| Mjesto | 石川土木 安産川 分流堰 - Prognoza |
| Pruža | kasen.pref.ishikawa.jp |
● 湊町 2 km hrr.mlit.go.jp
● 松任海岸小川地区 4 km hrr.mlit.go.jp
● 石川土木 倉部川 倉部 9 km kasen.pref.ishikawa.jp
● 石川土木 高橋川放水路 転倒堰 12 km kasen.pref.ishikawa.jp
● 県央土木 犀川 示野橋 14 km kasen.pref.ishikawa.jp
● 県央土木 伏見川 山科 14 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.