Measurement Flashcards
Non-recording rainfall gauge (Hellmann)
Collector (1 m above ground, opening 200 cm2, no heating)
observation period 1 day (DWD: 7.30 previous day - 7.30 CET)
Recording rainfall gauge (Hellmann)
Collector with registration (opening: 1 m, 200 cm2)
observation continuously analog (charts → digitizing required)
Digitally recording gauges
drop counter, tipping bucket or scale (opening: 1 m, 200 cm2)
obs. continuously digital (digital storage, remote transmission)
Radar rainfall observation
Radar reflectivity Z estimated from receiving power
Z-R-relationship required for estimation of rainfall
Measurement errors for point observations :
Always underestimation of rainfall:
- Wind induced error
- Losses from surface wetting
- Evaporation from collectors
Magnitude of errors:
- 10 - 20 % for rainfall
- about 25 % for snow
Methods for correction of systematic error:
- In Germany method acc. to Richter (1995) for daily data is often applied
[equation page 6]
- Internationally different approaches are in use, see e.g. Sevruk (2005)
When do we have to correct ?
- Water balance, continuous modelling → correction always required !
- Extremes, event based modelling → correction not mandatory !