● Il y a 53 minutes
| Lieu | 紅葉谷 - Prévisions |
| Fourni par | seishiga.kkr.mlit.go.jp |
Hier & Aujourd'hui
Comparaison de l'image de la dernière heure disponible (à droite) avec l'image d'il y a 24 heures (à gauche).
| Lieu | 紅葉谷 - Prévisions |
| Fourni par | seishiga.kkr.mlit.go.jp |
Données : ICON, DWD (résolution 13 km)
Mise à jour : 18:00 UTC (prochaine mise à jour : 00:00 UTC - préparé)
Heure actuelle : 02:00, 01/04/2025 (UTC)
For this output data, temperature is shown for 2 m au-dessus du sol. 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.