See the global technology behind tomorrow's weather map.
Forecasting begins with measurements from the entire atmosphere. Computers combine observations with physical equations to estimate the current state, then calculate how conditions may evolve.




Surface stations measure temperature, pressure, humidity, wind, and precipitation.
Learn MoreRadiosondes rise through the atmosphere beneath balloons.
Learn MoreWeather satellites observe clouds, temperature, moisture, fires, ice, oceans, and storms.
Learn MoreWeather radar sends radio waves and measures echoes from precipitation.
Learn MoreForecast models solve equations describing atmosphere and oceans.
Learn MoreEnsemble forecasts run models many times with slightly different starting conditions.
Learn MoreHuman forecasters interpret model guidance and local conditions.
Learn MoreForecast skill decreases with time.
Learn MoreNetworks of stations provide continuous local observations.
They measure temperature, moisture, pressure, and wind from the surface into the stratosphere.
Geostationary satellites repeatedly view the same region, while polar orbiters scan the whole planet.
Doppler radar also measures motion toward or away from the radar.
Different models use different resolution, physics, and data-assimilation methods.
The spread helps estimate forecast uncertainty.
Experience matters especially for terrain, coastlines, convection, and rapidly changing hazards.
The atmosphere is chaotic, so tiny initial uncertainties can grow into larger differences days later.