This fact sheet provides strategies and best practices for landowners and residents to sustain and restore riparian and stream health on their land and in their communities.
In the arid Southwest, riparian* areas serve as lifelines. Although they may occupy a small fraction of the landscape, these “ribbons of life” support most of the region’s biodiversity.1 However, they are increasingly stressed by drought, changes in climate, and growing water demands. Managing watersheds and aquifers as integrated systems takes advantage of natural processes to ensure that water sources remain resilient for the future. Approximately 94% of the streams in Arizona are intermittent or ephemeral but only a few perennial streams remain.2 However, intermittent and ephemeral streams perform many of the same hydrologic functions as perennial streams: moving water, sediment, nutrients, and debris through the stream network and providing connectivity within the watershed.3
When water from rain or snow soaks into the ground, it becomes groundwater. If the water table is high enough, groundwater can flow into surface-level rivers and streams, either on a permanent or seasonal basis. One of the common metrics for measuring the health of a stream is baseflow, which is the contribution of groundwater to a stream. The groundwater contribution to streamflow is particularly important during the dry and summer months because there is less rain and snowmelt. In periods of low rainfall or excessive ground water pumping, the water table can fall and cease to contribute to streamflow. This can happen even if the pumping occurs far away from the stream. This can result in streams that no longer have running surface water, but conservation strategies that slow runoff and encourage infiltration can raise water tables and increase streamflow.4 Figure 1 shows how stream water seepage contributes to groundwater below the water table. Continue reading.