● 亀の子橋水位観測所 1 km ktr.mlit.go.jp
● 綱島水位観測所 4 km ktr.mlit.go.jp
● 矢上橋水位観測所 7 km ktr.mlit.go.jp
● 鶴見区 (Tsurumi Ward) 7 km go.jp
● 矢川橋 11 km kasen-suibo.metro.tokyo.lg.jp
● 高津区 (Takatsu Ward) 11 km go.jp
Dati: ICON, DWD (risoluzione 13 km)
Aggiornato: 00:00 UTC (prossimo aggiornamento: 06:00 UTC - in preparazione)
Ora corrente: 07:00, 31/03/2025 (UTC)
For this output data, temperature is shown for 2 m sopra il suolo. 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.