|
10.5 °C |
Vjetar 27 km/h |
Padaline (1 sat) | 0 mm |
Vlaga | 48 % |
Tlak zraka | 1012 hPa |
Snježni pokrivač | 0 cm |
Vidljivost | 6 km |
Oblaci | 50 % |
Oblačni sloj | 1432 m |
Vremenska prognoza sa stanice Toulouse/blagnac, Udaljenost: 6 km (14:00 15.03.2025)
15:00 | 16:00 | 17:00 | 18:00 | 19:00 | 20:00 | 21:00 | 22:00 | 23:00 | 00:00 sutra | 01:00 sutra | 02:00 sutra | 03:00 sutra | 04:00 sutra | 05:00 sutra | 06:00 sutra | 07:00 sutra | 08:00 sutra | 09:00 sutra | 10:00 sutra | 11:00 sutra | 12:00 sutra | 13:00 sutra | 14:00 sutra | 15:00 sutra |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
9 °C
0 mm20 % SZ
19 km/h
Udari:
43 km/h |
9 °C
0.1 mm60 % SZ
17 km/h
Udari:
43 km/h |
8 °C
0 mm30 % SZ
17 km/h
Udari:
43 km/h |
8 °C
0 mm10 % SZ
16 km/h
|
6 °C
0 mm0 % SZ
11 km/h
|
5 °C
0 mm0 % SZ
6 km/h
|
4 °C
0 mm10 % Z
5 km/h
|
4 °C
0 mm10 % Z
5 km/h
|
3 °C
0 mm0 % JZ
6 km/h
|
3 °C
0 mm0 % JZ
6 km/h
|
3 °C
0 mm10 % Z
5 km/h
|
2 °C
0 mm0 % Z
5 km/h
|
2 °C
0 mm0 % Z
5 km/h
|
2 °C
0 mm0 % Z
3 km/h
|
1 °C
0 mm0 % Z
3 km/h
|
1 °C
0 mm0 % JZ
1 km/h
|
1 °C
0 mm0 % J
3 km/h
|
1 °C
0 mm0 % JZ
1 km/h
|
2 °C
0 mm0 % JZ
1 km/h
|
5 °C
0 mm10 % Z
5 km/h
|
7 °C
0 mm10 % Z
5 km/h
|
8 °C
0 mm10 % SZ
6 km/h
|
9 °C
0 mm10 % SZ
6 km/h
|
10 °C
0 mm10 % SZ
6 km/h
|
10 °C
0 mm10 % SZ
4 km/h
|
01:00 | 04:00 | 07:00 | 10:00 | 13:00 | 16:00 | 19:00 | 22:00 |
---|---|---|---|---|---|---|---|
3 °C
0 mm10 % Z
5 km/h
|
2 °C
0 mm0 % Z
3 km/h
|
1 °C
0 mm0 % J
3 km/h
|
5 °C
0 mm10 % Z
5 km/h
|
9 °C
0 mm10 % SZ
6 km/h
|
10 °C
0 mm10 % SZ
6 km/h
|
8 °C
0 mm10 % SI
7 km/h
|
5 °C
0 mm0 % I
3 km/h
|
25 |
20 |
15 |
10 |
5 |
0 |
-5 |
su 15 | ne 16 | po 17 | ut 18 | sr 19 | če 20 | pe 21 | su 22 | ne 23 | po 24 | ut 25 | sr 26 | če 27 | pe 28 |
Air quality index (marked as AQI) is developed by Environmental Protection Agency. Values over 300 represents hazardous air quality, between 200-300 very unhealthy, 150-200 unhealthy, 100-150 unhealthy for sensitive groups and below 100 or rather below 50 the air quality is good.
Kretanje: ↓jug | Vrijeme: 15.03.2025 14:00 |
Faza: dan | Visina: +43 ° |
Kretanje: ↓sjever | Vrijeme: 15.03.2025 14:00 |
Osvjetljenje: 98 % | Visina: −51 ° |
Datum | izlazak | zalazak | izlazak | Osvjetljenje |
15.03.2025 | — | 07:30 | 20:25 | 99 % do 97 % |
16.03.2025 | — | 07:46 | 21:28 | 97 % do 93 % |
17.03.2025 | — | 08:05 | 22:32 | 93 % do 88 % |
18.03.2025 | — | 08:26 | 23:38 | 87 % do 81 % |
19.03.2025 | — | 08:51 | — | 81 % do 73 % |
Faza 15.03.2025 | Vrijeme | Duljina |
noć | 00:00 do 05:32 | 5 sat 32 min. |
astronomski sumrak | 05:32 do 06:06 | 34 min. |
nautički sumrak | 06:06 do 06:39 | 33 min. |
civilni sumrak | 06:39 do 07:07 | 29 min. |
dan | 07:07 do 19:01 | 11 sat 53 min. |
civilni sumrak | 19:01 do 19:29 | 29 min. |
nautički sumrak | 19:29 do 20:03 | 33 min. |
astronomski sumrak | 20:03 do 20:36 | 34 min. |
noć | 20:36 do 00:00 | 3 sat 23 min. |
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.