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● 御鍋砂防堰堤 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 7 km hrr.mlit.go.jp
● 三ツ又合流点 9 km hrr.mlit.go.jp
● 石川土木 大日川 別宮 10 km kasen.pref.ishikawa.jp
Dati: ICON, DWD (risoluzione 13 km)
Aggiornato: 00:00 UTC (prossimo aggiornamento: 06:00 UTC - in preparazione)
Ora corrente: 08:00, 11/04/2025 (UTC)
For this output data, temperature is shown for 2 m sopra il suolo. 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.