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Published online 8 March 2006
Published in Vadose Zone J 5:248-260 (2006)
DOI: 10.2136/vzj2005.0025
© 2006 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Right arrow Watershed and Landscape Processes
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Automatic Calibration and Predictive Uncertainty Analysis of a Semidistributed Watershed Model

Zhulu Lin* and David E. Radcliffe

Dep. of Crop and Soil Sciences, Univ. of Georgia, Athens, GA 30602

Figure 1
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  		Fig. 1. Upper Etowah River basin with the solid dot indicating the watershed outlet at Canton, GA.

 

Figure 2
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  		Fig. 2. Daily precipitation (dashed line) and stream flow observations (solid dot) at Canton, GA (1983–2001).

 

Figure 3
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  		Fig. 3. Observed and modeled stream discharge at Canton, GA during the calibration period (1983–1992): (a) 1-yr daily flow (1987), (b) monthly flow volume, and (c) exceedance fractions.

 

Figure 4
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  		Fig. 4. Observed and modeled stream discharge at Canton, GA during the validation period (1993–2001): (a) 1-r daily flow (1995), (b) monthly flow volume, and (c) exceedance fractions.

 

Figure 5
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  		Fig. 5. Observations (solid dot) and model-generated stream flows from predictive uncertainty analysis (thin solid lines) during calibration period (a) 1-yr daily flow (1987), (b) monthly flow volume, (c) exceedance fractions.

 




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