| Località | 石川土木 高橋川放水路 転倒堰 - Previsione |
| Fornitore | kasen.pref.ishikawa.jp |
● 県央土木 伏見川 山科 8 km kasen.pref.ishikawa.jp
● 県央土木 犀川 下菊橋（三ヶ用水堰） 11 km kasen.pref.ishikawa.jp
● 石川土木 大日川 別宮 11 km kasen.pref.ishikawa.jp
● 県央土木 犀川 犀川大橋（転倒堰） 12 km kasen.pref.ishikawa.jp
● 石川土木 倉部川 倉部 12 km kasen.pref.ishikawa.jp
● 金沢市(Kanazawa) 13 km go.jp
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.