Measurement Flashcards

1
Q

Non-recording rainfall gauge (Hellmann)

A

 Collector (1 m above ground, opening 200 cm2, no heating)

 observation period 1 day (DWD: 7.30 previous day - 7.30 CET)

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2
Q

Recording rainfall gauge (Hellmann)

A

 Collector with registration (opening: 1 m, 200 cm2)

 observation continuously analog (charts → digitizing required)

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3
Q

Digitally recording gauges

A

 drop counter, tipping bucket or scale (opening: 1 m, 200 cm2)

 obs. continuously digital (digital storage, remote transmission)

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4
Q

Radar rainfall observation

A

 Radar reflectivity Z estimated from receiving power

 Z-R-relationship required for estimation of rainfall

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5
Q

Measurement errors for point observations :

Always underestimation of rainfall:

A
  1. Wind induced error
  2. Losses from surface wetting
  3. Evaporation from collectors

Magnitude of errors:

  • 10 - 20 % for rainfall
  • about 25 % for snow
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6
Q

Methods for correction of systematic error:

A
  • 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)
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7
Q

When do we have to correct ?

A
  1. Water balance, continuous modelling → correction always required !
  2. Extremes, event based modelling → correction not mandatory !
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