● 戸手樋管 1 km ktr.mlit.go.jp
● 鶴見区 (Tsurumi Ward) 3 km go.jp
● 矢上橋水位観測所 4 km ktr.mlit.go.jp
● 綱島水位観測所 6 km ktr.mlit.go.jp
● 中原区 (Nakahara Ward) 6 km go.jp
● 田園調布(上)観測所 6 km ktr.mlit.go.jp
Data: ICON, DWD (resolution 13 km)
Updated: 12:00 UTC (next update: 18:00 UTC - prepare)
Current time: 21:00, 2025/03/24 (UTC)
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.