Many basins in the western United States rely on adequate winter snowpack and the slow release of water as temperatures warm to sustain streamflow and meet demand through the dry summer season (Mote et al., 2018). Volume of streamflow is especially vulnerable in these snow-dominated regions due to long-term changes in precipitation and temperature, which impact maximum snow accumulation and runoff timing (Barnett et al., 2005;Clow, 2010). Since water year 1984, winter temperatures have increased significantly, and winter precipitation, maximum snow water equivalent, and snow covered days per decade decreased significantly in the Rio Grande basin (Harpold et al., 2012). In