝑑 – 𝐸𝑛𝑣𝑖𝑟𝑜𝑛. 𝐺𝑊 𝑅𝑒𝑞 (calculated annually then averaged over 41 years to consider buffer effect of GW) Mapping irrigation potential from renewable GW in Africa Altchenko & Villholth, 2015
  5. 5. Photo:DavidBrazier/IWMIPhoto:TomvanCakenberghe/IWMI  Hydrological data from the PCR-GLOBWB model (Utrecht University, the Netherlands, Wada et al., 2011) • Reference evapotranspiration • Water available from rain for crop (green water = transpiration soil 1 and 2) • Recharge  Other GW uses • human activities (domestic, livestock, industrial) based on ‘’present’’ human water demand derived from density of population and livestock, and unit requirement (FAO, geonetwork) • environment based on according to three different scenarios:  Scenario 1 : 70% of the recharge goes to environment  Scenario 2 : 50% of the recharge goes to environment  Scenario 3 : 30% of the recharge goes to environment Different geographical data compiled in GIS Resolution: 0.5 degree (≈ 50 km x 50 k cell)  Crop data • Crop distribution • Crop water demand • Irrigation efficiency monthly calendar for crop group water demand Methodology
  6. 6. Photo:DavidBrazier/IWMIPhoto:TomvanCakenberghe/IWMI  Average Net Irrigation Water Demand (1960-2000) Results Rainfall Cropland
  7. 7. Photo:DavidBrazier/IWMIPhoto:TomvanCakenberghe/IWMI  Proportion of cropland irrigable with groundwater A factor of 20 increase in overall GWI area possible (from 2 to ≈ 40 mill ha.) Environmental requirements represent 70% of recharge 50% of recharge 30% of recharge Area (106 ha) 44.6 74.9 105.3 % of cropland 20.5% 34.5% 48.5% Results 70% 30%50%
  8. 8. Photo:DavidBrazier/IWMIPhoto:TomvanCakenberghe/IWMI  Comparison with GW irrigated cropland in 2005 (Siebert et al., 2010) (a) Actual area irrigated with groundwater in 2005 expressed in ha. per cell adapted from Siebert et al. (2010) and (b) groundwater irrigation potential for scenario 2 for the year 2000 expressed as the percentage of the area irrigated with groundwater in 2005 Results
  9. 9. 9 The GWIDP is determined by combining the socio-economic factors influencing the groundwater irrigation development in Africa: • Lack of access to surface water: the GWIDP decreases closer to perennial surface water resources • Access to market: the GWIDP increases closer to towns and roads as groundwater irrigation is often associated with cash crops • Soil suitability for agriculture: irrigation is more suitable for specific soil characteristics. • Borehole investment: the GWIDP decreases with the depth of the groundwater table • Access to energy: the GWIDP increases closer to the electrical grid as electricity is the cheapest energy source for pumping. Overlaying with socio-economic factors
  10. 10. Photo:DavidBrazier/IWMIPhoto:TomvanCakenberghe/IWMI (a) Average annual recharge (mm/year), and (b) its coefficient of variation (%), both over the period 1960-2000 (data from Wada et al., 2011) Country Recharge (mm/yr) FAO, AQUAStat, 2009 Döll and Fiedler, 2008 This study Burkina Faso 34.6 39 39 Ethiopia 18.1 39 80 Ghana 110.3 105 127 Kenya 6.0 46 29 Malawi 21.1 164 170 Mali 16.1 22 23 Mozambique 21.3 104 82 Niger 2.0 12 4 Nigeria 94.2 163 154 Rwanda 265.8 68 78 Tanzania 31.7 93 90 Uganda 122.9 95 50 Zambia 62.4 108 117  Recharge variability Recharge uncertainty and variability  Recharge uncertainty
  11. 11. Photo:DavidBrazier/IWMIPhoto:TomvanCakenberghe/IWMI 11  A pan-African distributed map of GWIP has been produced for the first time  GW irrigated areas can be increased by a factor of 15 (2 to 30 mill ha), socio-economic factors considered  Potential is particularly significant in the semi-arid Sahel and East African corridor, with huge poverty alleviation potential for small-scale and smallholder irrigation  Climate change might affect GW recharge and increase crop water demand  Actual potential will depend on borehole yields, irrigation efficiency, and crop choices Conclusion Photo: Univ. of Strathclyde
  12. 12. Photo:DavidBrazier/IWMIPhoto:TomvanCakenberghe/IWMI Altchenko, Y. and Villholth, K.G.: Mapping irrigation potential from renewable groundwater in Africa - a quantitative hydrological approach. Hydrol. Earth Syst. Sci., 19, 1055-1067. doi:10.5194/hess-19- 1055-2015, 2015. Siebert, S., Burke, J., Faures, J. M., Frenken, K., Hoogeveen, J., Döll, P., and Portmann, F. T.: Groundwater use for irrigation – a global inventory, Hydrol. Earth Syst. Sci., 14, 1863–1880, doi:10.5194/hess- 14-1863-2010, 2010. Wada, Y., Van Beek, L, Viviroli, D., Dürr, H., Weingartner, R., and Bierkens, M.: Global monthly water stress: 2. Water demand and severity of water stress, Water Resour. Res., 47, W07517, doi:10.1029/2010WR009792, 2011.
  13. 13. Thank You Contact: k.villholth@cgiar.org