Runoff and Floodwater Farming in the MENA and SW North America
When it rains some water enters the soil, the rest runs off. As it gathers strength it becomes the floodwater that runs through valleys, streets, arroyos and wadis after a rain storm. Sparse vegetation, little soil development, soil crusts, and low infiltration/absorption contribute to fast peaking flows in arid regions[1]. Storms lead to floods that may continue for minutes, hours or days depending on the rainfall. Flood depths of 5-10 meters may occur in extreme events. Residents in arid and semi-arid lands have developed a wide range of strategies to hold and capture critically needed water. In many cases floodwater … Continue reading