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Difference between revisions of "Example figures: Quantile Q 0.01, Q 0.05, Q 0.95, Q 0.99"

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[[de:Beispielgrafiken: Quantile Q 0.01, Q 0.05, Q 0.95, Q 0.99]]
 
[[de:Beispielgrafiken: Quantile Q 0.01, Q 0.05, Q 0.95, Q 0.99]]
 
=Explanations=
 
=Explanations=
Water level value of a time series which is not exceeded by a certain percentage of all water level values.
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Water level for a time series which is not exceeded by a certain percentage of all values within the period of data analysis.
 
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* left top: result for quantile Q_0.01 (''not'' exceeded by 1 %).
* left top: value of the parameter for the quantile Q_0.01.
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* right top: result for quantile Q_0.05 (''not'' exceeded by 5 %).
* right top: value of the parameter for the quantile Q_0.05.
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* left bottom: result for quantile Q_0.95 (exceeded by 5 %).
* left bottom: value of the parameter for the quantile Q_0.95.  
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* right bottom: result for quantile Q_0.99 (exceeded by 1 %).
* right bottom: value of the parameter for the quantile Q_0.99.
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Computed for permanently flooded areas only.
  
 
=Examples=
 
=Examples=

Latest revision as of 10:41, 16 September 2014

Explanations

Water level for a time series which is not exceeded by a certain percentage of all values within the period of data analysis.

  • left top: result for quantile Q_0.01 (not exceeded by 1 %).
  • right top: result for quantile Q_0.05 (not exceeded by 5 %).
  • left bottom: result for quantile Q_0.95 (exceeded by 5 %).
  • right bottom: result for quantile Q_0.99 (exceeded by 1 %).

Computed for permanently flooded areas only.

Examples

Quantile Q_0.01 Quantile Q_0.05
Water level value of a time series below which 1% of the remaining water level values are lying.
Water level value of a time series below which 5% of the remaining water level values are lying.
Quantile Q_0.95 Quantile Q_0.99
Water level value of a time series which is not exceeded of 95% of the remaining water level values.
Water level value of a time series which is not exceeded of 99% of the remaining water level values.

Closely related quantities



back to Characteristic Numbers of Water Level (independent of tides)