“…When cultivated cropland are converted from forestland and grassland, ET generally tends to decrease, providing opportunity for more water to percolate down and contribute to groundwater recharge (e.g., Adane, Nasta, Zlotnik, & Wedin, ; Owuor et al, ; Scanlon, Jolly, Sophocleous, & Zhang, ), thus leading to downstream flow moderation. Field experiments demonstrated that grassland depletion contributes to changes in hydrologic processes such as ET, run‐off, soil moisture, and infiltration (Fiedler, Frasier, Ramirez, & Ahuja, ; Li et al, ), which are, in turn, influenced by inherent soil properties, land use and land cover patterns, the initial moisture condition, and rainfall patterns (Agnihotri & Yadav, ).…”