For many years government agencies, such as the United States Geological Survey and the National Weather Service, have used rules of thumb to predict when snowmelt would begin to impact area creeks and rivers. Specifically, daytime maximum temperatures in the valleys (1500-1800 m MSL) have long been used to predict the onset of snowmelt runoff. Additionally, minimum temperatures at mountain locations (2400-2900 m MSL) have provided indications of active overnight melting within this prime snowpack region. A comprehensive review of air temperature and SWEs from numerous observing stations in the basins and mountains was conducted to validate the merit of these rules of thumb. Improved correlations between temperature and snowmelt onset, amount, and timing will assist Wyoming hydrologists and forecasters in future years. Of particular interest is improving the ability to forecast anomalous runoff seasons that result during extreme climatological winter patterns.