Summary
Fog and low stratus can have a significant impact on aviation operations through reduced ceiling and visibilities. Satellite imagery and products are very effective tools for detecting the presence of low clouds and fog, determining their aeral coverage, and monitoring their evolution. This is especially true of radiation fog, where the fog area tends to dissipate from the edges inward with daytime heating.
Since satellites look down on clouds, it is hard to distinguish areas of low cloud from fog (which starts at ground level). Therefore, it is vital to use all of your weather data and integrate satellite information with surface and upper air observations to determine where fog may actually be occurring.
Satellite and other observational data are vital tools for evaluating NWP guidance. Based on how the models initialize, you may need to adjust the model forecast before writing the details of your aviation forecast.
