| Figure 1. Time series of matric potential head monitored in the unsaturated zone and daily precipitation at a rangeland site in the Texas High Plains. (a) Different colored lines represent heat dissipation sensors installed at varying depths. Increased precipitation in 2004 resulted in deep percolation to at least 3 m; however, roots of perennial grasses and scattered shrubs removed the excess water by evapotranspiration over the following 2 years (Scanlon et al., 2005). |