The document summarizes research estimating water surface temperature in Devils Lake, North Dakota using the split window algorithm with Landsat 8 thermal infrared bands. The algorithm uses brightness temperature from the bands and coefficients accounting for atmospheric effects to calculate surface temperature. The estimates were validated against buoy observations and hydrodynamic models of the lake, with calibrated streamflow and hourly water temperature simulations showing good agreement to field data. Satellite imagery provides spatially detailed skin temperature estimates while models offer higher temporal resolution and temperature profiles.