Most energy models use the temperature reported at the nearest airport. That number is measured, on purpose, in a way that ignores sunlight, hot pavement, and the heat a city stores from one day to the next. This post walks through the physics, uses open satellite and backyard-weather-station data to measure how far Phoenix neighborhoods drift from the airport, and compares spatial models (H3 hex bins, Gaussian processes, gradient boosting) for turning a free day-ahead forecast and historical satellite readings into the surface, radiant, and operative temperatures a home actually experiences.