Opdateret:
05/02/12 kl.
05:55
Buskelundtoften, Silkeborg
|56°10'58''N 9°30'26''Ø | Højde over havet: 75,35 meter
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Solar and UV
| Solar | UV | |
| Time 05:55 | 0 Watt/M2 | 0.0 |
| Max stay in sun (burntime) | --- minutes | |
| Today high | 0 Watt/M2 at 00:00 | 0.0 at 00:00 |
| Today low | 0.0 at 00:00 | |
| Yesterday high | 356.4 Watt/M2 at 12:16 | 0.0 at 00:00 |
| 24 hours ago | 0.0 Watt/M2 | 0.0 |
| This month high | 457.2 Watt/M2 at 1-2-2012 | 0.4 at 1-2-2012 |
| This year high | 457.2 Watt/M2 at 1-2-2012 | 1.5 at 1-1-2012 |
| ALL-TIME high | 1508.4 Watt/M2 at 13-6-2010 | 6.5 at 2-6-2011 |
| Sunshine hours today | 00:00 hours | |
| Sunshine hours - last 10 minutes | 0 hour | |
| Sunshine hours - last 60 minutes | 0 hour | |
| Sunshinehours - last hole hour | 0 hour | |
| Sunshinehour in percent of max - last 10 minutes | 0% | |
| Sunshinehour in percent of max - last 60 minutes | 0% | |
| Sunshinehours - yesterday | 04:58 timer | |
| Sunshinehours - this month | 16:56 timer |
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Javascript required Solar1hour
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Javascript required Solar24hours
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Javascript required Solar124hours
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Javascript required Solar7days
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Javascript required UV24hours
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Javascript required UV7days
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UV Forecast:
|
5 Feb 2012:
0.4 
Low |
6 Feb 2012:
0.5
Low |
7 Feb 2012:
0.5
Low |
8 Feb 2012:
0.6
Low |
9 Feb 2012:
0.6
Low |
10 Feb 2012:
0.7
Low |
11 Feb 2012:
0.7
Low |
Evapotranspiration (ET)
| Evapotranspiration (ET) is the sum of evaporation and plant transpiration. Evaporation accounts for the movement of water to the air from sources such as the soil, canopy interception, and waterbodies. Transpiration accounts for the movement of water within a plant and the subsequent loss of water as vapour through stomata in its leaves. Evapotranspiration is an important part of the water cycle. | |
| Time 05:55 | 0.0 mm |
| Total of today | 0.0 mm |
| Total yesterday | 0.2 mm |
| Total last 7 days | 1.6 mm |
| Total this month | 1.2 mm |
HUMIDITY
Humidity or relative humidity measures the amount of water vapor in the air relative to the temperature. It is important in weather because humidity affects how humans feel. A hot, humid day feels hotter because we cannot sweat as effectively. A cool, dry day feels colder because moisture evaporates more easily.
Humidity or relative humidity measures the amount of water vapor in the air relative to the temperature. It is important in weather because humidity affects how humans feel. A hot, humid day feels hotter because we cannot sweat as effectively. A cool, dry day feels colder because moisture evaporates more easily.
