We have earlier seen that Waterbalance of a given location explains the fundamental mechanism of the nature of hydrological cycle in a given Soil-Plant-Atmospheric regime. In this page, the users can visualize the nature of waterbalance in any location of their choice in the MENA region. The underlying data used is the high resolution monthly climate datasets. These monthly datasets are first converted into long term averaged (15 years) annual values. Thereafter these annual values are used to analyze the water balance components. As you can see, at long time steps (e.g. annual) the change in soil water storage (ΔS) tends to zero. In locations where ΔS deviates from zero, there is a high probability of Rain Water Harvesting. The regression equation analysis gives an idea regarding how well the water balance is “closed” in the user defined area of interest.