● 下流女原 2 km hrr.mlit.go.jp
● 瀬戸砂防堰堤 2 km hrr.mlit.go.jp
● 尾添川第1号砂防堰堤 3 km hrr.mlit.go.jp
● 猿花上流砂防堰堤 6 km hrr.mlit.go.jp
● 白山ブナオ山の動物たち 6 km sizenken.biodic.go.jp
● 三ツ又合流点 8 km hrr.mlit.go.jp
Données : ICON, DWD (résolution 13 km)
Mise à jour : 06:00 UTC (prochaine mise à jour : 12:00 UTC - préparé)
Heure actuelle : 12:00, 30/03/2025 (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.