Estimating regional patterns and drivers of summer low flows in Idaho rivers and streams based on channel morphology data from EPA’s National Aquatic Resource Surveys
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As in many parts of the U.S., alterations in the flow of rivers and streams in Idaho have great potential to adversely affect physical habitat, water quality, and biological assemblages. The magnitude, frequency and timing of stream flows can be altered by flood and low flow management, changes in the impervious surface area within a drainage basin, extraction of surface and groundwater, and by natural or anthropogenic changes in precipitation or evaporation. In collaboration with EPA and USGS colleagues, I calculated low flow discharge based on field measurements of channel morphology routinely collected at sites sampled by the USEPA’s National Aquatic Resource Surveys (NARS). By truthing these estimates against USGS gauges and NARS snapshot discharge measurements, we were able to expand on the range of stream and river sizes where discharge measurements were available. This enabled us to estimate low flow alteration in all the NARS sites, where comprehensive measures of biota, physical habitat, and chemistry were also made. Our predictions of low-flow discharge (Log10-transformed) had a regression RMSE=0.54 compared with actual low flow discharge measurements (m3/s) ranging over six orders of magnitude at >700 closely matched USGS gauge locations in the U.S. The primary drivers of low flow discharge in Idaho and other Pacific Northwest river and stream sample sites were drainage area, precipitation, and temperature; but anthropogenic activities altered summer low flows substantially. Low flows in Idaho river and stream sample sites were negatively associated with the general level of anthropogenic activity. Diminished summer low flows were primarily associated with road density and agricultural land use, particularly when agricultural land use was in or near riparian areas, whereas urban land uses were associated with augmented summer flows. In larger Idaho rivers, dams were associated with higher-than-expected summer flows, but in smaller streams and rivers, dams were associated with lower-than-expected summer flows. Our approach offers promise for supporting the evaluation of the effects of hydrologic alteration on physical habitat and biota in rivers and streams routinely monitored by state, federal, and tribal agencies.