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Jučer & Danas

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Visina:

Morska površina 5 cm iz. nad. vis.2 m iz. nad. vis.Anomalija, 2 m 950 hPa, 500 m 925 hPa, 750 m 900 hPa, 1000 m 850 hPa, 1500 m 800 hPa, 2000 m 750 hPa, 2500 m 700 hPa, 3000 m 650 hPa, 3600 m 600 hPa, 4200 m 500 hPa, 5500 m 300 hPa, 9000 m 200 hPa, 12000 m 10 hPa, 30000 m Nulta izoterma

Grmljavinska oluja

Snježni pokrivač

Onečišćavanje zraka

Temperatura Osjet ugode Padaline Radar Satelit Oblaci Brzina vjetra Udari vjetra Tlak zraka Grmljavinska oluja Vlaga More Snježni pokrivač Onečišćavanje zraka

Reproduciraj Natrag Dalje Promijeni datumDanas, 23.03.202500:00 01:00 02:00 03:00 04:00 05:00 06:00 07:00 08:00 09:00 10:00 11:00 12:00 13:00 14:00 15:00 16:00 17:00 18:00 19:00 20:00 21:00 22:00 23:00

po	ut	sr	če	pe	su	ne
17	18	19	20	21	22	23
24	25	26	27	28	29	30
31ožujak	01	02	03	04	05	06

ut
18. ožu
sr
19. ožu
če
20. ožu
pe
21. ožu
su
22. ožu

00:00
03:00
06:00
09:00
12:00

Model:

Animacija vjetra:

Nema Normalni Snažni Blagi Tamni Brzi

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.

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Kraków - Wawel i zakole Wisły

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