Natural Streamflow Estimates for Watersheds in the Lower Yakima River 1 David L. Smith 2 Gardner Johnson 3 Ted Williams 1 Senior Scientist-Ecohydraulics, S.P. Cramer and Associates, 121 W. Sweet Ave., Moscow, ID 83843,
[email protected], 208-310-9518 (mobile), 208-892-9669 (office) 2 Hydrologist, S.P. Cramer and Associates, 600 NW Fariss Road, Gresham, OR 97030 3 GIS Technician, S.P. Cramer and Associates, 600 NW Fariss Road, Gresham, OR 97030 S.P. Cramer and Associates Executive Summary Irrigation in the Yakima Valley has altered the regional hydrology through changes in streamflow and the spatial extent of groundwater. Natural topographic features such as draws, coulees and ravines are used as drains to discharge irrigation water (surface and groundwater) back to the Yakima River. Salmonids are documented in some of the drains raising the question of irrigation impacts on habitat as there is speculation that the drains were historic habitat. We assessed the volume and temporal variability of streamflow that would occur in six drains without the influence of irrigation. We used gage data from other streams that are not influenced by irrigation to estimate streamflow volume and timing, and we compared the results to two reference streams in the Yakima River Valley that have a small amount of perennial streamflow. We estimate that natural streamflow in the six study drains ranged from 33 to 390 acre·ft/year depending on the contributing area. Runoff occurred infrequently often spanning years between flow events, and was unpredictable. The geology of the study drains was highly permeable indicating that infiltration of what runoff occurs would be rapid.