● Sain-Bel 1 km meteo-sain-bel.fr
● Yzeron 12 km vision-environnement.com
● Anse 17 km bojolpif.com
● Anse 17 km bojolpif.com
● Mont Boussuivre 17 km meteo-rhone-loire.org
For this output data, temperature is shown for 2 m iz. nad. vis.. The calculations take into account the terrain (elevation), but with lower resolution than in reality. Therefore the models cannot differentiate, for instance, the temperature on a mountain peak or on a city square scorched by the sun. The general rule is that the centres of large cities are 1 °C to 3 °C warmer than the surrounding area or natural landscapes. Significant temperature differences over a small area are primarily caused in the winter by an inversion. A short yet noticeable cooling can also occur after a local summer storm.