| Mjesto | 石川土木 倉部川 倉部 - Prognoza |
| Pruža | kasen.pref.ishikawa.jp |
● 松任海岸小川地区 5 km hrr.mlit.go.jp
● 県央土木 犀川 示野橋 5 km 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 犀川大橋（転倒堰） 8 km kasen.pref.ishikawa.jp
● 石川土木 安産川 分流堰 9 km kasen.pref.ishikawa.jp
● 金沢市(Kanazawa) 9 km go.jp
For this output data, temperature is shown for 2 m iz. nad. vis.. 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.