The snowmelt season for water years 2001 to 2003 were modeled for the Salt, Tonto, and Verde basins in Arizona using the Snowmelt Runoff Model (SRM). The SRM is a degree-day-driven snowmelt model. The purpose was to assess how well the SRM could simulate the snowmelt runoff conditions in Arizona, an arid subtropical environment that was also experiencing severe drought. Arizona's snowmelt season is characterized by multiple accumulation periods and near complete melt off periods that often occur during midwinter. Successful simulation of the streamflow would necessitate defining the proper values and patterns of the SRM parameters and assessing how this parameterization differs from other basins where the SRM has been run.
Correlation coefficient values for modeled and measured streamflow on the Salt, Tonto, and Verde basins were 0.89, 0.89, and 0.91, respectively. Index of agreement values were 0.93, 0.94, and 0.95, respectively. Runoff coefficients increased during the snowmelt season until the end of March and beginning of April. Coefficients had a more typical behavior for the remainder of the season as they decreased through June. The magnitude of the runoff coefficients was relatively low due to the dry atmosphere and drought conditions. Degree-day factors for all basins were constant. The x and y parameters associated with the recession coefficients had the effect of increasing the slope of the recession limb of the hydrograph.