最近的網絡攝像頭
● 青葉台 2 km kasen-suibo.metro.tokyo.lg.jp
● 荏原調節池上 2 km kasen-suibo.metro.tokyo.lg.jp
● 和田見橋 6 km kasen-suibo.metro.tokyo.lg.jp
● 南小滝橋 7 km kasen-suibo.metro.tokyo.lg.jp
● 田園調布(上)観測所 8 km ktr.mlit.go.jp
● 中原区 (Nakahara Ward) 8 km go.jp
● 青葉台 2 km kasen-suibo.metro.tokyo.lg.jp
● 荏原調節池上 2 km kasen-suibo.metro.tokyo.lg.jp
● 和田見橋 6 km kasen-suibo.metro.tokyo.lg.jp
● 南小滝橋 7 km kasen-suibo.metro.tokyo.lg.jp
● 田園調布(上)観測所 8 km ktr.mlit.go.jp
● 中原区 (Nakahara Ward) 8 km go.jp
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.