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The Solar suitability mapping framework was developed using a GIS-based Multi-Criteria Evaluation (MCE) technique. The multi-criteria evaluation was implemented by combining spatial information from a number of geospatial drivers for solar based irrigation. These data sourced from a number of national and international databases include solar irradiation, slope, groundwater levels, aquifer productivity, groundwater storage, groundwater sustainability, proximity to rivers, proximity to small dams and inland valleys, soil characteristics, crop and land suitability, population, roads and travel time to markets. First, a constraint layer was developed to differentiate areas that would be suitable for solar based irrigation from those that cannot be suitable under any condition. Protected zones, forested and urban areas, and areas with extreme with droughts identified as unsuitable for agricultural production were excluded.
The absolute values of each of the input drivers (solar irradiation, slope, groundwater levels, aquifer productivity, groundwater storage, proximity to rivers, inland valleys and reservoirs, soil texture, soil drainage, soil depth, soil organic carbon, soil available water content, distance to roads, population density and travel time to markets) were rescaled to a 1-5 scale and used to derive weighted combination maps for the suitable areas. Layer weights were determined and assigned using the Saaty Analytic Hierarchy process in a GIS environment. A nearest neighbour resampling scheme was used to resample each of the individual inputs to obtain final suitability areas at a 90 meter resolution.
Suitability for solar-powered irrigation was mapped when considering different water resources: only surface water, only groundwater and both surface and groundwater at various groundwater depths (0-7 m, 7-25 m, 25-50 m, 50 – 100 m, 100-250 m).
Legends were generated using an equal interval class. The legends range from 20% probability in least suitable areas to 100% probability in highly suitable areas. Graduation is as below:
Least suitable 0 - 30% probability
Less suitable 30.1 - 60% probability
Moderately suitable 60.1 - 75% probability
Suitable 75.1 - 90% probability
Highly suitable 90.1% - 100% probability
To improve predictions for your country or region, consider contributing/sharing validation data or additional data so that your data can be included in the framework. IWMI always respects the data policy of data providers and will not publically share any data unless written permission is given to do so. Agencies that contribute their data will be dully acknowledged.
Hengl, T., de Jesus, J.M., Heuvelink, G.B.M., Gonzalez, R.M., Kilibarda, M., Blagotic, A., Wei, S., Wright, M.N., Geng, X., Bauer-Marschallinger, B., Guevara, M.A., Vargas, R., MacMillan, R.A., Batjes, N.H., Leenaars, J.G.B., Ribeiro, E., Wheeler, I., Mantel, S.K., Kempen, B., 2017. SoilGrids250m: Global gridded soil information based on machine learning. PLoS Biol. 12, 729–736.
MacDonald, A.M., Bonsor, H.C., Dochartaigh, B.É.Ó., Taylor, R.G., 2012. Quantitative maps of groundwater resources in Africa. Environ. Res. Lett. 7.
Schmitter, P., Kibret, K.S., Lefore, N., Barron, J., 2018. Suitability mapping framework for solar photovoltaic pumps for smallholder farmers in sub-Saharan Africa. Appl. Geogr. 94, 41–57.
Instructions Select one or both water source(s) you are planning to abstract using solar based pumping.
Description Ground water represents all water which occurs below the land surface. It includes both water within the unsaturated and saturated zones.
Surface water represents all water above the earth’s surface. This includes lakes, reservoirs, wetlands, rivers, small ponds or any other form of water stored in the landscape.
Surface water represents all water above the earth’s surface. This includes lakes, reservoirs, wetlands, rivers, small ponds or any other form of water stored in the landscape.
Instructions Select one or both water source(s) you are planning to abstract using solar based pumping.
Groundwater represents all water which occurs below the land surface. It includes both water within the unsaturated and saturated zones. (for more information see here )
Surfacewater represents all water above the earth's surface. This includes lakes, reservoirs, wetlands, rivers, small ponds or any other form of water stored in the landscape.
Surface water represents all water above the earth’s surface. This includes lakes, reservoirs, wetlands, rivers, small ponds or any other form of water stored in the landscape.
Based on the pump specifications of the surface pump or a submersible pump, select the maximum head (m) where the flow rate first reaches zero (Global LEAP 2019 buyers guide). (photo credit Global LEAP 2019 buyers guide)
0m - 7m: The interval assumes that below 7m the pump would be unable to lift water.
7m - 25m: The interval assumes pump lifts water from 7m to 25m depth only.
25m - 50m: The interval assumes pump lifts water from 25m to 50m depth only.
50m - 100m: The interval assumes pump lifts water from 50m to 100m depth only.
100m - 250m: The interval assumes pump lifts water from 100m to 250m depth only.
0m - 250m: The interval assumes pump lifts water from 0m to 250m depth only.
Pump examples can be accessed here
To estimate the dimensions, type and financial viability of Solar Powered Irrigation Systems for a specific farming situation please use the Solar Powered Irrigation Systems Toolbox here
Legends were generated using an unequal interval class from 0-30% probability in least suitable areas to 90.1-100% probability in highly suitable areas. Graduation is as below:
Least suitable 0 - 30% probability
Less suitable 30.1 - 60% probability
Moderately suitable 60.1 - 75% probability
Suitable 75.1 - 90% probability
Highly suitable 90.1% - 100% probability
The selection summary will display your selected water source, maximum head and country of your interest. You can go back to any of the previous steps if modifications are needed. To analyse the areal suitability click 'Calculate Suitability'.
Instructions: This section will present you calculation results. Multi-section is possible and results upto four calculation sections can be added for analysis.
Once you have select one or more (water source + lifting capacity for underground water + location) you can use below buttons to plot your results, download results or to remove result section.
Welcome to our interactive online tool to assess land suitability for photovoltaic based irrigation using solar energy. The tool supports you in identifying suitable areas for solar based irrigation depending on water sources and pump characteristics. To use the tool, click on the left panel and select your water source, pump capacity and country of interest. For a detailed description on the methodology and spatial information used please go to the methodology tab. As data remains scarce for some countries in Africa we appreciate if you would like to support us by sharing relevant spatial information so we can refine our maps. Please use the lower left box to share any relevant information. As we continuously strive to update and refine the tool for you we would appreciate any feedback. Please use our message button at the top right corner to send us a message or any comments and queries you may have or take a brief survey on the use of the tool.
We hope you enjoy your platform,
The International Water Management Institute, Futurepump and GIZ
GW - Ground Water
SW - Surface Water
GW - Ground Water
SW - Surface Water
Make adjustments to your searches by toggling between them here.
Interested in multiple locations and searches? Add another calculation here before analysing - can add up to 4 at a time.
Select your location by selecting a country. Further localise your selection by district/zone.
You can select Ground water, Surface water or both.
Select a water lifting capacity as necessary for ground water.
Great. You are almost ready to submit your calculations. Click the big arrow to analyse.
Great, you're almost there to submit your calculation, hit the big arrow to analyse.
(All area outputs are calculated in km2)
Calculation | 1 | 2 | 3 | 4 |
---|---|---|---|---|
Location | No Location | Guinea-Bissau | Cameroon | Zimbabwe |
Source | GW/SW | GW/SW | GW/SW | GW/SW |
Depth | X-XXm | X-XXm | X-XXm | X-XXm |
Least Suitable | X | X | X | X |
Less Suitable | X | X | X | X |
Moderately Suitable | X | X | X | X |
Suitable | X | X | X | X |
Highly Suitable | X | X | X | X |
(All area outputs are calculated in km2)
Calculation | 1 | 2 | 3 | 4 |
---|---|---|---|---|
Location | No Location | Guinea-Bissau | Cameroon | Zimbabwe |
Source | GW/SW0 | GW/SW | GW/SW | GW/SW |
Depth | X-XXm0 | X-XXm | X-XXm | X-XXm |
Least Suitable | X0 | X | X | X |
Least Suitable | X0 | X | X | X |
Least Suitable | X0 | X | X | X |
Least Suitable | X0 | X | X | X |
Least Suitable | X0 | X | X | X |
Check about impact of input data for suitability by switching the toggle button at right bottom corner.
Shows the contribution of the main input data layers to solar suitability for a selected area. A thumbs up indicates at least half of the area selected is suitable. A thumbs down indicates more than half of the selected area is not suitable.