| Lieu | 亀の子橋水位観測所 - Prévisions |
| Fourni par | ktr.mlit.go.jp |
● 小机大橋水位観測所 1 km ktr.mlit.go.jp
● 綱島水位観測所 3 km ktr.mlit.go.jp
● 矢上橋水位観測所 6 km ktr.mlit.go.jp
● 鶴見区 (Tsurumi Ward) 6 km go.jp
● 戸手船着場 8 km ktr.mlit.go.jp
● 中原区 (Nakahara Ward) 9 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.