| Località | 神取橋右岸22.1ｋｍ - Previsione |
| Fornitore | cam.river.go.jp from river.go.jp |
● JR佳景山駅右岸18.1ｋｍ 4 km cam.river.go.jp
● 脇谷水門左岸34.1ｋｍ 10 km cam.river.go.jp
● 上地地区右岸11.6ｋｍ 13 km cam.river.go.jp
● 小野橋4.2ｋｍ 15 km cam.river.go.jp
● 釜谷水門右岸0.8km 20 km cam.river.go.jp
● 大郷大橋左岸17.5ｋｍ 20 km cam.river.go.jp
For this output data, temperature is shown for 2 m sopra il suolo. 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.