● 金沢市(Kanazawa) 3 km go.jp
● 県央土木 森下川 薬師 3 km kasen.pref.ishikawa.jp
● 県央土木 犀川 犀川大橋（転倒堰） 4 km kasen.pref.ishikawa.jp
● 県央土木 犀川 下菊橋（三ヶ用水堰） 4 km kasen.pref.ishikawa.jp
● 県央土木 大野川 機具橋 7 km kasen.pref.ishikawa.jp
● 県央土木 伏見川 山科 7 km kasen.pref.ishikawa.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.