Nowcasting in meteorology uses surface
weather station data,
wind profiler data, and any other weather data available to initialize the current weather situation and forecast by extrapolation for a period of 0 to 6 hours. In this time range it is possible to forecast small features such as individual storms with reasonable accuracy.
Weather radar echoes and satellite data, giving cloud coverage, are particularly important in nowcasting because they are very detailed and pick out the size, shape, intensity, speed and direction of movement of individual features of weather on a continuous basis and a vastly better resolution than surface weather stations. But with the development of mesoscale numerical weather models, these information can be ingested into an
expert system to produce a much better forecast combining
numerical weather prediction and local effects not normally possible to be known beforehand. Different research groups, public and private, have developed such programs. For instance, the French weather service,
Météo-France, is using a software, named
ASPIC to extrapolate to a fine scale the areas of precipitation. Other examples are
AutoNowcaster which has been developed by
UCAR to predict short term motion and evolution of thunderstorms,
3D nowcasting an experimental technology by the RIKEN Advanced Institute for Computational Science and private firms like
Tomorrow.io (formerly ClimaCell) using its proprietary HyperCast software for nowcasting precipitation type and intensity at 300-500 m geospatial resolution. == Usage ==