The demand for water storage to mitigate seasonal shortages in semiarid regions increases with changes in rainfall and drought patterns and expansion of agricultural water needs (Assouline et al., 2015;Dai, 2011). Traditionally, local systems of small (on farm) reservoirs have been used by civilizations all over the world to meet water needs during the dry season (Raymond, 1969) and sustain their livelihood (domestic, agriculture, and livestock) (Payen et al., 2012). These small reservoirs (<0.1 km 2 ) are filled during the rainy season, thus offering economical and localized solution for water storage (Lasage & Verburg, 2015). Inventories have shown that storage in local impoundments and farm reservoirs smaller than 0.1 km 2 dominate in number and geographic distribution of artificial water reservoirs (Downing et al., 2006). Recently, we estimated that over 2.9 million reservoirs smaller than 0.1 km 2 are presently in use in semiarid regions with total surface area of 17,800 km 2 and seasonal storage of 37 km 3 (Mady et al., 2020). Due to high evaporative demand in these regions, evaporation losses have significant impact on effective storage and limit water availability in the dry season (Battisti & Naylor, 2009;Craig, 2008). Estimates suggest that in hot periods evaporation losses from water reservoirs range from 10% in Spain (Martínez Álvarez et al., 2008) to 50% in Australia (Craig 2005;Rost et al., 2008). Regionally resolved analyses by Mady et al. (2020) suggest that globally 30% of the stored volume in small reservoirs could be lost to evaporation during the dry season (in semiarid regions).Various mitigation techniques have been proposed for reducing evaporation losses, differing in their suppression efficiency and construction and maintenance costs (