2011
DOI: 10.3133/sir20115128
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Updated one-dimensional hydraulic model of the Kootenai River, Idaho: A supplement to Scientific Investigations Report 2005-5110

Abstract: Vertical coordinate information is referenced to the North American Vertical Datum of 1988 (NAVD 88). Horizontal coordinate information is referenced to the North American Datum of 1983 (NAD 83).

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Cited by 3 publications
(3 citation statements)
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“…In order to achieve our objective of estimating depth‐averaged velocity, we designed our Bayesian network based on simulations from the depth‐averaged equations describing the flow of water in a one‐dimensional channel often referred to as the Saint Venant equations, (h)t+(uh)x=0 and ut+uux+ghx+n2u|u|h4/3=0 where h is water head elevation from the reference level, t is time, x is the distance along the channel, u is the flow velocity in the x direction, g is the gravitational constant, and n is the Manning coefficient describing bed roughness [ Stelling et al ., ]. Several previous studies [ Berenbrock and Bennett , ; Czuba and Barton , ] demonstrate that one‐dimensional approximations of flow produce errors less than 20% of depth‐averaged and cross‐section averaged velocity when compared with observations on the Kootenai River.…”
Section: Methodsmentioning
confidence: 99%
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“…In order to achieve our objective of estimating depth‐averaged velocity, we designed our Bayesian network based on simulations from the depth‐averaged equations describing the flow of water in a one‐dimensional channel often referred to as the Saint Venant equations, (h)t+(uh)x=0 and ut+uux+ghx+n2u|u|h4/3=0 where h is water head elevation from the reference level, t is time, x is the distance along the channel, u is the flow velocity in the x direction, g is the gravitational constant, and n is the Manning coefficient describing bed roughness [ Stelling et al ., ]. Several previous studies [ Berenbrock and Bennett , ; Czuba and Barton , ] demonstrate that one‐dimensional approximations of flow produce errors less than 20% of depth‐averaged and cross‐section averaged velocity when compared with observations on the Kootenai River.…”
Section: Methodsmentioning
confidence: 99%
“…In order to design and implement a recovery program, information about past, present, and future hydrologic conditions must be known. Since data are not available for all river restoration scenarios, hydrodynamic model simulations of actual and plausible river conditions must be implemented [ Czuba and Barton , ].…”
Section: Introductionmentioning
confidence: 99%
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