| Lokasi | Αθήνα - Λυκαβηττός - Prakiraan Cuaca |
| Diberikan oleh | uoa.gr from meteo.di.uoa.gr |
● Αθήνα - Σύνταγμα 1 km forecastweather.gr
● Αθήνα - Ακρόπολη 4 2 km uoa.gr
● Athens 3 km meteo.di.uoa.gr
● Αθήνα - Γκάζι 3 km meteo.gr
● Υμηττός 2 3 km forecastweather.gr
● Υμηττός 3 km uoa.gr
For this output data, temperature is shown for 2 m di atas tanah. 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.