| Lieu | 田園調布(上)観測所 - Prévisions |
| Fourni par | ktr.mlit.go.jp |
● 中原区 (Nakahara Ward) 1 km go.jp
● 矢川橋 2 km kasen-suibo.metro.tokyo.lg.jp
● 高津区 (Takatsu Ward) 4 km go.jp
● 矢上橋水位観測所 4 km ktr.mlit.go.jp
● 高津区 (Takatsu Ward) 4 km go.jp
● 戸手樋管 6 km ktr.mlit.go.jp
Données : ICON, DWD (résolution 13 km)
Mise à jour : 06:00 UTC (prochaine mise à jour : 12:00 UTC - préparé)
Heure actuelle : 16:00, 21/03/2025 (UTC)
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.