● 農免大橋 3 km hrr.mlit.go.jp
● 経田橋 4 km hrr.mlit.go.jp
● 津幡土木 大海川 八野大橋 15 km kasen.pref.ishikawa.jp
● 津幡土木 宇ノ気川 文化橋 15 km kasen.pref.ishikawa.jp
● 県央土木 森下川 薬師 16 km kasen.pref.ishikawa.jp
● 高岡出張所 16 km hrr.mlit.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.