2008
DOI: 10.3133/sir20085013
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Hydrologic and water-quality characterization and modeling of the Onondaga Lake Basin, Onondaga County, New York

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Cited by 7 publications
(13 citation statements)
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“…During the model development, a number of assumptions and simplifications were made to simplify complex hydrological processes which can contribute to have increased errors in the model output. According to Coon and Reddy [83], errors in a hydrological model can arise from various sources including: (i) errors in precipitation and streamflow data; (ii) limitations in model structure; (iii) errors in model calibration; (iv) inaccurate estimation and interpretation of land-use and land-cover data; and (v) changes in land-use during the simulation period. While developing the model, the precipitation data used were obtained from point-based rainfall gauge stations and then applied uniformly over a specified area around the gauging stations defined by the Thiessen-polygon method.…”
Section: Modelling Errors Limitations and Future Directionsmentioning
confidence: 99%
“…During the model development, a number of assumptions and simplifications were made to simplify complex hydrological processes which can contribute to have increased errors in the model output. According to Coon and Reddy [83], errors in a hydrological model can arise from various sources including: (i) errors in precipitation and streamflow data; (ii) limitations in model structure; (iii) errors in model calibration; (iv) inaccurate estimation and interpretation of land-use and land-cover data; and (v) changes in land-use during the simulation period. While developing the model, the precipitation data used were obtained from point-based rainfall gauge stations and then applied uniformly over a specified area around the gauging stations defined by the Thiessen-polygon method.…”
Section: Modelling Errors Limitations and Future Directionsmentioning
confidence: 99%
“…Onondaga Creek has the second largest drainage area (298 km 2 ) in the Onondaga Lake watershed and contributes the greatest surface water inflow. The creek is approximately 26.7 mi (43 km) in length and descends more than 0.19 mi (0.30 km) from its headwaters [17]. Land use is predominantly forest (50%) and agriculture (31%), with approximately 19% considered developed [18].…”
Section: Study Sitementioning
confidence: 99%
“…Uncertainties in hydrological models include (i) errors and limitations in input datasets, (ii) parameterization or assumptions in the model, (iii) calibration errors, (iv) land classification/cover errors, and (v) catchment scale/transfer errors (Coon and Reddy 2008). It has also been noted that when dealing with precipitation and hydrology, a deterministic forecast gives the user an “illusion of certainty” whereas a probabilistic system inherently accounts for uncertainty.…”
Section: Uncertaintymentioning
confidence: 99%