Assessment of soil-based and calibrated parameters of the Sacramento model and parameter transferability
The Sacramento Model (SAC-SMA) was calibrated to 12 Model Parameter Estimation Experiment (MOPEX) river basins using a combination of manual and automatic (SCE-UA) calibration. Two sets of parameters were developed for each basin: those based on calibration (CAB) and those derived from soil-based al...
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| Published in | Journal of hydrology (Amsterdam) Vol. 320; no. 1; pp. 117 - 131 |
|---|---|
| Main Authors | , |
| Format | Journal Article |
| Language | English |
| Published |
Elsevier B.V
30.03.2006
|
| Subjects | |
| Online Access | Get full text |
| ISSN | 0022-1694 1879-2707 |
| DOI | 10.1016/j.jhydrol.2005.07.008 |
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| Abstract | The Sacramento Model (SAC-SMA) was calibrated to 12 Model Parameter Estimation Experiment (MOPEX) river basins using a combination of manual and automatic (SCE-UA) calibration. Two sets of parameters were developed for each basin: those based on calibration (CAB) and those derived from soil-based algorithms (SoiB). Split-sample tests (20 years for calibration and 19 years for Testing or validation) of simulated hydrographs using CAB based parameters and SoiB based parameters were made to judge model effectiveness. Generally, simulations based on CAB parameters were superior to SoiB based simulations, though neither was satisfactory. To test for calibrated model parameter transferability, CAB parameters of each MOPEX basin were applied to the other 11 river basins (IntCAB). In terms of Bias the 144 sets of IntCAB results obtained were similar to SoiB parameters, but slightly inferior in terms of the Nash–Sutcliffe coefficient (
E
f). In an attempt to enhance parameter transferability, CAB parameters of basin
j applied to basin
i were re-scaled (IntCABSoiB), but the end results were similar to IntCAB, except the Bias statistics were marginally improved. Finally, IntCAB results in terms of the median
E
f were regressed against basin simple hydrologic similarity measures computed in terms of the median Euclidean distance derived from: (a) three annual water budget measures (HED1, HED2, HED3), (b) monthly greenness fractions (GFED), and (c) physical arc distance (ArcDist). A simple regression between the median
E
f and the median HED1, HED2, HED3 has a
R
2 of 0.5, 0.48, and 0.47, respectively, which shows that HED is a limited indicator of hydrologic similarity.
R
2 drops to about 0.3 when GFED is used to represent the hydrologic similarity. There was no predictive relationship between the median
E
f and the median ArcDist. |
|---|---|
| AbstractList | The Sacramento Model (SAC-SMA) was calibrated to 12 Model Parameter Estimation Experiment (MOPEX) river basins using a combination of manual and automatic (SCE-UA) calibration. Two sets of parameters were developed for each basin: those based on calibration (CAB) and those derived from soil-based algorithms (SoiB). Split-sample tests (20 years for calibration and 19 years for Testing or validation) of simulated hydrographs using CAB based parameters and SoiB based parameters were made to judge model effectiveness. Generally, simulations based on CAB parameters were superior to SoiB based simulations, though neither was satisfactory. To test for calibrated model parameter transferability, CAB parameters of each MOPEX basin were applied to the other 11 river basins (IntCAB). In terms of Bias the 144 sets of IntCAB results obtained were similar to SoiB parameters, but slightly inferior in terms of the Nash-Sutcliffe coefficient (E(f)). In an attempt to enhance parameter transferability, CAB parameters of basin j applied to basin i were re-scaled (IntCABSoiB), but the end results were similar to IntCAB, except the Bias statistics were marginally improved. Finally, IntCAB results in terms of the median E(f) were regressed against basin simple hydrologic similarity measures computed in terms of the median Euclidean distance derived from: (a) three annual water budget measures (HED1, HED2, HED3), (b) monthly greenness fractions (GFED), and (c) physical arc distance (ArcDist). A simple regression between the median E(f) and the median HED1, HED2, HED3 has a R2 of 0.5, 0.48, and 0.47, respectively, which shows that HED is a limited indicator of hydrologic similarity. R2 drops to about 0.3 when GFED is used to represent the hydrologic similarity. There was no predictive relationship between the median E(f) and the median ArcDist. The Sacramento Model (SAC-SMA) was calibrated to 12 Model Parameter Estimation Experiment (MOPEX) river basins using a combination of manual and automatic (SCE-UA) calibration. Two sets of parameters were developed for each basin: those based on calibration (CAB) and those derived from soil-based algorithms (SoiB). Split-sample tests (20 years for calibration and 19 years for Testing or validation) of simulated hydrographs using CAB based parameters and SoiB based parameters were made to judge model effectiveness. Generally, simulations based on CAB parameters were superior to SoiB based simulations, though neither was satisfactory. To test for calibrated model parameter transferability, CAB parameters of each MOPEX basin were applied to the other 11 river basins (IntCAB). In terms of Bias the 144 sets of IntCAB results obtained were similar to SoiB parameters, but slightly inferior in terms of the Nash-Sutcliffe coefficient (Ef). In an attempt to enhance parameter transferability, CAB parameters of basin j applied to basin i were re-scaled (IntCABSoiB), but the end results were similar to IntCAB, except the Bias statistics were marginally improved. Finally, IntCAB results in terms of the median Ef were regressed against basin simple hydrologic similarity measures computed in terms of the median Euclidean distance derived from: (a) three annual water budget measures (HED1, HED2, HED3), (b) monthly greenness fractions (GFED), and (c) physical arc distance (ArcDist). A simple regression between the median Ef and the median HED1, HED2, HED3 has a R2of 0DDT5, 0DDT48, and 0DDT47, respectively, which shows that HED is a limited indicator of hydrologic similarity. R2drops to about 0DDT3 when GFED is used to represent the hydrologic similarity. There was no predictive relationship between the median Ef and the median ArcDist. The Sacramento Model (SAC-SMA) was calibrated to 12 Model Parameter Estimation Experiment (MOPEX) river basins using a combination of manual and automatic (SCE-UA) calibration. Two sets of parameters were developed for each basin: those based on calibration (CAB) and those derived from soil-based algorithms (SoiB). Split-sample tests (20 years for calibration and 19 years for Testing or validation) of simulated hydrographs using CAB based parameters and SoiB based parameters were made to judge model effectiveness. Generally, simulations based on CAB parameters were superior to SoiB based simulations, though neither was satisfactory. To test for calibrated model parameter transferability, CAB parameters of each MOPEX basin were applied to the other 11 river basins (IntCAB). In terms of Bias the 144 sets of IntCAB results obtained were similar to SoiB parameters, but slightly inferior in terms of the Nash-Sutcliffe coefficient (Ef). In an attempt to enhance parameter transferability, CAB parameters of basin j applied to basin i were re-scaled (IntCABSoiB), but the end results were similar to IntCAB, except the Bias statistics were marginally improved. Finally, IntCAB results in terms of the median Ef were regressed against basin simple hydrologic similarity measures computed in terms of the median Euclidean distance derived from: (a) three annual water budget measures (HED1, HED2, HED3), (b) monthly greenness fractions (GFED), and (c) physical arc distance (ArcDist). A simple regression between the median Ef and the median HED1, HED2, HED3 has a R(2)of 0*5,0*48, and 0*47, respectively, which shows that HED is a limited indicator of hydrologic similarity. R(2)drops to about 0*3 when GFED is used to represent the hydrologic similarity. There was no predictive relationship between the median Ef and the median ArcDist. The Sacramento Model (SAC-SMA) was calibrated to 12 Model Parameter Estimation Experiment (MOPEX) river basins using a combination of manual and automatic (SCE-UA) calibration. Two sets of parameters were developed for each basin: those based on calibration (CAB) and those derived from soil-based algorithms (SoiB). Split-sample tests (20 years for calibration and 19 years for Testing or validation) of simulated hydrographs using CAB based parameters and SoiB based parameters were made to judge model effectiveness. Generally, simulations based on CAB parameters were superior to SoiB based simulations, though neither was satisfactory. To test for calibrated model parameter transferability, CAB parameters of each MOPEX basin were applied to the other 11 river basins (IntCAB). In terms of Bias the 144 sets of IntCAB results obtained were similar to SoiB parameters, but slightly inferior in terms of the Nash–Sutcliffe coefficient ( E f). In an attempt to enhance parameter transferability, CAB parameters of basin j applied to basin i were re-scaled (IntCABSoiB), but the end results were similar to IntCAB, except the Bias statistics were marginally improved. Finally, IntCAB results in terms of the median E f were regressed against basin simple hydrologic similarity measures computed in terms of the median Euclidean distance derived from: (a) three annual water budget measures (HED1, HED2, HED3), (b) monthly greenness fractions (GFED), and (c) physical arc distance (ArcDist). A simple regression between the median E f and the median HED1, HED2, HED3 has a R 2 of 0.5, 0.48, and 0.47, respectively, which shows that HED is a limited indicator of hydrologic similarity. R 2 drops to about 0.3 when GFED is used to represent the hydrologic similarity. There was no predictive relationship between the median E f and the median ArcDist. The Sacramento Model (SAC-SMA) was calibrated to 12 Model Parameter Estimation Experiment (MOPEX) river basins using a combination of manual and automatic (SCE-UA) calibration. Two sets of parameters were developed for each basin: those based on calibration (CAB) and those derived from soil-based algorithms (SoiB). Split-sample tests (20 years for calibration and 19 years for Testing or validation) of simulated hydrographs using CAB based parameters and SoiB based parameters were made to judge model effectiveness. Generally, simulations based on CAB parameters were superior to SoiB based simulations, though neither was satisfactory. To test for calibrated model parameter transferability, CAB parameters of each MOPEX basin were applied to the other 11 river basins (IntCAB). In terms of Bias the 144 sets of IntCAB results obtained were similar to SoiB parameters, but slightly inferior in terms of the Nash- Sutcliffe coefficient (E sub(f)). In an attempt to enhance parameter transferability, CAB parameters of basin j applied to basin i were re- scaled (IntCABSoiB), but the end results were similar to IntCAB, except the Bias statistics were marginally improved. Finally, IntCAB results in terms of the median E sub(f) were regressed against basin simple hydrologic similarity measures computed in terms of the median Euclidean distance derived from: (a) three annual water budget measures (HED1, HED2, HED3), (b) monthly greenness fractions (GFED), and (c) physical arc distance (ArcDist). A simple regression between the median E sub(f) and the median HED1, HED2, HED3 has a R super(2) of 0.5, 0.48, and 0.47, respectively, which shows that HED is a limited indicator of hydrologic similarity. R super(2) drops to about 0.3 when GFED is used to represent the hydrologic similarity. There was no predictive relationship between the median E sub(f) and the median ArcDist. |
| Author | Gan, Thian Yew Burges, Stephen J. |
| Author_xml | – sequence: 1 givenname: Thian Yew surname: Gan fullname: Gan, Thian Yew email: tgan@ualberta.ca organization: Department of Civil and Environmental Engineering, University of Alberta, Edmonton, AB, Canada T6G 2G7 – sequence: 2 givenname: Stephen J. surname: Burges fullname: Burges, Stephen J. email: sbsurges@u.washington.edu organization: Department of Civil and Environmental Engineering, University of Washington, Seattle, WA 98195-2700, USA |
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| Keywords | Hydrologic similarity MOPEX (Model Parameter Estimation Experiment) Sacramento rainfall-runoff model (SAC-SMA) Calibrated (CAB) and Soil-based (SoiB) parameters Parameter transferability Euclidean distance |
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| Title | Assessment of soil-based and calibrated parameters of the Sacramento model and parameter transferability |
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