最近的網絡攝像頭
● 田園調布(上)観測所 1 km ktr.mlit.go.jp
● 矢川橋 3 km kasen-suibo.metro.tokyo.lg.jp
● 矢上橋水位観測所 4 km ktr.mlit.go.jp
● 戸手樋管 5 km ktr.mlit.go.jp
● 高津区 (Takatsu Ward) 5 km go.jp
● 戸手船着場 6 km ktr.mlit.go.jp
● 田園調布(上)観測所 1 km ktr.mlit.go.jp
● 矢川橋 3 km kasen-suibo.metro.tokyo.lg.jp
● 矢上橋水位観測所 4 km ktr.mlit.go.jp
● 戸手樋管 5 km ktr.mlit.go.jp
● 高津区 (Takatsu Ward) 5 km go.jp
● 戸手船着場 6 km ktr.mlit.go.jp
資料: ICON, DWD (解析度13 km)
更新 12:00 UTC (下一次更新: 18:00 UTC - 準備)
當前時間: 22:00, 2025-04-12 (UTC)
For this output data, temperature is shown for 地面2公尺. 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.