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Estimating the unit hydrograph and effective rainfall from observed output
Barry Croke
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Engineering
Response Curve
100%
Response Function
100%
Deconvolution
100%
Impulse Response
100%
Model Structure
50%
Temporal Variation
50%
Drying Method
50%
Forward Approach
50%
Earth and Planetary Sciences
Streamflow
100%
Unit Hydrograph
100%
Deconvolution
40%
Temporal Variation
20%
Autocorrelation
20%
Potential Evapotranspiration
20%