| Mjesto | Skansbron - Prognoza |
| Pruža | trafikverket.se |
| Smjer | jug |
● Sicklalänken Ö 2 km trafikverket.se
● Danvikstull 2 km trafikverket.se
● Tpl Sofielundsplan 2 km trafikverket.se
● Tpl Lugnet 2 km trafikverket.se
● Tpl Sickla mot Nacka 2 km trafikverket.se
● Sockenvägen 3 km trafikverket.se
Podaci: ICON, DWD (razlučivost 7 km)
Ažurirani: 09:00 UTC (sljedeće ažuriranje: 12:00 UTC - pripremi)
Vrijeme sad: 14:00, 21.03.2025 (UTC)
For this output data, temperature is shown for 2 m iz. nad. vis.. 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.