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● Lyžařský areál Struhy 1 km klturnov.cz
● Lyžařský areál Struhy 1 km klturnov.cz
● Letiště Všeň 6 km vetromerka.cz
● Malá Skála 6 km ms-free.net
● Hrubá Skála 6 km pension-jana.cz
● Koberovy 7 km koberovy.cz
● Lyžařský areál Struhy 1 km klturnov.cz
● Lyžařský areál Struhy 1 km klturnov.cz
● Letiště Všeň 6 km vetromerka.cz
● Malá Skála 6 km ms-free.net
● Hrubá Skála 6 km pension-jana.cz
● Koberovy 7 km koberovy.cz
Podaci: ICON, DWD (razlučivost 7 km)
Ažurirani: 09:00 UTC (sljedeće ažuriranje: 12:00 UTC - pripremi)
Vrijeme sad: 15:00, 14.04.2025 (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.