| Location | 荏原調節池上 - Forecast |
| Provided by | kasen-suibo.metro.tokyo.lg.jp |
● 渋谷橋 2 km kasen-suibo.metro.tokyo.lg.jp
● 青葉台 3 km kasen-suibo.metro.tokyo.lg.jp
● 田園調布(上)観測所 6 km ktr.mlit.go.jp
● 中原区 (Nakahara Ward) 6 km go.jp
● 矢川橋 7 km kasen-suibo.metro.tokyo.lg.jp
● 和田見橋 8 km kasen-suibo.metro.tokyo.lg.jp
For this output data, temperature is shown for 2 m above ground. 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.