Difference between revisions of "Climatic measurements"
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The climate is the driver for hydorlogical systems. A typical climate station measures the following parameters: | The climate is the driver for hydorlogical systems. A typical climate station measures the following parameters: | ||
| − | == | + | ==Air temperature== |
==Radiation== | ==Radiation== | ||
| + | Can be distinguished into incoming radiation and reflected radiation, the difference beeing the [[Net Radiation - Net Radiometer %28NR-Lite%29|net radiation]] | ||
| + | |||
| + | For each type, the part of the electromagnetic spectrum can be further distinguished (VIS, NIR and/or FIR) | ||
| + | |||
| + | For a hydrological climate station the net radiation (VIS and the IR) is important (For calcultaion of the evapotranspiration). | ||
==Wind== | ==Wind== | ||
| Line 12: | Line 17: | ||
==Humidity== | ==Humidity== | ||
| − | ==Sunshine== | + | ==Air Pressure== |
| + | |||
| + | ==Sunshine hour== | ||
| + | |||
| + | ==Soil temperature== | ||
==Problems/Questions:== | ==Problems/Questions:== | ||
Latest revision as of 11:22, 10 August 2007
Purpose:
The climate is the driver for hydorlogical systems. A typical climate station measures the following parameters:
Air temperature
Radiation
Can be distinguished into incoming radiation and reflected radiation, the difference beeing the net radiation
For each type, the part of the electromagnetic spectrum can be further distinguished (VIS, NIR and/or FIR)
For a hydrological climate station the net radiation (VIS and the IR) is important (For calcultaion of the evapotranspiration).