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Verification of a one-dimensional, unsteady-flow model for the Fox River in Illinois
The previously-calibrated application of the Full EQuations (FEQ) model of one-dimensional, unsteady flow to a 30.7-mile reach of the Fox River in northeastern Illinois was verified with discharge, stage, and dye-transport data collected during a 12-day period in October-November 1990. The period included unsteady flow induced by the operation of a sluice gate dam located at the upstream end of the reach. The model flow field was input to the Branched Lagrangian Transport Model (BLTM) for the simulation of dye transport. The results of the FEQ and BLTM model simulations are compared with the measured data and sensitivity analyses of the model parameters for this application are presented.
Suggested Citation
Ishii, A., Turner, M.J., 1996, Verification of a one-dimensional, unsteady-flow model for the Fox River in Illinois: U.S. Geological Survey Water Supply Paper 2477, v, 65 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2477.
Publication type
Report
Publication Subtype
USGS Numbered Series
Title
Verification of a one-dimensional, unsteady-flow model for the Fox River in Illinois
Series title
Water Supply Paper
Series number
2477
DOI
10.3133/wsp2477
Year Published
1996
Language
ENGLISH
Publisher
U.S. G.P.O. ;
For sale by the U.S. Geological Survey, Information Services,