| Lieu | 津幡土木 河北潟放水路 大根布防潮水門 - Prévisions |
| Fourni par | kasen.pref.ishikawa.jp |
● 県央土木 大野川 機具橋 4 km kasen.pref.ishikawa.jp
● 津幡土木 宇ノ気川 文化橋 8 km kasen.pref.ishikawa.jp
● 県央土木 森下川 薬師 9 km kasen.pref.ishikawa.jp
● 春日山 10 km go.jp
● 県央土木 犀川 示野橋 10 km kasen.pref.ishikawa.jp
● 金沢市(Kanazawa) 10 km go.jp
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.